Maharashtra Board Class 11 Geography Chapter 4 Climatic Regions Solutions

Get the most accurate MSBSHSE Solutions for Class 11 Geography Chapter 4 Climatic Regions here. Updated for the 2026-27 academic session, these solutions are based on the latest MSBSHSE textbooks for Class 11 Geography. Our expert-created answers for Class 11 Geography are available for free download in PDF format.

Detailed Chapter 4 Climatic Regions MSBSHSE Solutions for Class 11 Geography

For Class 11 students, solving MSBSHSE textbook questions is the most effective way to build a strong conceptual foundation. Our Class 11 Geography solutions follow a detailed, step-by-step approach to ensure you understand the logic behind every answer. Practicing these Chapter 4 Climatic Regions solutions will improve your exam performance.

Class 11 Geography Chapter 4 Climatic Regions MSBSHSE Solutions PDF

Std 11 Geography Chapter 4 Question Answer Climatic Regions Maharashtra Board

Class 11 Geography Chapter 4 Climatic Regions Question Answer Maharashtra Board

Geography Class 11 Chapter 4 Question Answer Maharashtra Board

Question 1. Write the names of climatic regions according to the factors that dominate their characteristics.
Answer:

Name of climatic regionLatitudinal locationWinds and wind systemProximity to seaContinental locationAltitude
Tropical Monsoon ClimateBetween 10° to 30° latitudes N and SSummer onshore and winter offshore wind movementCoastal areas--
Tropical Savannah ClimateBetween 10° to 20° latitudes N and SAlternating ITCZ and subtropical high and EasterliesCoastal areas and interior also--
Tropical desert of Arid regionBetween 20° and 30° latitudes N and SDiverging circulation of subtropical high and windy conditionsProximity to sea and interior areas--
Mediterranean ClimateBetween 30° and 40° latitudes N and SSubtropical high in summer, Westerlies in winterCoastal locations--
China type ClimateBetween 20° and 40° N and SHumid onshore air movement in summer cyclonic storm in winterEast coastal location--
Marine West European type of climateBetween 45° to 60° latitudes N and SUnder the influence of WesterliesWest coastal location--
Taiga or Sub-Artic climateBetween 55° and 65° N latitudesWesterlies in summer, strong polar anticyclones in winter (Asia)Far away from seaContinental area-
Tundra climateBetween 65° to 90° N latitudesPolar anticyclonesProximity to coast--
Ice sheetsNear the N and S polesFrequent polar anticyclones-Interior areas-
Highland or mountain typeIn all mountainous regionsCold bitter windsSome places near the coastSome places continental locationHigh altitudes
In simple words: Climatic regions are categorized based on factors like latitude, wind systems, proximity to the sea, continental location, and altitude, which together determine the overall climate characteristics.

🎯 Exam Tip: Understanding the dominant factors for each climatic region helps in distinguishing them and is crucial for map-based questions and explanations.

 

2. Choose the Correct Alternative

Question 1. Monsoon region
(a) annual average temperature around 27°C
>2500 mm annual precipitation
Indonesia
Hard-wood evergreen trees
(b) Average temperature in Summers around 35° C
< 2500 mm annual rainfall
South East Asia
Hard wood deciduous trees
(c) Temperatures in summer around 35° C
1000 mm annual rainfall
Continental part of Indian peninsula
Tall and thick grass
(d) Average temperatures in summer around 27° C
1000 mm rainfall in winter
South Africa
Hard-wooded, waxy, evergreen forests
Answer: (b) Average temperature in Summers around 35° C
< 2500 mm annual rainfall
South East Asia
Hard wood deciduous trees

In simple words: The monsoon region typically features warm summers around 35°C, less than 2500 mm of annual rainfall, is found in areas like South East Asia, and supports hard wood deciduous trees.

🎯 Exam Tip: For MCQ questions, thoroughly compare all options to identify the most accurate description matching the characteristics of the specific climatic region mentioned.

 

Question 2. The region with high diurnal range of temperature
(a) Tropical rainforests
(b) Tropical grasslands
(c) Tropical desert regions
(d) Tropical Monsoon regions
Answer: (c) Tropical desert regions
In simple words: Tropical desert regions experience the largest differences between daytime high and nighttime low temperatures due to clear skies and lack of moisture.

🎯 Exam Tip: Remember that lack of humidity and cloud cover in deserts allows for rapid heating during the day and rapid cooling at night, leading to a high diurnal temperature range.

 

Question 3. Lumbering flourished as an occupation from Newfoundland to Alaska in North America because
(a) Tundra Climatic Region
(b) Taiga Climatic Region
(c) West European Climatic Region
(d) China-type climatic region
Answer: (b) Taiga Climatic Region
In simple words: Lumbering is a key activity in the Taiga Climatic Region because it is characterized by extensive coniferous forests, which are valuable for timber.

🎯 Exam Tip: Associate specific climatic regions with their dominant vegetation types and corresponding economic activities like lumbering (coniferous forests in Taiga).

 

Question 4. The main reason behind the months of precipitation in the graphs of Monsoon climatic regions being different is
(a) ITCZ
(b) orographic rainfall
(c) hemispheres are different
(d) apparent movement of the sun
Answer: (a) ITCZ
In simple words: The shifting of the Intertropical Convergence Zone (ITCZ) is the primary factor influencing the timing of precipitation in monsoon climatic regions, leading to different rainy seasons across hemispheres.

🎯 Exam Tip: The ITCZ's migration significantly impacts global weather patterns, particularly the timing and intensity of monsoons. Understanding its role is crucial for questions on seasonal rainfall.

 

3. Give Geographical Reasons.

Question 1. In monsoon climate region, rainfall occurs in specific season.
Answer: In monsoon climate region, rainfall occurs in specific season because-
1. The differential heating and cooling of land and water creates low pressure on the land while the sea experiences high pressure.
2. This is strongly related to shifting of the ITCZ. During the summer the ITCZ moves north to the latitudes of 20°-25°.
3. Several months later, the moisture laden summer monsoon is replaced by dry north-east monsoon.
4. By this time, the ITCZ has shifted to the southern hemisphere.
5. In northern hemisphere, the winds move from sea to land bringing moisture along with them in summers and gives rainfall.
6. In southern hemisphere same conditions prevail when there are winters in the northern hemisphere.
In simple words: Monsoon rainfall is seasonal because it's driven by the differential heating of land and sea, causing pressure changes and the movement of the ITCZ, which brings moisture-laden winds during specific summer months.

🎯 Exam Tip: When explaining monsoons, always refer to the ITCZ's movement and the land-sea temperature contrast as key drivers for seasonal rainfall patterns.

 

Question 2. Taiga region is not found in Southern Hemisphere.
Answer: Taiga region is not found in Southern Hemisphere because-
1. There is not much land at higher altitude in the southern hemisphere (until inside the Antarctic circle) where it is permanently ice covered.
2. Most of the land is fairly close to oceans and thus tempered by marine warming.
3. Whereas, Taiga is found throughout the high Northern latitudes between Tundra and the temperate forest, characterised by coniferous forests.
4. The strong oceanic influence in the southern hemisphere reduces the severity of the winter, thus, affecting the temperature and precipitation.
In simple words: The Taiga region is absent in the Southern Hemisphere mainly due to the scarcity of landmass at suitable latitudes and the moderating effect of vast oceans, which prevent the extreme continental conditions necessary for Taiga forests.

🎯 Exam Tip: Relate the absence of specific biomes like Taiga in a hemisphere to the distribution of landmasses and oceanic influences, which modify climate significantly.

 

Question 3. The diurnal range of temperature is more in desert areas.
Answer: The diurnal range of temperature is more in desert areas because-
1. Deserts get hot during the day, but cool down rapidly during night. The main reasons for the temperature fluctuation between day and night are the lack of humidity and cloud cover.
2. Because of water's relatively high specific heat, humid air takes longer to warm or cool, while air on land warms or cools more quickly.
3. Because desert areas receive a large amount of sunlight, the temperatures can get very high, but during night the dry air cools quickly.
4. The lack of cloud cover overhead allows the warmer air to rise into the atmosphere while cooler air settles in its place.
5. Basically, desert temperature varies so much because there is less moisture and cloud to keep the heat there.
In simple words: Deserts have a high diurnal temperature range because the lack of moisture and clouds allows for rapid heating during the day due to intense sunlight and quick heat loss at night through radiation.

🎯 Exam Tip: Focus on the role of humidity and cloud cover in regulating temperature. Their absence in deserts directly leads to extreme daily temperature swings.

 

Question 4. There is no concept of season in equatorial regions.
Answer: There is no concept of season in equatorial regions because-
1. The equatorial region lies between 0° to 10° latitudes in both the hemispheres.
2. The sun is exactly overhead in the equatorial regions throughout the year giving maximum insolation.
3. Thus, constant high temperatures are experienced throughout the year, which gives rise to heavy convectional precipitation.
4. Days and nights are almost of equal length and thus, the concept of summer and winter as being hot and cold seasons do not exist in these parts.
In simple words: Equatorial regions lack distinct seasons because they receive consistent, intense sunlight throughout the year, leading to uniformly high temperatures and regular convectional rainfall.

🎯 Exam Tip: For equatorial climates, emphasize consistent insolation, high temperatures, and convectional rainfall as key reasons for the absence of seasonal variation.

 

Question 5. The Savannah region is prone to droughts.
Answer: The Savannah region is prone to droughts because-
1. The region lies between 10° to 20° N and S latitudes, where the sun's rays at noon are never far from overhead and thus the insolation is maximum and temperature is constantly high here.
2. Distinct wet and dry seasons of relatively equal duration are found. Most of the regions annual rainfall is experienced during the wet season and very little precipitation falls during the dry season.
3. A lengthy dry season and a relatively short wet season is the characteristic of Savannah region.
4. Thus, in Savannah region the dry season becomes more severe and often drought conditions prevail during the course of the year.
In simple words: Savannah regions are prone to droughts due to their distinct and often lengthy dry seasons, during which very little precipitation falls, despite high temperatures and maximum insolation.

🎯 Exam Tip: Highlight the pronounced wet and dry seasons characteristic of Savannah climate. The duration and intensity of the dry season are key to explaining drought susceptibility.

 

Question 6. Though Mussoorie and Dehradun are located on the same latitude, why is their climate different?
Answer: Though Mussoorie and Dehradun are located on the same latitude, their climate is different because-
1. Dehradun lies in the humid sub-tropical climatic region where the summers are long, hot and humid. Whereas, Mussoorie is a hill station in Dehradun district of Uttarakhand which lies in sub-tropical climatic regions that are very wet.
2. Dehradun lies at an elevation of average 450 m above mean sea level whereas Mussoorie is at an elevations of 1880 m above mean sea level.
3. In Dehradun during monsoon season there is often heavy and protracted rainfall, whereas in Mussoorie an average of 660 mm orographic rainfall is experienced.
4. The winter temperature is around 1°C and 20°C in Dehradun with fog commonly experienced. Mussoorie usually receives few spells of snowfall in December, January and February.
In simple words: Despite being on the same latitude, Mussoorie and Dehradun have different climates primarily due to their significant difference in altitude; Mussoorie, being a hill station at a much higher elevation, experiences cooler temperatures and snowfall compared to Dehradun's warmer, humid subtropical climate.

🎯 Exam Tip: When latitude is constant, factors like altitude, proximity to mountains (orographic rainfall), and local topography become critical in explaining climatic variations between two places.

 

4. Differentiate Between.

Question 1. Equatorial Rainforests and Savannah Climatic Regions.
Answer:

Equatorial RainforestsSavannah Climatic Regions
Latitudinal extentIt lies between 0° to 10° latitudes in both the hemispheres.It lies between 10° to 20° latitudes N and S.
TemperatureAs it lies near the equators sun rays are perpendicular and hence temperature is constantly high with average temperature around 27°C.Distinct wet summers and dry winters with summer temperatures around 35°C and winter temperature around 24°C.
RainfallHeavy convectional rainfall of 2500 mm to 3000 mm is evenly distributed over the year.In this region average rainfall of 250 mm to 1000 mm is expected.
VegetationEvergreen trees with dense three layered vegetation are found in rainforests.Tall thick grass (Elephant grass) with scattered drought-resistant trees are found in this region.
AnimalsClimbing and jumping animals, reptiles, etc., are found in this region.Grazing of animals is common. Herbivorous, carnivorous and scavengers are found in this region.
Regions of the worldThis type of climate is found in the Amazon basin, Congo basin, east coast of Central America, Madagascar, Malaysia, Indonesia, Philippines and Papua New Guinea.This type of climate is found in India in peninsular plateau and rain-shadow zone in Maharashtra, Telangana and Karnataka; parts of Mizoram. It is also found along borders of Congo, South Central Africa, Llanos of Venezuela, Campos of Brazil, etc.
In simple words: Equatorial rainforests are characterized by constant high temperatures and year-round heavy rainfall, supporting dense evergreen vegetation, while Savannah regions have distinct wet and dry seasons, higher summer temperatures, and are dominated by tall grasses and scattered drought-resistant trees.

🎯 Exam Tip: When differentiating climatic regions, focus on key parameters like latitudinal extent, temperature patterns, rainfall distribution (seasonal vs. year-round), and characteristic vegetation and animal life.

 

Question 2. Taiga Region and Tundra Region.
Answer:

Taiga RegionTundra Region
Latitudinal extentTaiga region is found between 55° to 65° North latitude.Tundra region is found between 65° to 90° North latitude.
Temperature (Summer)Brief cool summers with temperature around 15°C to 20° C.Summer temperature is around 0°C.
Temperature (Winter)Bitterly cold winters with temperature less than 0°C is found in this region.Winter temperature is around -20°C to -30°C.
PrecipitationYear-round precipitation is around 300 to 500 mm in summers, snowfall in winters.Precipitation is in form of snow around 300 to 500 mm.
Other Atmospheric phenomenonHeavy cloud cover, high humidity, drizzle, fog, frost, cold winter poleward are the characteristics of Taiga region.Low evaporation, coastal fog are the characteristics of Tundra region.
LocationContinental location.Proximity to coasts.
VegetationConiferous forest with soft wood, vegetables and root crops are found.Tundra vegetation, swamps during melting is formed.
Animal lifeAnimals with fur like moose, foxes, bear, etc., are found.Animals with fur like polar bear, seal, walrus are found.
Human occupationHunting and lumbering is the major occupation.Hunting and fishing is the major occupation.
Regions of the worldNorthern part of North America from Newfoundland to Alaska, northern Eurasia from Scandinavia through most of Siberia to the Bering Sea and Sea of Okhotsk are the major regions where Taiga region is found.Arctic ocean borderlands of North America, Greenland and Eurasia, Antarctic, Peninsula, some polar islands are the major regions under Tundra vegetation.
In simple words: Taiga is a sub-arctic climate with cold winters and cool summers, characterized by coniferous forests, while Tundra is an even colder polar climate with permafrost, very short summers, and low-growing vegetation.

🎯 Exam Tip: Focus on the latitudinal differences, severity of winters, presence of trees (Taiga) vs. low-lying vegetation (Tundra), and dominant human activities for clear differentiation.

 

Question 3. Monsoon and Mediterranean Regions.
Answer:

Monsoon RegionMediterranean Region
Latitudinal extentWithin 10° to 30° North and South of equator.Western coastal region between 30° to 40° North and South.
TemperatureSummer temperature is around 27°C to 32°C while winter temperature is 15°C to 24°C. High annual range of temperature.Summers are warm and dry and temperature is around 21°C to 27°C while winters are mild and moist and temperature is around 10°C to 14°C.
RainfallRainfall is between 250 to 2500 mm, excessively wet during rainy season.Rainfall is around 500 to 1000 mm in winter.
VegetationTropical rainforest, ranges from jungle to thorn forest in drier boundaries.Scrub, forests have leaves evergreen, hard, thick leathery and small. Coniferous vegetation on higher altitudes and grass in areas of low rainfall is found.
Human LifeAgriculture is the main occupation of people of monsoon region.Winter- sown grains, olives, grapes, vegetables, citrus fruits are found.
Development of tourism and cinema industry.
Regions of the worldCoastal areas of South West India and South East Asia, South West Africa, North East and South East Brazil, Northern part of Australia and parts of Japan come under the monsoon winds.Central California, borders of Mediterranean Sea, Cape Town (South Africa), Southern and South West Australia, Central part of Chile are the major region under Mediterranean climate.
In simple words: Monsoon regions have hot, humid summers with heavy rainfall and cooler, drier winters, primarily supporting agriculture, whereas Mediterranean regions experience hot, dry summers and mild, wet winters, ideal for winter-sown crops like olives and grapes.

🎯 Exam Tip: The key differentiator is the timing of rainfall: monsoons receive summer rain, while Mediterranean climates receive winter rain due to shifting pressure belts.

 

5. Answer In Detail.

Question 1. Explain, with examples, the effects of latitude on a place's climate.
Answer: Latitudes affect the climate of a place in different ways-
Places close to the equator receive more sunlight:
1. The equatorial region lying between 0° to 5° North and South latitudes receive maximum heat as the sunrays are directly falling on the equator.
2. Due to which the region receives heavy rainfall throughout the year.
3. As a result, evergreen forests are found is such regions.
4. Example: Amazon basin.
Places close to the tropical region receives less sunlight:
1. Temperature gradually decreases with increasing distance from the equator, as the angle of sun's rays decreases from it.
2. In tropical areas the sun rays become slanting and thus it gives less heat but covers more area.
3. Example regions lying between Tropic of Cancer 231/2°N to Tropic of Capricorn 23/4°S. Similarly, in the temperate regions 66X/20N and S and the polar regions the climate become extremely cool as the intensity of heat decreases. These regions are thus covered by snow.
In simple words: Latitude primarily determines climate by influencing the angle of the sun's rays; equatorial regions receive direct, intense sunlight causing high temperatures and rainfall, while higher latitudes receive slanting rays, resulting in cooler temperatures and snow cover.

🎯 Exam Tip: When discussing the effect of latitude, always link the angle of the sun's rays to the intensity of insolation received, which then dictates temperature and precipitation patterns.

 

Question 2. Explain with examples, how winds affect the climate of a place.
Answer:
1. The winds affect the climate because they create the hot and cold air which moves around.
2. Prevailing winds affect the climate of an area. The direction of local winds is determined by the daily temperature of variations.
3. When winds blow from warm areas, they carry higher temperatures while winds blowing from cold areas carry lower temperatures.
4. Thus, winds bring in heat/ cold from the direction it has been blown from and thus changes the temperature of the place which affects the climate. For e.g., cold wind waves from the Himalayas carry coldness to the parts of the Deccan plateau.
5. Winds that blow from the sea often carry moisture and give rain to the coast. For e.g.. south-west monsoon winds give heavy rainfall in the western coastline of India.
6. Some winds are warm and dry, they increase the temperature during winter season. For example, winds that blow to Britain from warm areas such as Africa are warm and dry. Such warm and dry winds increase the summer temperature in some areas.
In simple words: Winds influence climate by transporting air masses with specific temperature and moisture characteristics from their source regions; for example, cold winds from mountains bring coolness, while moist winds from oceans bring rainfall.

🎯 Exam Tip: Focus on two main effects of winds on climate: temperature moderation (carrying heat or cold) and precipitation (carrying moisture from oceans or land).

 

Question 3. Russia is larger than Chile in area but does not experience climatic diversity as Chile. Explain.
Answer:
1. The latitude and longitude of Russia is 61.5240°N and 105.3188°E respectively. It is located in northern Asia, between Europe on one side and North Pacific Ocean on the other side.
2. Chile is situated along western margin of South American continent. Its latitude and longitude are 35.6751°S and 71.5430°W respectively.
3. Russia has continental location since it is surrounded to south and west by huge landmass, and to the north lies Arctic ocean which is frozen, so it is like snow covered land.
4. Thus, due to continental location there are dry summer and very cold winters with temperatures of -30° and less and sometimes heavy snowfall.
5. The winter is mostly dry, snow covers the ground from the end of October to mid-March.
6. In Chile the coastal location and the east-west extent is very less.
7. There is a lot of climatic diversity in Chile. There is Atacama Desert in the north, Mediterranean climate at the central part, extreme cold climate in the east.
8. The most important factors that control the climate of Chile are Pacific anticyclone, cold Humboldt ocean current and mountain ranges along the coastline.
9. Thus, though Russia is larger than Chile in area but does not experience climatic diversity as Chile.
In simple words: Chile, despite being smaller, exhibits greater climatic diversity than Russia due to its unique north-south elongated shape and coastal mountain ranges, which lead to a variety of climates from deserts to Mediterranean and extreme cold, unlike Russia's largely continental and uniformly cold climate.

🎯 Exam Tip: Geographical extent, orientation (north-south vs. east-west), continental vs. coastal location, and the presence of significant topographical features like mountain ranges are crucial for explaining climatic diversity.

 

Question 4. Explain the factors affecting climate of a place giving examples.
Answer: Factors affecting climate of a place are as follows
ℹ️ चित्र व्याख्या (Diagram Explanation): यह आरेख एक फ्लोचार्ट के रूप में किसी स्थान की जलवायु को प्रभावित करने वाले छह प्रमुख कारकों को दर्शाता है। ये कारक हैं अक्षांश (Latitude), ऊँचाई (Altitude), समुद्र से दूरी (Distance from the Sea), प्रचलित पवनें (Prevailing Winds), समुद्री धाराएँ (Ocean Currents), और ढलान का पहलू (Aspect of Slope)। यह छात्रों को जलवायु निर्धारकों की एक स्पष्ट और संक्षिप्त सूची प्रदान करता है।
Latitude: Latitude is the primary factor influencing distribution of atmospheric temperature. Generally, latitudes of high degrees are less warm than the low degrees of latitudes. Thus, sun's rays making a high angle to the ground, experience high temperature throughout the year. Temperature gradually decreases with increasing distance from the equator as the angle of the sun's rays decreases away from it. Hence, the polar region experiences very low temperature.
Altitude: The atmosphere is indirectly heated by terrestrial radiation from surface of the earth. Therefore, the place near the sea level experiences higher temperature than the places situated at higher altitude. In other words, the temperature generally decreases with increase in height. The rate of decrease of temperature with increase in height is known as Normal Lapse rate. It is 6.4°C per 1000 meters altitude.
Distance from the Sea : The location of place with respect to the sea also determines the temperature of that place. Though, the sun provides same amount of heat over land and water bodies, there is difference in their heating and cooling capacity. Compared to land, the sea (water) gets heated slowly and loses heat slowly. On the other hand, land heats up and cools down faster. Therefore, the variation in temperature over the water bodies is less as compared to land masses. The coastal areas come under the moderating influence of the sea and land breezes and experience moderate or equable climate while interior parts of the continents experience extreme climate.
Prevailing winds : Winds affect the temperature and rainfall of any area. Winds carry with them the temperature of their source regions. Hot winds increase the temperature while cold winds decrease the temperature, e.g., cold wind waves from Himalayas carry low temperature to parts of the Deccan Plateau. Thus, south west monsoon winds in India reduce the temperature after the onset of monsoon in June all over the country.
Some winds carry moisture and give rain to the area they visit. For example, South-west monsoon winds give rainfall to western coastline of India.
Ocean currents : Ocean currents considerably influence temperature of the adjacent land area. Warm currents raise the temperature of the coastal areas, whereas cold currents reduce the temperature near the coast where they flow.
Aspect of slope : In the northern hemisphere the south facing slopes and in the southern hemisphere the north facing slopes always face the sun. Hence, sun facing slopes are warmer and the opposite slopes are cooler.
In simple words: Climate is influenced by latitude (sun's angle), altitude (temperature decrease with height), distance from the sea (moderating effect), prevailing winds (carrying temperature and moisture), ocean currents (warming or cooling coasts), and aspect of slope (sun exposure).

🎯 Exam Tip: When listing factors affecting climate, provide a concise explanation and a relevant example for each to demonstrate a comprehensive understanding.

 

6. On A World Map, Show The Following Areas
(1) Equatorial Rainforests and Savannah Climatic Regions.
(1) Savannah climatic region in Africa
(2) Highland climatic region in India
(3) Chile and Russia
(4) Ice cap climatic region
(5) Desert
Answer:
ℹ️ चित्र व्याख्या (Diagram Explanation): यह एक विश्व मानचित्र है जो विभिन्न जलवायु क्षेत्रों के वितरण को दर्शाता है। इसमें इक्वेटोरियल वर्षावन, सवाना जलवायु क्षेत्र (विशेषकर अफ्रीका में), भारत में पहाड़ी जलवायु क्षेत्र, चिली और रूस, बर्फ की टोपी वाले जलवायु क्षेत्र, रेगिस्तान जलवायु क्षेत्र, टैगा क्षेत्र और मानसून क्षेत्र दिखाए गए हैं। छात्र इस मानचित्र का उपयोग विश्व के विभिन्न भौगोलिक क्षेत्रों में इन जलवायु प्रकारों की स्थिति को समझने के लिए कर सकते हैं।
In simple words: This question requires identifying and marking specific climatic regions such as equatorial rainforests, savannah, highland, ice cap, desert, and the countries Chile and Russia on a world map to understand their global distribution.

🎯 Exam Tip: For map-based questions, accurately locate and label each specified region. Practice identifying the characteristic geographical extent of each climatic zone.

 

11th Geography Digest Chapter 4 Climatic Regions Intext Questions And Answers

Use Your Brain Power!

Question 1.
(i) Have you ever thought why there is difference in the skin colour of various people in the world?
(ii) Why all the people in the world do not eat same food?
(iii) Why there is a variety in clothing pattern and types too? Even our houses are different.
(iv) How come flora and fauna are restricted to a particular region?
(v) Why different fruits are found in different places? (Textbook Page No. 44)
Answer:
(i) There is variation in skin colour of people depending on the latitudes. For. e.g., people near the equator are dark since the sunrays are vertical and hence there is too much heat, while people in temperate or polar region are fair since sunrays in these regions are slanting due to increase in distance from sun. Hence, there is low temperature and colour of skin is fair.
(ii) There is variation in food because food depends on geographical factors like climate, soil, location etc. For example, in extreme cold climate areas soil is covered with snow, so agriculture is not possible, people eat fish and meat of fur bearing animals. The countries located along the coastline eat fish and rice because fishing is carried out at the coastal areas and rice is grown on fertile delta of the river along the coastline.
(iii) People prefer to use clothes according to climate. For example, Inuits in Polar region wear fur clothes due to extreme cold climate, Europeans wear woollen cloths in winter due to cold climate, Asians mostly wear cotton clothes except in winter.
The pattern of house depends upon the climate and availability of material in the surrounding area. For example, in heavy rainfall areas houses have sloping roofs, in hot climatic areas houses are made up of stones or thick walls to prevent the effect of outside hot air.
People use material available in the surrounding area for construction of houses. For example, Inuits in Polar region use snow to build houses, since it is available in plenty. These peculiar houses are called Igloos.
(iv) Particular temperature and rainfall are essential for the growth of flora. For example, coniferous forest grows in cool climate and snowfall. Flora provides food and shelter to fauna, therefore wherever there is thick flora, fauna is bound to be there. In grassland region grass eating animals like dear, antelope, rabbits are seen but the camel is seen only in the desert.
(v) Every fruit crop requires particular type of climate; therefore, different fruits grow in different areas depending upon the climate. For example, apples are grown in Jammu and Kashmir, mangoes, cashew nuts and jackfruits are grown in the Konkan region due to suitable climate.
In simple words: Human characteristics (skin color, food, clothing, housing) and natural distribution of flora and fauna and fruits are all largely determined by the local climate, which dictates environmental conditions, resource availability, and adaptive responses.

🎯 Exam Tip: When explaining human and natural variations globally, always connect them to the underlying climatic conditions, emphasizing adaptation and resource dependency.

(ii) There is variation in food because food depends on geographical factors like climate, soil, location etc. For example, in extreme cold climate areas soil is covered with snow, so agriculture is not possible, people eat fish and meat of fur bearing animals. The countries located along the coastline eat fish and rice because fishing is carried out at the coastal areas and rice is grown on fertile delta of the river along the coastline.
(iii) People prefer to use clothes according to climate. For example, Inuits in Polar region wear fur clothes due to extreme cold climate, Europeans wear woollen cloths in winter due to cold climate, Asians mostly wear cotton clothes except in winter.
The pattern of house depends upon the climate and availability of material in the surrounding area. For example, in heavy rainfall areas houses have sloping roofs, in hot climatic areas houses are made up of stones or thick walls to prevent the effect of outside hot air.
People use material available in the surrounding area for construction of houses. For example, Inuits in Polar region use snow to build houses, since it is available in plenty. These peculiar houses are called Igloos.
(iv) Particular temperature and rainfall are essential for the growth of flora. For example, coniferous forest grows in cool climate and snowfall. Flora provides food and shelter to fauna, therefore wherever there is thick flora, fauna is bound to be there. In grassland region grass eating animals like dear, antelope, rabbits are seen but the camel is seen only in the desert.
(v) Every fruit crop requires particular type of climate; therefore, different fruits grow in different areas depending upon the climate. For example, apples are grown in Jammu and Kashmir, mangoes, cashew nuts and jackfruits are grown in the Konkan region due to suitable climate.
In simple words: Human activities like diet, clothing, housing, and agriculture are directly shaped by local climate, geography, and resource availability across different regions of the world.

🎯 Exam Tip: Understanding how geographical factors dictate human lifestyles is key for comprehensive answers in human-environment interaction questions.

Question 2.
(i) What would be the annual range of temperature in this region?
(ii) Where is this type of climate found in India?
Answer:
(i) In equatorial region both diurnal and annual range of temperature will be low as it experiences high temperature all year round. The annual range of temperature may be as low as 3°C.
(ii) This type of tropical rainforest climate is found in north eastern states of India, western coast of West Bengal, and Andaman and Nicobar Islands.
In simple words: Equatorial regions experience consistently high temperatures year-round with a very small annual temperature range, typically seen in India's northeastern states and islands.

🎯 Exam Tip: Remember that equatorial regions are characterized by low annual temperature range and high rainfall, crucial points for describing their climate.

Question 3.Comment upon the type of weathering which will occur in this region.
Answer: Mechanical and chemical weathering is predominant in this region.
In simple words: Both physical and chemical processes are highly active in breaking down rocks and soil in this region.

🎯 Exam Tip: Predominance of both weathering types indicates a dynamic environment, often linked to areas with significant temperature fluctuations and moisture.

Question 4.
(i) Which agricultural crops are produced here?
(ii) Why are longitudes not given in geographical distribution?
Answer:
(i) Maize and rice are grown all over Savannah region. Sorghum and millets are grown in northern Savannah. Stray crops and vegetables are grown in all regions.
(ii) Temperature is the main element of climate. The temperature varies with latitude and not with longitudes. Geographical distribution is the natural arrangement of the various forms of plants and animals in different regions and localities of the earth. This distribution varies with the latitude as we go away from the equator towards the poles. Thus, longitudes are not given.
In simple words: Savannah regions produce crops like maize, rice, sorghum, and millets; geographical distributions of climate are primarily mapped by latitude because temperature, a key climate factor, varies significantly with distance from the equator, not longitude.

🎯 Exam Tip: For geographical distributions, focus on latitude's impact on temperature and climate zones, as longitude primarily affects time and not climate patterns.

Question 5.Comment upon the rate of weathering in this climate.
Answer: Mechanical or physical weathering is predominant in arid regions. The rate of weathering is very slow in this region.
In simple words: In arid climates, mechanical weathering is the main process, but its overall rate is very slow due to limited moisture for chemical reactions.

🎯 Exam Tip: Low moisture in arid regions leads to slow weathering, predominantly mechanical due to temperature changes, not chemical breakdown.

Question 6.Why do people in Europe use olive oil for cooking?
Answer: Most olives are grown in the southern part and is used for almost every application. It is a healthy type of oil which makes it great for cooking.
In simple words: Olive oil is widely used in Europe because olives are abundantly grown in the southern parts of the continent, and it's considered a healthy cooking oil.

🎯 Exam Tip: Connect agricultural practices and staple foods to regional climate and available resources, as seen with olive cultivation in Mediterranean climates.

Question 7.What factors make this region agriculturally productive?
Answer: Year-round precipitation and fertile soil along the rivers make the region agriculturally productive.
In simple words: Consistent rainfall throughout the year combined with rich riverine soils makes this region highly productive for agriculture.

🎯 Exam Tip: Highlight continuous water availability and nutrient-rich soils as primary drivers for sustained agricultural productivity in a region.

Question 8.
(i) Why does Chile recur frequently in examples of geographical distribution?
(ii) Why has fishing developed here?
Answer:
(i) The geography of Chile is extremely diverse as the country extends from a latitude 17° South to Cape Horn at 56° and ocean on the west to Andes on the east. It borders Pacific Ocean towards south and small part of the south is towards the Atlantic Ocean.
(ii) Due to long indented coastlines and cool climate, fishing is done on a large scale. Presence of South Pacific Ocean and small part of South Atlantic Ocean are major fishing regions.
In simple words: Chile is often cited in geographical examples due to its extreme latitudinal and varied topography, leading to diverse climates; its extensive, indented coastlines and cool ocean waters foster significant fishing industries.

🎯 Exam Tip: When discussing regional diversity, use examples like Chile to illustrate how a country's shape and location can lead to a wide range of climates and economic activities.

Question 9.
(i) What would be the annual range of temperature in this climate? What could be the occupational activities carried out by humans here?
(ii) What type of weathering will be prominent here?
Answer:
(i) The annual range of temperature in Taiga is 60°, the summer temperature can be 10°C and average winter temperature is -60°C. Hunting and lumbering can be carried out in this region.
(ii) Since the region is covered by snow weathering is slow. Mechanical weathering is prominent here but is very slow. Alternate freezing and thawing takes place here.
In simple words: The Taiga region experiences a vast annual temperature range (around 60°C) with cold winters and cool summers, supporting occupations like hunting and lumbering; weathering here is primarily slow mechanical weathering, characterized by freezing and thawing.

🎯 Exam Tip: For high-latitude regions like Taiga, remember the huge temperature swings and the dominance of cryological processes in weathering, alongside primary resource-based occupations.

Question 10.What kinds of mass movement may happen here?
Answer: Slow mass movement takes place here in the form of slumping where snow particles moves short distance down the slope.
In simple words: In this region, slow mass movement occurs as slumping, where snow particles gradually slide down slopes over short distances.

🎯 Exam Tip: Understand that snow-covered, cold environments are prone to specific types of slow mass movement like slumping, driven by gravity and freeze-thaw cycles.

Question 11.
(i) What kind of activities will bring people from other regions to this climate?
(ii) What could be the occupations followed here?
Answer:
(i) Since this region is severely covered by snow, scientific research and exploration can be done or fishing and hunting can be done but on a very smaller scale.
(ii) Hunting of aquatic life is the dominant occupation followed here.
In simple words: Activities attracting people to this snow-covered region include scientific research, exploration, and limited fishing and hunting; the primary occupation is hunting aquatic life.

🎯 Exam Tip: In extremely cold, snow-covered regions, economic activities are often specialized and limited to scientific endeavors, and sustainable hunting/fishing of resilient species.

Question 12.
(i) What type of human activities will develop in this region?
(ii) In what ways might high latitudes be different from high altitudes?
Answer:
(i) Terrace farming, animal rearing and tourism are the types of human activities that might develop in this region.
(ii) High latitudes are the regions away from the equator. The intensity of sunlight goes on decreasing as we move away from the equator towards the poles. The equatorial and tropical regions will have precipitation in the form of rainfall.
High altitude regions are the regions at an elevation from the mean sea level. In high altitude regions temperature decreases with increase in height therefore they are covered by snow as precipitation is in the form of snowfall.
In simple words: In this region, human activities such as terrace farming, animal rearing, and tourism may develop. High latitudes are characterized by decreasing sunlight intensity and rainfall further from the equator, while high altitudes experience temperature drops with increasing elevation, leading to snowfall.

🎯 Exam Tip: Differentiate between high latitudes (governed by sun angle and global circulation) and high altitudes (governed by lapse rate and topography) to explain their distinct climatic and human activity patterns.

Can You Tell?

Question 1.Make a list of the human activities you think that are not influenced by climatic elements.
Answer: There are five major activities of man.
Primary: Agriculture, fishing, lumbering, hunting and gathering.
Secondary: Industries and manufacturing.
Tertiary: Services like transport and communication, teachers, doctors, etc.
Quaternary: Research and development etc.
Quinary: Highly intelligent activities.
In simple words: All human activities, including primary resource extraction, secondary manufacturing, tertiary services, quaternary information processing, and quinary decision-making, are influenced by climatic elements to some extent.

🎯 Exam Tip: Emphasize that while some activities seem less direct, climate indirectly influences resource availability, infrastructure, and even human comfort and productivity across all economic sectors.

2. Read the graphs and answer the following questions.
ℹ️ चित्र व्याख्या (Diagram Explanation): यह आरेख ब्राजील के बेलेम और सिंगापुर के लिए मासिक वर्षा (नीला बार) और औसत तापमान (गुलाबी रेखा) को दर्शाता है। यह दर्शाता है कि दोनों स्थानों पर पूरे वर्ष उच्च तापमान और लगातार वर्षा होती है, जो भूमध्यरेखीय जलवायु का विशिष्ट पैटर्न है।
Question 1.In which months there is no rainfall?
Answer: In both Belem and Singapore it rains throughout the year.
In simple words: Both Belem and Singapore experience rainfall every month of the year, with no dry periods.

🎯 Exam Tip: Continuous year-round rainfall is a defining characteristic of equatorial climates, often associated with high humidity and convectional precipitation.

Question 2.In which month is the temperature highest?
Answer: The temperatures is highest in the month of October in Belem and in the month of May in Singapore.
In simple words: Belem records its highest temperature in October, while Singapore experiences its peak temperature in May.

🎯 Exam Tip: Note that while equatorial regions have consistent high temperatures, slight variations due to overhead sun position or local factors can lead to specific warmest months.

Question 3.In which month is the temperature lowest?
Answer: The temperature is lowest in the months of January and February in Belem and in the month of December and January in Singapore.
In simple words: Belem experiences its lowest temperatures in January and February, whereas Singapore's coolest months are December and January.

🎯 Exam Tip: Even in consistently warm equatorial climates, slight temperature dips occur, usually influenced by seasonal shifts in global pressure systems or increased cloud cover.

Question 4.What could be the factors which influence the climate of these places?
Answer: Both Belem and Singapore lie in the equatorial region, i.e., at 1° 27′ S to 48° 30′ W and 1° 17′ N and 103° 51′ E respectively. Thus, in both Belem and Singapore, the climate is characterised by uniform temperature and pressure, high humidity and abundant rainfall as the sunrays are perpendicular on the equator throughout the year.
In simple words: Belem and Singapore's equatorial location results in consistently high temperatures, uniform pressure, high humidity, and abundant rainfall because the sun's rays are directly overhead year-round.

🎯 Exam Tip: The primary factors influencing equatorial climates are direct insolation (sun's rays overhead) leading to high temperatures, low pressure, and convectional rainfall.

Question 5.Write a concluding statement about the climate of both the places based on the questions above.
Answer: Both cities experiences rainfall throughout the year. These is no dry season month. Average temperature varies little throughout. There is no distinct season, uniform temperature, high humidity and abundant rainfall. They have equatorial type of climate.
In simple words: Belem and Singapore both exhibit a typical equatorial climate, characterized by year-round rainfall, no distinct dry season, consistently high and uniform temperatures, and high humidity.

🎯 Exam Tip: A conclusive statement about equatorial climates should always include continuous rainfall, high humidity, and stable, high temperatures throughout the year.

3. Read the graph and answer the following questions.
ℹ️ चित्र व्याख्या (Diagram Explanation): यह आरेख भारत के मंगलुरु और ऑस्ट्रेलिया के केर्न्स के लिए मासिक वर्षा (नीला बार) और औसत तापमान (गुलाबी रेखा) को दर्शाता है। यह दक्षिणी और उत्तरी गोलार्ध में उनकी संबंधित मानसून और उष्णकटिबंधीय जलवायु विशेषताओं को उजागर करता है।
Question 1.Name the months of highest and lowest rainfall. What is the difference between the values of rainfall?
Answer: In Mangaluru highest rainfall month is July with around 1143 mm rainfall and lowest rainfall was found in the month of January which is the driest month. Thus, the difference between the values of rainfall is 1143 mm.
In Cairns highest rainfall is 486 mm in the month of February and least amount of rainfall occurs in August around 37 mm. Thus, the difference between the values of rainfall is 449 mm.
In simple words: Mangaluru's highest rainfall is in July (1143 mm) and lowest in January, with a difference of 1143 mm; Cairns' highest is in February (486 mm) and lowest in August (37 mm), with a difference of 449 mm.

🎯 Exam Tip: Clearly identify the peak and minimum rainfall months and calculate the difference to accurately describe the precipitation variability of a region.

Question 2.Name the months of highest and lowest temperature.
Answer: Highest and Lowest temperature in Mangaluru is in April around 32.4°C and in January with 21.6°C respectively. Highest and lowest temperature in Cairns is in January at around 27.5° C and July being coldest month 16.4°C respectively.
In simple words: Mangaluru's highest temperature is in April (32.4°C) and lowest in January (21.6°C); Cairns experiences its highest temperature in January (27.5°C) and lowest in July (16.4°C).

🎯 Exam Tip: When analyzing climate graphs, precisely identifying the months for maximum and minimum temperatures is crucial for comparing thermal regimes of different locations.

Question 3.Are the months of rainfall same in both the places? If not, why?
Answer: No, the months of rainfall are not same in both the places. It rains in Mangaluru from May to November whereas, in Cairns rainfall is observed in the months from November to May.
In simple words: Rainfall seasons differ between Mangaluru (May-November) and Cairns (November-May) because they are located in different hemispheres, experiencing opposite seasonal patterns.

🎯 Exam Tip: The primary reason for different rainfall months in two locations is their position in opposing hemispheres, causing reversed seasonal cycles.

Question 4.What could be the factors which influence the climate of these places?
Answer: The major factor which influences the climate of Mangaluru and Cairo is that Mangaluru lies in Northern hemispheres and Cairns in Southern hemispheres.
In simple words: The primary factor influencing the climates of Mangaluru and Cairns is their location in different hemispheres (Northern and Southern, respectively), which dictates their seasonal patterns.

🎯 Exam Tip: Hemispheric location is a fundamental factor determining the seasonal timing of climatic events like monsoon rainfall due to the Earth's tilt and revolution.

Question 5.What difference do you find in the graphs in fig and these?
Answer: There is variation in rainfall and temperature graphs of Mangaluru and Cairo as these lies in different hemispheres while the graphs of Fig. represent same temperature and rainfall throughout the year at Belem and Singapore. Both lie in the equatorial region, so not much variation is observed.
In simple words: The graphs for Mangaluru and Cairo show seasonal variations in rainfall and temperature due to their different hemispheres, unlike Belem and Singapore, which, being equatorial, show consistent year-round patterns.

🎯 Exam Tip: Always compare the seasonal variability (or lack thereof) in temperature and rainfall patterns when analyzing climate graphs from different latitudinal zones and hemispheres.

Question 6.Write a concluding statement about the climate of both the places.
Answer: The climate of Mangaluru and Cairo is tropical. There is significant rainfall in most of the months of the year with short dry season. In Mangaluru, January is the driest month with 00 mm. of precipitation. Most of the precipitation is in July. While, in Cairo, the least amount of rainfall occurs in August. In February, precipitation is the highest.
In simple words: Both Mangaluru and Cairo have tropical climates with significant rainfall for most of the year and short dry seasons, though their driest and wettest months vary due to their distinct geographical locations and seasonal influences.

🎯 Exam Tip: Concluding statements should synthesize rainfall and temperature patterns, highlighting seasonality and classification (e.g., tropical monsoon, desert) based on graphical evidence.

4. Read the graph and answer the following questions.
ℹ️ चित्र व्याख्या (Diagram Explanation): यह आरेख लागोस, नाइजीरिया और ब्रासीलिया, ब्राजील के लिए मासिक वर्षा (नीला बार) और औसत तापमान (गुलाबी रेखा) को दर्शाता है। यह दोनों स्थानों की भूमध्यरेखीय या उष्णकटिबंधीय जलवायु को दिखाता है, जिसमें पूरे वर्ष उच्च तापमान और आर्द्र या शुष्क मौसम के साथ महत्वपूर्ण वर्षा होती है।
Question 1.In which months is there no rainfall?
Answer: It rains throughout the year in both Lagos and Brasilia.
In simple words: Both Lagos and Brasilia receive rainfall consistently throughout every month of the year.

🎯 Exam Tip: Note that "no rainfall" scenarios are rare in tropical/equatorial regions; continuous precipitation often points to specific climate classifications.

Question 2.In which month is the temperature highest?
Answer: Temperature is highest in the month of March in Lagos and in the month of September in Brasilia.
In simple words: Lagos reaches its highest temperature in March, while Brasilia records its warmest month in September.

🎯 Exam Tip: The warmest month can vary even in tropical regions due to factors like overhead sun migration, cloud cover, or onset of monsoon. Be precise with months.

Question 3.In which month is the temperature lowest?
Answer: The temperature is lowest in Lagos in the month of August and that in the month of June in Brasilia.
In simple words: Lagos experiences its lowest temperatures in August, while Brasilia's coolest month is June.

🎯 Exam Tip: Identify the coldest month carefully, as it often correlates with increased cloudiness, higher rainfall, or specific seasonal wind patterns.

Question 4.Are the months of rainfall same in both the places? If not, why?
Answer: It is wettest in June in Lagos and January is the wettest month in Brasilia, Lagos is situated near the equator. Thus, there is significant precipitation difference between the rainy season and summer season.
Brasilia is located at the top of Brazilian highlands. It has milder climate due to elevation and with two distinct seasons, the rainy season and dry season.
In simple words: Rainfall months differ; Lagos is wettest in June due to its equatorial proximity, while Brasilia is wettest in January, influenced by its highland elevation which creates distinct wet and dry seasons.

🎯 Exam Tip: Differences in rainfall patterns can stem from both latitudinal position (equatorial proximity) and local geographical factors like elevation, which create distinct microclimates.

Question 5.What could be the factors influencing the climate of these places?
Answer: Lagos being near the equator and Brasilia located on the Brasilia highland, influences the climate of these places.
In simple words: Lagos's equatorial location and Brasilia's position on the Brazilian highlands are the main factors shaping their respective climates.

🎯 Exam Tip: Always consider both global factors (latitude) and local factors (topography, altitude) when explaining climatic influences on specific locations.

Question 6.What difference do you find in the previous and these graphs?
Answer: The total monthly precipitation is light in Mangaluru in the month of June, July, August and that of Cairns in the month of January, February, March whereas in equatorial region precipitation is experienced throughout the year. From this the graph of monsoon climate, we find that maximum precipitation is during the months of June to September.
In simple words: These graphs (Lagos, Brasilia) show year-round equatorial precipitation, distinct from Mangaluru and Cairns, where rainfall is lighter during specific months, indicative of monsoon climates with defined wet seasons.

🎯 Exam Tip: Compare precipitation distribution: equatorial climates show consistent year-round rain, while monsoon climates exhibit a distinct wet season with lighter rainfall in other months.

Question 7.Write a concluding statement about the climate of both the places.
Answer: The rainfall is much more in summer than the winters in Lagos. The least amount of rainfall occurs in December while greater amount of precipitation occurs in June. The temperature is higher on an average in March, whereas lowest temperature occurs in August. With regards to Brasilia here too the rainfall is much more in summer than the winters. Precipitation is lowest in June and highest in January, September is the hottest month and lowest temperature is in June.
In simple words: Lagos experiences heavier summer rainfall (peak in June, lowest in December) and higher average temperatures in March (lowest in August); Brasilia also has heavier summer rainfall (peak in January, lowest in June), with September as its hottest month and June as its coolest.

🎯 Exam Tip: When summarizing, specify seasonal rainfall and temperature peaks/troughs for each location to highlight their distinct climatic patterns and compare them effectively.

5. Read the graph and answer the following questions.
ℹ️ चित्र व्याख्या (Diagram Explanation): यह आरेख ऑस्ट्रेलिया के एलिस स्प्रिंग्स और मिस्र के काहिरा के लिए मासिक वर्षा (नीला बार) और औसत तापमान (गुलाबी रेखा) को दर्शाता है। यह शुष्क या अर्ध-शुष्क उपोष्णकटिबंधीय रेगिस्तानी जलवायु का प्रतिनिधित्व करता है, जिसमें पूरे वर्ष बहुत कम वर्षा और तापमान में महत्वपूर्ण बदलाव होते हैं।
Question 1.Name the months of highest and lowest rainfall. What is the difference between the values of rainfall?
Answer: In Alice Springs, September is the driest month with around just 10 mm rainfall. Whereas the most precipitation falls in the month of January around 38 mm. The difference between the value is around 28 mm.
Similarly, In Cairo, the driest month is May with no precipitation at all whereas it rains about 5 mm in the month of January. The difference between the values is just 5 mm.
In simple words: Alice Springs' driest month is September (10 mm) and wettest is January (38 mm), with a 28 mm difference; Cairo's driest is May (0 mm) and wettest is January (5 mm), with a 5 mm difference.

🎯 Exam Tip: For arid regions, note the extremely low precipitation values and the significant difference even between "wettest" and "driest" months, which are still minimal.

Question 2.Name the months of highest and lowest temperature.
Answer: The warmest month in Alice Springs is January with an average temperature of 38.7°C while July experiences lowest temperature of about 11.5°C. In Cairo, July is the warmest month with 27.6°C and lowest temperatures is in January with around 13.1°C temperature.
In simple words: Alice Springs is warmest in January (38.7°C) and coolest in July (11.5°C); Cairo is warmest in July (27.6°C) and coolest in January (13.1°C).

🎯 Exam Tip: Be precise with the month and corresponding temperature for both highest and lowest values to show clear understanding of seasonal thermal variation.

Question 3.Are the months of rainfall same in both the place? If not, why?
Answer: No, the months of rainfall are not same in both the places because Alice Springs lies in the Southern Hemisphere while Cairo lies in the Northern Hemisphere.
In simple words: Rainfall months differ because Alice Springs is in the Southern Hemisphere, and Cairo is in the Northern Hemisphere, leading to opposite seasonal precipitation patterns.

🎯 Exam Tip: The most common reason for differing seasonal patterns between two locations is their placement in opposite hemispheres, causing their summer and winter to be reversed.

Question 4.What could be the factors which influence the climate of these places?
Answer: Cairo in Egypt is located to the north of Tropic of Cancer, and Alice Springs is located just south of Tropic of Capricorn. Therefore, both the areas come under subtropical high-pressure belt. The air becomes dry here. The winds in this region blows out of the region, so there is very low rainfall. The region of Alice Springs is part of central Ranges scrub area of dry scrubby grasslands. Majority of the Egypt's landscape is desert, hence extreme aridity is experienced.
In simple words: Both Cairo and Alice Springs are influenced by their location within subtropical high-pressure belts, which leads to dry, outward-blowing winds and very low rainfall, resulting in extreme aridity and desert landscapes.

🎯 Exam Tip: Subtropical high-pressure belts are a key factor in desert climates, causing sinking dry air and preventing significant rainfall; their location relative to the tropics is crucial.

Question 5.What difference do you find in the previous and these graphs?
Answer: In the previous graphs rainfall is depicted for almost all the months. But in the graphs representing climate of Alice Springs and Cairo, rainfall is very low or almost negligible.
Temperature variation can also be depicted in the previous graphs and graphs of Alice Springs and Cairo.
In simple words: These graphs (Alice Springs, Cairo) show significantly lower and often negligible rainfall compared to previous graphs, which depicted rainfall in almost all months, though temperature variations are present in both sets.

🎯 Exam Tip: When comparing climate graphs, a critical distinction is the total annual precipitation and its distribution, which clearly separates humid from arid climates.

Question 6.Write a concluding statement about the climate of both the places.
Answer: Rainfall is very less in Alice Springs whereas almost negligible in Cairo. This is due to the latitudinal extent of both the places and subtropical high-pressure belt. Cairo is in or near the subtropical desert biome whereas Alice Springs is in or near subtropical desert scrub biome. The average annual temperature is 35°C warmer. Average monthly temperature varies by 3.7°C in Cairo.
In simple words: Both Alice Springs and Cairo are characterized by extremely low rainfall, largely due to their subtropical high-pressure belt locations, fitting into desert or desert scrub biomes, with Alice Springs being significantly warmer annually and Cairo showing less monthly temperature variation.

🎯 Exam Tip: A comprehensive conclusion for desert climates should highlight the influence of high-pressure belts, minimal precipitation, and specific temperature characteristics like high annual averages and diurnal/monthly variations.

6. Read the graph and answer the following questions.
ℹ️ चित्र व्याख्या (Diagram Explanation): यह आरेख ऑस्ट्रेलिया के पर्थ और इटली के रोम के लिए मासिक वर्षा (नीला बार) और औसत तापमान (गुलाबी रेखा) को दर्शाता है। यह भूमध्यसागरीय जलवायु का प्रतिनिधित्व करता है, जिसमें शुष्क, गर्म ग्रीष्मकाल और हल्के, गीले सर्दियाँ होती हैं।
Question 1.Name the months of highest rainfall.
Answer: Perth experiences highest rainfall in the month of June whereas Rome experiences highest rainfall in November.
In simple words: Perth's peak rainfall occurs in June, while Rome's highest precipitation is in November.

🎯 Exam Tip: For Mediterranean climates, remember that rainfall primarily occurs in winter months, and its timing will be reversed between the Northern and Southern Hemispheres.

Question 2.Name the months of lowest temperatures.
Answer: The temperature in Perth is the lowest in July and the temperature in Rome is the lowest in January.
In simple words: Perth's coldest month is July, and Rome's coldest month is January.

🎯 Exam Tip: The coldest months align with winter in each hemisphere, which is July in the Southern Hemisphere and January in the Northern Hemisphere.

Question 3.Are the answers to 1 and 2 same?
Answer: No, the answers are not same.
In simple words: The months of highest rainfall and lowest temperature are not the same for both Perth and Rome.

🎯 Exam Tip: Always verify if the patterns are identical or distinct between different locations, particularly when comparing two hemispheres.

Question 4.Are the months of rainfall same in both the places If not, why?
Answer: No, it does not rain in the same months in Perth and Rome. Perth lies on 31°57′ S to 115°51′ E longitude and Rome lies on 41°53′ N to 12°30′ E longitude. It means Perth is located in the Southern - Hemisphere, whereas Rome is in the Northern Hemisphere. Perth is near the Subtropical dry forest biome, whereas Rome is near the warm temperate moist forest biome.
In simple words: Rainfall seasons differ between Perth and Rome because they are in opposite hemispheres (Southern and Northern, respectively), leading to reversed seasonal patterns.

🎯 Exam Tip: The main reason for distinct rainfall patterns in different locations is their hemispheric location, which dictates the timing of summer and winter seasons.

Question 5.What could be the factors which influence the climate of a place?
Answer: The special feature of climate of this region is long dry summers and mild and wet winters. This because of subtropical high pressure in summer and westerly wind movement in winter.
In simple words: The climate of this region is influenced by factors such as subtropical high pressure in summer, causing dry conditions, and westerly wind movement in winter, bringing mild, wet weather.

🎯 Exam Tip: When analyzing Mediterranean climates, focus on the seasonal shift in pressure systems (subtropical high in summer, westerlies in winter) as key influencing factors.

Question 6.What difference do you find in the previous graphs and these graphs?
Answer: In Mediterranean regions, summers are long and warm and dry whereas winters are mild and wet. They are different from low-latitudinal climates where the temperature is high throughout the year. Rainfall in winter is the characteristic of this region but previous graph shows very meagre rainfall.
In simple words: These graphs, typical of Mediterranean climates, show long, dry summers and mild, wet winters, contrasting with previous graphs that exhibited high temperatures year-round and negligible rainfall, or continuous precipitation.

🎯 Exam Tip: The key differentiator for Mediterranean climates is the inverse relationship between temperature and precipitation seasonality: dry summers, wet winters, unlike equatorial or desert climates.

Question 7.Write a concluding statement about the climate of both the places.
Answer: Rainfall is highest in the month of June, around 175 mm in Perth, while its lowest in the month of January around just 7 mm. Whereas, November experiences highest rainfall of about 114 mm and lowest of about 17 mm in July in Rome. Temperature reaches its highest in February around 24.8°C and lowest in July around 13.6°C in Perth, while July experiences highest temperature of about 24.4° C and least about 7.7° in January in Rome.
In simple words: Perth's climate shows highest rainfall in June (175 mm) and lowest in January (7 mm), with peak temperature in February (24.8°C) and lowest in July (13.6°C); Rome has highest rainfall in November (114 mm) and lowest in July (17 mm), with peak temperature in July (24.4°C) and lowest in January (7.7°C).

🎯 Exam Tip: When providing a concluding statement, ensure to explicitly state the highest/lowest precipitation and temperature values along with their corresponding months for both locations.

7. Read the graph and answer the following questions.
ℹ️ चित्र व्याख्या (Diagram Explanation): यह आरेख ऑस्ट्रेलिया के ब्रिस्बेन और चीन के शंघाई के लिए मासिक वर्षा (नीला बार) और औसत तापमान (गुलाबी रेखा) को दर्शाता है। यह उनकी पूर्वी-तटीय या मानसूनी जलवायु विशेषताओं को उजागर करता है, जिसमें पूरे वर्ष उच्च तापमान और आर्द्र या शुष्क मौसम के साथ महत्वपूर्ण वर्षा होती है।
Question 1.Name the months of highest and lowest rainfall.
Answer: In Brisbane, highest rainfall occurs in the months of February, while lowest rainfall is in the month of September. In Shanghai, June experiences highest rainfall, while precipitation is lowest in December.
In simple words: Brisbane's highest rainfall is in February, with September being the driest; Shanghai sees its peak rainfall in June and lowest precipitation in December.

🎯 Exam Tip: Identify the months of maximum and minimum precipitation accurately for each location to highlight their seasonal rainfall patterns, which are crucial for eastern-margin climates.

Question 2.Name the months of highest and lowest temperatures. Relate them with rainfall months.
Answer: In Brisbane temperature is highest in January and lowest in July, while Shanghai experiences highest temperature in July and lowest in January.
In Brisbane, temperature is highest in January whereas rainfall is highest in February and high in January, whereas in Perth, July records highest temperature and June records highest rainfall. Similarly, temperature is least in January and rainfall is least in December.
In simple words: Brisbane's temperature peaks in January (matching high rainfall), lowest in July; Shanghai's temperature peaks in July (matching high rainfall), lowest in January.

🎯 Exam Tip: Analyze the relationship between temperature and rainfall. Often, high temperatures coincide with high rainfall in eastern-margin climates due to summer monsoon effects, but note exceptions like Perth if mentioned.

Question 3.Are the months of rainfall same in both the places? If not why?
Answer: No, both places have rainfall in different months. This is probably because Brisbane is located is Southern Hemisphere. Brisbane is in the south east corner of Queensland. The region is on the coastal plains, east of Great Dividing Range.
Shanghai is located in the Northern Hemisphere, located on Yangtze River Delta on China's east coast and has proximity to the Pacific Ocean via East China Sea.
In simple words: Rainfall seasons differ because Brisbane is in the Southern Hemisphere while Shanghai is in the Northern Hemisphere, experiencing reversed seasonal rainfall patterns. Their specific coastal and topographical locations also play a role.

🎯 Exam Tip: Hemispheric location is the primary driver for different seasonal rainfall timings; always consider specific geographic features like coastal plains or river deltas as secondary influences.

Question 4.What could be the factors which influence the climate of these places?
Answer: Brisbane and Shanghai, both lie in the eastern parts of the southern and northern hemispheres respectively. Due to proximity to the coral sea of the Pacific Ocean and warm ocean current, Brisbane's overall temperature variability is somewhat less.
Shanghai is located in the middle of China's east coast near the mouth of river Yangtze to the North, the East china sea to the east, Hangzhou Bay to the south and Jiangsu and Zhejiang provinces to the west.
In simple words: Brisbane's climate is influenced by its eastern coastal location in the Southern Hemisphere, warm ocean currents, and proximity to the Pacific, leading to less temperature variability; Shanghai's climate is shaped by its eastern coastal location in the Northern Hemisphere, near the Yangtze River mouth and East China Sea.

🎯 Exam Tip: Eastern margin climates are influenced by warm ocean currents, proximity to large water bodies, and their hemispheric location, leading to specific temperature and precipitation patterns.

Question 5.What difference do you find in the previous and these graphs?
Answer: The major difference between Mediterranean and China type is that, the Mediterranean is found on the western margins of the continents while china type is found is the eastern parts almost in same latitudes.
In Mediterranean type winter rainfall is the characteristics feature, while china type experiences rainfall throughout the year.
In simple words: These graphs (Brisbane, Shanghai, representing China type climate) show year-round rainfall, distinct from Mediterranean climate graphs which feature dry summers and wet winters; China type climates are typically found on eastern continental margins at similar latitudes to Mediterranean climates on western margins.

🎯 Exam Tip: Differentiate between western (Mediterranean: dry summer, wet winter) and eastern (China type: year-round rainfall, often summer maximum) continental margin climates at similar latitudes, noting their distinct precipitation patterns.

Question 6.Write a concluding statement about the climate of both the places.
Answer: Both the places receive rainfall from convectional showers. Precipitation is year-round. In Brisbane variation in the precipitation between driest and wettest months is 133 mm. During the year, average temperatures vary by 10.3°C.
In simple words: Both Brisbane and Shanghai climates are characterized by year-round convectional rainfall, with Brisbane showing a 133 mm difference between wettest and driest months and an annual temperature variation of 10.3°C.

🎯 Exam Tip: In concluding statements for eastern-margin climates, emphasize year-round precipitation, convectional rainfall, and quantify precipitation variability and annual temperature range if data allows.

8. Read the graph and answer the following questions.
ℹ️ चित्र व्याख्या (Diagram Explanation): यह आरेख यूएसए के पोर्टलैंड और ऑस्ट्रेलिया के मेलबर्न के लिए मासिक वर्षा (नीला बार) और औसत तापमान (गुलाबी रेखा) को दर्शाता है। यह शीतोष्ण समुद्री जलवायु या पश्चिमी यूरोपीय प्रकार की जलवायु का प्रतिनिधित्व करता है, जिसमें पूरे वर्ष मध्यम वर्षा और अपेक्षाकृत हल्के तापमान होते हैं।
Question 1.In which months do you find temperature the lowest?
Answer: Temperature is the lowest in the month of January in Portland and in Melbourne it's in the month of July.
In simple words: Portland's lowest temperature occurs in January, while Melbourne experiences its coolest month in July.

🎯 Exam Tip: Identify the coldest month for each location, noting that this corresponds to winter in their respective hemispheres (January for Northern, July for Southern).

Question 2.In which month is the precipitation lowest?
Answer: Precipitation is lowest in the month of July in Portland and lowest precipitation is found in the month of February in Melbourne.
In simple words: Portland's lowest precipitation is in July, and Melbourne's lowest precipitation occurs in February.

🎯 Exam Tip: Pinpoint the months with minimal precipitation to understand the seasonal distribution of dryness, even in regions with year-round rainfall.

Question 3.What are the highest values of precipitation?
Answer: In Portland highest precipitation is in the month of December with an average of
In simple words: Portland receives its highest precipitation in December.

🎯 Exam Tip: State the specific month and the corresponding precipitation value for the peak rainfall to provide accurate graphical analysis.

9. Read The Graph And Answer The Following Questions.


ℹ️ चित्र व्याख्या (Diagram Explanation): यह ग्राफ़ व्हाइटहॉर्स, कनाडा और आर्कान्जेल्स्क, रूस के लिए मासिक वर्षा (मिमी में) और तापमान (डिग्री सेल्सियस में) को दर्शाता है। यह उप-आर्कटिक जलवायु पैटर्न को चित्रित करता है, जो इन उच्च-अक्षांश महाद्वीपीय स्थानों के लिए वर्ष भर में ठंडे तापमान (अक्सर हिमांक से नीचे) और अपेक्षाकृत कम वर्षा को दर्शाता है।

Question 1. Note the values of the axes, how different are these graphs from the earlies ones?
Answer: The values of Taiga or Sub-Arctic regions show the mean annual temperature below freezing point (0°C) that is from 0° to -35° C. These values are not observed in rest of the graphs.
In simple words: These graphs are unique because their temperature scales go well below freezing (0°C to -35°C), which wasn't seen in the previous climate graphs.

🎯 Exam Tip: Pay attention to the range of values on the axes, especially for temperature, as it highlights key climatic differences between regions.

Question 2. Note the highest and the lowest temperature and their months.
Answer: In Whitehorse, the highest temperature recorded is around 20.0°C in the month of July, whereas January is the coldest month with average temperature of -23°C. In Arkhangelsk, the highest temperature is in the month of July around 20°C and lowest in the month of January around -18°C.
In simple words: Both Whitehorse and Arkhangelsk experience their warmest temperatures (around 20°C) in July and their coldest temperatures (around -18°C to -23°C) in January.

🎯 Exam Tip: Clearly state both the highest and lowest temperatures along with their corresponding months for each location to score full marks.

Question 3. Note the highest and lowest rainfall and their months.
Answer: Highest rainfall recorded is about 35 to 37 mm in the months of July, August in Whitehorse and lowest is in the month of April with just 9 mm. In Arkhangelsk, the greatest amount of precipitation occurs in August with an average of 66 mm. The lowest amount of rainfall occurs in February. The average is this month in 27 mm.
In simple words: Whitehorse gets most rain in July-August and least in April, while Arkhangelsk has its highest rainfall in August and lowest in February.

🎯 Exam Tip: Differentiate between rainfall amounts and months for each location mentioned, ensuring precise data points are included.

Question 4. Why does not a place from Southern Hemisphere appear here?
Answer: There isn't much land at higher latitudes in hemisphere (until inside the Antarctic circle where it is permanently ice covered) and most of that land is fairly close to oceans and it has effect of marine warming.
In simple words: The Southern Hemisphere lacks large landmasses at high latitudes (beyond the Antarctic circle), and the land present is warmed by the ocean, preventing the distinct sub-arctic continental climates shown here.

🎯 Exam Tip: Focus on the geographical distribution of landmasses and oceanic influence as key reasons for the absence of such climatic regions in the Southern Hemisphere.

Question 5. What factors are responsible for this climate?
Answer: Located in large Continental landmass between 55°-65° latitude, the Sub-Arctic climate is removed from any moderating influence of an ocean. It therefore, experiences a very large range in annual temperature. During the summer it is dominated by the westerlies and cyclonic activity the winter it is the polar hight and Easterlies. The Sub-Arctic climate has continental polar air masses.
In simple words: This climate is caused by large continental landmasses far from oceans at 55°-65° latitude, leading to extreme temperature variations, with westerlies and cyclones in summer, and polar highs and easterlies with continental polar air masses in winter.

🎯 Exam Tip: Identify and explain the interplay of continental location, latitude, distance from the ocean, prevailing winds, and air masses as primary factors.

10. Read The Graph And Answer The Following Questions.


ℹ️ चित्र व्याख्या (Diagram Explanation): यह ग्राफ़ बैरो, अलास्का और बैरेंट्सबर्ग, नॉर्वे के लिए मासिक वर्षा (मिमी में) और तापमान (डिग्री सेल्सियस में) को दर्शाता है। यह ध्रुवीय या टुंड्रा जलवायु परिस्थितियों का प्रतिनिधित्व करता है, जिसकी विशेषता अत्यंत कम तापमान (हिमांक से काफी नीचे) और पूरे वर्ष बहुत कम वर्षा होती है, जो अधिकतर बर्फ के रूप में होती है।

Question 1. Why is it that both the graphs are from the northern Hemisphere?
Answer: Tundra is located at the top of the world, near the north pole. Tundra is a Finnish word which means barren land. Thus, Tundra region having least vegetation and polar or arctic climate is found in North America and Eurasia between the southern limit of the permanent ice caps in the north and the northern limit of temperate coniferous forest of taiga climate in the south.
In simple words: Tundra climates are mostly found in the Northern Hemisphere because the vast landmasses at very high latitudes (near the North Pole) allow for the formation of these barren, permanently frozen regions between the ice caps and taiga forests.

🎯 Exam Tip: Connect the concept of tundra (barren land) with its high-latitude location in the Northern Hemisphere and its position relative to ice caps and taiga forests.

Question 2. Which are the warmest and the coolest months?
Answer: In Barrow, the warmest month is July while lowest temperature is in the month of February. Same temperature conditions are observed in Barentsburg.
In simple words: In both Barrow and Barentsburg, July is the warmest month, and February is the coolest.

🎯 Exam Tip: For comparative questions, clearly state the warmest and coolest months for all locations or note if they share the same pattern.

Question 3. What is the annual range of temperature?
Answer: The average annual range of temperature in Barrow is -12.2°C while in Barentsburg it is -5.9° C.
In simple words: The average yearly temperature swing in Barrow is -12.2°C, and in Barentsburg, it's -5.9°C.

🎯 Exam Tip: Calculate the annual range by finding the difference between the highest and lowest monthly average temperatures.

Question 4. Why does not the duration of day (sometimes more than 24 hours) influence its temperatures or precipitation?
Answer: This is because the sun's rays are oblique and little insolation is received being at higher latitude -65° to 90° North.
In simple words: Even with very long daylight hours at high latitudes, the sun's rays are so slanted that they provide very little direct heat (insolation), which means temperatures remain low and don't significantly increase precipitation.

🎯 Exam Tip: Emphasize the angle of the sun's rays (obliqueness) and the resulting low insolation at high latitudes as the primary reason for consistently low temperatures, despite extended daylight.

11. Read The Graph And Answer The Following Questions.


ℹ️ चित्र व्याख्या (Diagram Explanation): यह ग्राफ़ आइसमिट्टे, ग्रीनलैंड (उत्तरी गोलार्ध) और स्कॉट साउथ स्टेशन, अंटार्कटिका (दक्षिणी गोलार्ध) के लिए मासिक वर्षा (मिमी में) और तापमान (डिग्री सेल्सियस में) को दर्शाता है। यह अत्यधिक ध्रुवीय बर्फ़ीली टोपी जलवायु को चित्रित करता है, जिसकी विशेषता पूरे वर्ष लगातार बहुत कम तापमान (हिमांक से काफी नीचे) और न्यूनतम वर्षा होती है।

Question 1. Which are the warmest and the coolest months?
Answer: The warmest month is July and the coolest month is February in Eismitte. While in Scott South Station warmest months are December and January and coolest month is August.
In simple words: Eismitte is warmest in July and coolest in February, but Scott South Station is warmest in December-January and coolest in August, reflecting opposite hemispheres.

🎯 Exam Tip: Note the seasonal reversal in warmest/coolest months between the Northern (Eismitte) and Southern (Scott South Station) Hemispheres.

Question 2. Name the months of highest and lowest rainfall.
Answer: The month with highest rainfall in Eismitte is December and lowest rainfall is in May. While in Scott South Station highest rainfall is in the month of February, while lowest rainfall is observed in July and August.
In simple words: Eismitte sees its highest rainfall in December and lowest in May. Scott South Station has highest rainfall in February and lowest in July-August.

🎯 Exam Tip: Clearly identify the months of peak and minimal precipitation for each location, indicating the total amount if available from the graph for precision.

Question 3. In what way do you find similarities of this climate with other climate types of high latitudes?
Answer: Precipitation is very low in high latitude regions and mostly it is in the form of snowfall. Temperature is below freezing point (CPC) in all the high latitude regions. This is because the sun's rays are oblique and hence temperature is low. These regions are mostly under permanent snow cover.
In simple words: High-latitude climates, including these, share characteristics like very low precipitation (often snow), temperatures consistently below freezing, slanted sun rays causing low heat, and permanent snow cover.

🎯 Exam Tip: Compare and contrast highland climates with high-latitude climates, highlighting similarities in precipitation type (snowfall), snow cover, low temperatures due to insolation, and the effect of altitude.

Question 4. What factors influence this type of climate?
Answer: Little or no insolation during most of the months in a year, oblique sunrays are the factors responsible for this type of climate.
In simple words: This climate is primarily influenced by the extremely low amount of sunlight received throughout the year due to the very slanted angle of the sun's rays at these high latitudes.

🎯 Exam Tip: The primary factors are low insolation (incoming solar radiation) and the highly oblique angle of the sun's rays, directly linked to high latitude.

12. Read The Graph And Answer The Following Questions.


ℹ️ चित्र व्याख्या (Diagram Explanation): यह ग्राफ़ शिमला, भारत और एल अल्टो, बोलीविया के लिए मासिक वर्षा (मिमी में) और तापमान (डिग्री सेल्सियस में) को दर्शाता है। यह पर्वतीय या उच्चभूमि जलवायु को चित्रित करता है, जिसकी विशेषता उच्च ऊंचाई और स्थानीय स्थलाकृति से प्रभावित निम्न तापमान और भिन्न वर्षा पैटर्न होते हैं।

Question 1. Which are the warmest and the coolest months?
Answer: The warmest month is June while coolest month is January in Shimla. November is the hottest month and July is the coolest month in El Alto.
In simple words: In Shimla, June is warmest and January is coolest. In El Alto, November is hottest and July is coolest.

🎯 Exam Tip: Clearly state the warmest and coolest months for each location, noting any differences due to their respective hemispheres (Shimla in Northern, El Alto in Southern).

Question 2. Name the months of highest and lowest precipitation.
Answer: Most of the precipitation is in the months of July, whereas driest month is November is in Shimla. Precipitation is highest in January and lowest in June in El Alto.
In simple words: Shimla gets most precipitation in July and is driest in November. El Alto has highest precipitation in January and lowest in June.

🎯 Exam Tip: Identify the months of highest and lowest precipitation for both Shimla and El Alto, specifying their respective seasonal patterns.

Question 3. In what ways do you find similarities of this climate with other types of high latitudes?
Answer: In these regions, precipitation is in the form of snowfall. The regions are covered by snow. Temperature is very low, as the sunrays are oblique and little insolation is received. Temperature decreases with increasing altitude.
In simple words: Highland climates share similarities with high-latitude climates: precipitation often as snowfall, snow-covered regions, very low temperatures due to oblique sunrays and low insolation, and decreasing temperature with increasing altitude.

🎯 Exam Tip: Compare and contrast highland climates with high-latitude climates, highlighting similarities in precipitation type (snowfall), snow cover, low temperatures due to insolation, and the effect of altitude.

Question 4. Why are the axis showing temperature different in both the graphs?
Answer: Shimla is located at 31°6 N to 77°10 E and its elevation is 2,276 m whereas El Alto is located on 16°31 S to 68°10 W with an elevation of 4,150 mts. The temperature axes are different because temperature decreases with increasing altitude, and these places have significantly different elevations and latitudinal positions, resulting in distinct temperature ranges.
In simple words: The temperature axes differ because Shimla (2,276m, Northern Hemisphere) and El Alto (4,150m, Southern Hemisphere) have vastly different altitudes and locations, which lead to different temperature ranges according to the principle that temperature drops with higher elevation.

🎯 Exam Tip: When explaining differences in graph axes, always link them back to the specific geographical data (latitude, longitude, and especially altitude for highland climates) of the locations.

Question 5. What factors influence this type of climate?
Answer: The higher reaches of mountain, altitude, location of leeward or windward side, precipitation are the factors affecting climates of mountain type of climate.
In simple words: Mountain climates are influenced by high altitude, the specific side of the mountain (leeward or windward) which affects moisture, and overall precipitation patterns in the higher mountain regions.

🎯 Exam Tip: List the key geographical factors – altitude, mountain orientation (windward/leeward), and precipitation – as the primary drivers of mountain climate.

Find Out! (Textbook Page No. 44)

Question. Use internet or reference books to find out about the attempts at classification of climates.
Answer: Classification of climate was given by Wladimir Peter Koppen, Charles Warren Thornthwaite and Glenn Thomas Trewartha. [Student are required to research and attempt this question on their own]
In simple words: Climate classification systems were developed by scientists like Wladimir Koppen, Charles Thornthwaite, and Glenn Trewartha to categorize Earth's diverse climates.

🎯 Exam Tip: When asked about historical classifications, remember the prominent figures like Koppen, Thornthwaite, and Trewartha who laid the groundwork for modern climate science.

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