NCERT Solutions Class 11 Geography Chapter 9 Solar Radiation Heat Balance and Temperature have been provided below and is also available in Pdf for free download. The NCERT solutions for Class 11 Geography have been prepared as per the latest syllabus, NCERT books and examination pattern suggested in Class 11 by CBSE, NCERT and KVS. Questions given in NCERT book for Class 11 Geography are an important part of exams for Class 11 Geography and if answered properly can help you to get higher marks. Refer to more Chapter-wise answers for NCERT Class 11 Geography and also download more latest study material for all subjects. Chapter 9 Solar Radiation Heat Balance and Temperature is an important topic in Class 11, please refer to answers provided below to help you score better in exams
Chapter 9 Solar Radiation Heat Balance and Temperature Class 11 Geography NCERT Solutions
Class 11 Geography students should refer to the following NCERT questions with answers for Chapter 9 Solar Radiation Heat Balance and Temperature in Class 11. These NCERT Solutions with answers for Class 11 Geography will come in exams and help you to score good marks
Chapter 9 Solar Radiation Heat Balance and Temperature NCERT Solutions Class 11 Geography
NCERT Solution for Class 11 Geography for chapter 9 Solar Radiation Heat Balance and Temperature
1. Multiple choice question
(i) The sun is directly overhead at noon on 21st June at:
(a) The equator
(b) 23.5° S
(c) 23.5° N
(d) 66.5° N
Answer: (c) 23.5° N
(ii) In which one of the following cities, are the days the longest?
(a) Tiruvanantpuram
(b) Chandigarh
(c) Hyderabad
(d) Nagpur
Answer: (b) Chandigarh
(iii) The atmosphere is mainly heated by the:
(a) Short wave solar radiation
(b) Reflected solar radiation
(c) Long wave terrestrial radiation
(d) Scattered solar radiation
Answer: (c) Long wave terrestrial radiation
(iv) Make correct pairs from the following two columns.
(i) Insolation |
(a) The difference between the mean temperature of the warmest and the coldest months |
(ii) Albedo |
(b) The lines joining the places of equal temperature |
(iii) Isotherm |
(c) The incoming solar radiation |
(iv) Annual range |
(d) The percentage of visible light reflected by an object |
Answer:
(i) Insolation |
(c) The incoming solar radiation |
(ii) Albedo |
(d) The percentage of visible light reflected by an object |
(iii) Isotherm |
(b) The lines joining the places of equal temperature |
(iv) Annual range |
(a) The difference between the mean temperature of the warmest and the coldest months |
(v) The main reason that the earth experiences highest temperatures in the subtropics in the northern hemisphere rather than at the equator is:
(a) Subtropical areas tend to have less cloud cover than equatorial areas.
(b) Subtropical areas have longer day hours in the summer than the equatorial.
(c) Subtropical areas have an enhanced “green house effect” compared to equatorial areas.
(d) Subtropical areas are nearer to the oceanic areas than the equatorial locations.
Answer: (a) Subtropical areas tend to have less cloud cover than equatorial areas.
2. Answer the following questions in about 30 words
(i) How does the unequal distribution of heat over the planet earth in space and time cause variations in weather and climate?
Answer: Equator receives comparatively less insolation than the tropics. Generally, at the same latitude the insolation is more over the continent than over the oceans. In winter, the middle and higher latitudes receive less radiation than in summer. Places near the equator are much hotter than those located near the poles. Summers are always hotter than winters. Therefore, the unequal distribution of heat over the earth in space and time cause large-scale variations in weather and climate.
(ii) What are the factors that control temperature distribution on the surface of the earth?
Answer: The factors that control temperature distribution on the surface of the earth are latitude or distance from equator, height from sea level, distance from Ocean, ocean currents, prevailing winds, angle of slope, nature of land, rainfall, etc.
(iii) In India, why is the day temperature maximum in May and why not after the summer solstice?
Answer: In India, the maximum day temperature is recorded in the first week of May. In June, the southwest monsoons arrive at the Kerala coast and advance further inland in June and July. These southwest moisture laden monsoon winds have cooling effect therefore; summer solstice in June is cooler than May.
(iv) Why is the annual range of temperature high in the Siberian plains?
Answer: Siberian plains in Russia have continental climate because it is located far from the ocean and equalising effect of sea/ocean is least. Therefore, annual range of temperature is high in the Siberian plains.
3. Answer the following questions in about 150 words
(i) How do the latitude and the tilt in the axis of rotation of the earth affect the amount of radiation received at the earth’s surface?
Answer: The earth's axis makes an angle of 66.5° with the plane of its orbit round the sun has a greater influence on the amount of isolation received at different latitudes. In June, the Northern Hemisphere is inclined towards the sun and receives more solar radiation than the Southern Hemisphere. In December, the Southern Hemisphere is inclined towards the sun and receives more solar radiation than the Northern Hemisphere. Latitude also makes a difference in the amount of solar radiation received on the earth. The sun's rays are almost vertical near the equator for most part of the year and they are inclined at the poles. Therefore, the places near the equator receive more solar radiation than those located near the poles.
(ii) Discuss the processes through which the earth- atmosphere system maintains heat balance.
Answer: The sun's rays are almost vertical at the equator and oblique towards the poles. Therefore, the incoming solar radiation is maximum at the equator and it decreases towards the poles. There are variations in the amount of radiation received at the earth’s surface. Up to 38° north and south latitudes, the incoming solar radiation are greater than the outgoing terrestrial radiation. Therefore, the tropics should have been getting progressively hotter and the poles getting progressively cooler. However, this is not so. The atmosphere and the oceans act as giant thermal engines that transfer heat from the tropics towards the poles. Due to imbalance of heat, winds and ocean currents are produced. Thus, the transfer of surplus energy from the lower latitudes to the deficit energy zone of the higher latitudes maintains an overall balance over the earth's surface. This is termed as the heat budget or heat balance of the earth.
(iii) Compare the global distribution of temperature in January over the northern and the southern hemisphere of the earth.
Answer: Global Distribution of Temperature in January: The sun shines almost vertically over Tropic of Capricorn in the southern hemisphere in the month of January. It is summer in the southern hemisphere and winter in the northern hemisphere. There is high temperature over the land mass in the southern hemisphere. The temperature rising over 30°C in north- west Argentina, east-central Africa, Borneo and Central Australia. In the same time, the landmasses in the northern hemisphere are cooler than the oceans. The northeast Asia, northern part of North America and Europe, and Greenland received lowest temperature. Verkhoyansk in Siberian Russia experiences mean January temperature of -50°C. The air over the ocean is warmer than that over the landmasses in the northern hemisphere. The isotherms bend toward equator while crossing the landmasses and toward pole while crossing the oceans. In the southern hemisphere, the isotherms bend toward equator while crossing the oceans and toward pole while crossing the landmasses. Isotherms are irregular and closely spaced in the northern hemisphere, due to the presence of vast expanse of landmasses. However, isotherms are more widely spaced in the southern hemisphere in the month of January.
NCERT Solutions Class 11 Geography Chapter 1 Geography as a Discipline |
NCERT Solutions Class 11 Geography Chapter 2 The Origin and Evolution of the Earth |
NCERT Solutions Class 11 Geography Chapter 3 Interior of the Earth |
NCERT Solutions Class 11 Geography Chapter 4 Distribution of the Oceans and Continents |
NCERT Solutions Class 11 Geography Chapter 5 Minerals and Rocks |
NCERT Solutions Class 11 Geography Chapter 6 Geomorphic processes |
NCERT Solutions Class 11 Geography Chapter 7 Landforms and their Evolution |
NCERT Solutions Class 11 Geography Chapter 8 Composition and Structure of Atmosphere |
NCERT Solutions Class 11 Geography Chapter 9 Solar Radiation Heat Balance and Temperature |
NCERT Solutions Class 11 Geography Chapter 10 Atmospheric circulation and weather Systems |
NCERT Solutions Class 11 Geography Chapter 11 Water in the Atmosphere |
NCERT Solutions Class 11 Geography Chapter 12 World Climate and Climate Change |
NCERT Solutions Class 11 Geography Chapter 13 Water Oceans |
NCERT Solutions Class 11 Geography Chapter 14 Movements of Ocean Water |
NCERT Solutions Class 11 Geography Chapter 15 Life on the Earth |
NCERT Solutions Class 11 Geography Chapter 16 Biodiversity and Conservation |
NCERT Solutions Class 11 Geography Chapter 1 India Location |
NCERT Solutions Class 11 Geography Chapter 2 Structure and Physiography |
NCERT Solutions Class 11 Geography Chapter 3 Drainage System |
NCERT Solutions Class 11 Geography Chapter 4 Climate |
NCERT Solutions Class 11 Geography Chapter 5 Natural Vegetation |
NCERT Solutions Class 11 Geography Chapter 6 Soils |
NCERT Solutions Class 11 Geography Chapter 7 Natural Hazards and Disasters |
NCERT Solutions Class 11 Geography Chapter 1 Introduction to Maps |
NCERT Solutions Class 11 Geography Chapter 2 Map Scale |
NCERT Solutions Class 11 Geography Chapter 3 Latitude Longitude and Time |
NCERT Solutions Class 11 Geography Chapter 4 Map Projections |
NCERT Solutions Class 11 Geography Chapter 5 Topographical Maps |
NCERT Solutions Class 11 Geography Chapter 6 Introduction to Aerial Photographs |
NCERT Solutions Class 11 Geography Chapter 7 Introduction to Remote Sensing |
NCERT Solutions Class 11 Geography Chapter 8 Weather Instruments Maps and Charts |
NCERT Solutions Class 11 Geography Chapter 9 Solar Radiation Heat Balance and Temperature
The above provided NCERT Solutions Class 11 Geography Chapter 9 Solar Radiation Heat Balance and Temperature is available on our website www.studiestoday.com for free download in Pdf. You can read the solutions to all questions given in your Class 11 Geography textbook online or you can easily download them in pdf. The answers to each question in Chapter 9 Solar Radiation Heat Balance and Temperature of Geography Class 11 has been designed based on the latest syllabus released for the current year. We have also provided detailed explanations for all difficult topics in Chapter 9 Solar Radiation Heat Balance and Temperature Class 11 chapter of Geography so that it can be easier for students to understand all answers. These solutions of Chapter 9 Solar Radiation Heat Balance and Temperature NCERT Questions given in your textbook for Class 11 Geography have been designed to help students understand the difficult topics of Geography in an easy manner. These will also help to build a strong foundation in the Geography. There is a combination of theoretical and practical questions relating to all chapters in Geography to check the overall learning of the students of Class 11.
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