UPSC  >  Geography for UPSC CSE  >  Test: Solar Radiation, Heat Balance & Temperature - 1 Download as PDF

Test: Solar Radiation, Heat Balance & Temperature - 1


Test Description

10 Questions MCQ Test Geography for UPSC CSE | Test: Solar Radiation, Heat Balance & Temperature - 1

Test: Solar Radiation, Heat Balance & Temperature - 1 for UPSC 2022 is part of Geography for UPSC CSE preparation. The Test: Solar Radiation, Heat Balance & Temperature - 1 questions and answers have been prepared according to the UPSC exam syllabus.The Test: Solar Radiation, Heat Balance & Temperature - 1 MCQs are made for UPSC 2022 Exam. Find important definitions, questions, notes, meanings, examples, exercises, MCQs and online tests for Test: Solar Radiation, Heat Balance & Temperature - 1 below.
Solutions of Test: Solar Radiation, Heat Balance & Temperature - 1 questions in English are available as part of our Geography for UPSC CSE for UPSC & Test: Solar Radiation, Heat Balance & Temperature - 1 solutions in Hindi for Geography for UPSC CSE course. Download more important topics, notes, lectures and mock test series for UPSC Exam by signing up for free. Attempt Test: Solar Radiation, Heat Balance & Temperature - 1 | 10 questions in 10 minutes | Mock test for UPSC preparation | Free important questions MCQ to study Geography for UPSC CSE for UPSC Exam | Download free PDF with solutions
1 Crore+ students have signed up on EduRev. Have you?
Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 1

Higher latitudes are not permanently frozen because of

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 1

There is a surplus of net radiation balance between 40 degrees north and south and the regions near the poles have a deficit. The surplus heat energy from the tropics is redistributed pole wards and as a result the tropics do not get progressively heated up due to the accumulation of excess heat or the high latitudes get permanently frozen due to excess deficit.

Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 2

The heat energy absorbed by a known area in a fixed time is determined with the help of an instrument called

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 2

The effects of absorption by the atmosphere are eliminated by finding the value of the solar constant at various altitudes of the sun on the same day.

Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 3

The earth radiates energy to the atmosphere in:

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 3

This energy heats up the atmosphere from below.

Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 4

In which one of the following cities, are the days the longest in Summar?

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 4

In summer (March to September), in the northern hemisphere, as we move northwards, the length of the day increases. But in winter (September to March) the length of the night increases as we move northwards. since Chandigarh is northernmost among the options

Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 5

Insolation refers to ________

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 5

The energy received by the earth is known as incoming solar radiation, which in short is termed as insolation.

Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 6

The envelop of the air is called _________

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 6

Atmosphere is a mixture of different gases and it envelopes the earth all round. It contains life-giving gases like oxygen for humans and animals and carbon dioxide for plants.

Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 7

Differences in pressure on the earth surface causes:

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 7

Pressure differences cause winds.

Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 8

The sun is vertically over head at noon on 21st June at

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 8

The sun can be directly overhead on June 21st when it is at the Tropic of Cancer, which is 23.5 degrees north of the equator. Similarly, the sun is only directly overhead at the winters solstice for locations on the Tropic of Capricorn, 23.5 degrees south of the equator. On the euqinoxes, both spring and autumn, the sun is only directly overhead at the equator.

Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 9

Maximum insolation is received over the ____________

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 9

Sub-tropical deserts receive maximum amount of insolation because cloudiness is the least there.

Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 10

What is Isotherm?

Detailed Solution for Test: Solar Radiation, Heat Balance & Temperature - 1 - Question 10

Isotherms are the lines joining places of equal temperature.

161 videos|466 docs|207 tests
Use Code STAYHOME200 and get INR 200 additional OFF
Use Coupon Code
Information about Test: Solar Radiation, Heat Balance & Temperature - 1 Page
In this test you can find the Exam questions for Test: Solar Radiation, Heat Balance & Temperature - 1 solved & explained in the simplest way possible. Besides giving Questions and answers for Test: Solar Radiation, Heat Balance & Temperature - 1, EduRev gives you an ample number of Online tests for practice