5. The figure below shows the solar insolation at the top of the atmosphere and at the earth's surface on June 21 from the equator to the north pole. Discuss why the top of the atmosphere at the north poles appears to receive more solar radiation than the top of the atmosphere at the equator, and despite the high insolation at the top of the atmosphere at the north pole, the surface at the north pole appears to receive much less radiation than other latitudes. Top of atmosphere Earth's surface 15 30 45 60 75 90 Equator Latitude (°N) North Pole Insolation
5. The figure below shows the solar insolation at the top of the atmosphere and at the earth's surface on June 21 from the equator to the north pole. Discuss why the top of the atmosphere at the north poles appears to receive more solar radiation than the top of the atmosphere at the equator, and despite the high insolation at the top of the atmosphere at the north pole, the surface at the north pole appears to receive much less radiation than other latitudes. Top of atmosphere Earth's surface 15 30 45 60 75 90 Equator Latitude (°N) North Pole Insolation
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Transcribed Image Text:Lab 3: Insolation & Seasons
ESC205: Principles of Meteorology
5. The figure below shows the solar insolation at the top of the atmosphere and at the earth's
surface on June 21 from the equator to the north pole. Discuss why the top of the
atmosphere at the north poles appears to receive more solar radiation than the top of the
atmosphere at the equator, and despite the high insolation at the top of the atmosphere at
the north pole, the surface at the north pole appears to receive much less radiation than
other latitudes.
Top of atmosphere
Earth's surface
15
30
45
60
75
90
Equator
Latitude (°N)
North Pole
Insolation
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