Pertaining to Lab 3 Q14, why is the peak net radiation approximately the same on the two dates seen in figures 3-5 and 3-6? The weather conditions must have been the same on those dates (i.e. clouds, pressure, temperature, etc.) The data for both days must have been taken on surfaces with the same albedo Botswana is right on the equator so it has very little variation throughout the year The latent heat, sensible, heat, and soil fluxes when averaged together are about the same on both days The sun angles are similar on both dates Surplus net radiation at the surface can be expendedin three general ways:sensible heat flux to the atmosphere (energyexpended in heating the air at Earth's surface),soil heat flux (energy expended in heating thesoil)latent heat flux (energy used in evaporatingmoisture from the surface).Figures 3-5 and 3-6 show the net surface radiationat Maun on March 19, 2000, and September 24, 2000,respectively.800-Net radiation600-400-200-Soil flux0-Sensibleheat-200--400Energy (watts per square meter)00:00Latentheat- 00:9012:00-- 00:81- 00:00March 19Figure 3-5. Net surface radiation-Maun, Botswana,March 19, 2000.Lab 3 The Surface Energy Budget14. Why is the peak net radiation approximately the sameon the two dates?15. How does the net surface radiation pattern differbetween the two dates during daylight hours?800600-400-200Energy (watts per square meter)0--200--400-Latentheat- 00:00- 00:9012:00Net radiationobbSoil flux- 00:8Sensibleheat- 00:00September 24Figure 3-6. Net surface radiation-Maun, Botswana,September 24, 2000.31

The amount of solar radiation reaching the earth surface is directly proportional to the incident…

Answered: Pertaining to Lab 3 Q14, why is the…

Elements Of Electromagnetics

7th Edition

ISBN:9780190698614

Author:Sadiku, Matthew N. O.

Publisher:Sadiku, Matthew N. O.

ChapterMA: Math Assessment

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Pertaining to Lab 3 Q14, why is the peak net radiation approximately the same on the two dates seen in figures 3-5 and 3-6?

		The weather conditions must have been the same on those dates (i.e. clouds, pressure, temperature, etc.)
		The data for both days must have been taken on surfaces with the same albedo
		Botswana is right on the equator so it has very little variation throughout the year
		The latent heat, sensible, heat, and soil fluxes when averaged together are about the same on both days
		The sun angles are similar on both dates

Surplus net radiation at the surface can be expended
in three general ways:
sensible heat flux to the atmosphere (energy
expended in heating the air at Earth's surface),
soil heat flux (energy expended in heating the
soil)
latent heat flux (energy used in evaporating
moisture from the surface).
Figures 3-5 and 3-6 show the net surface radiation
at Maun on March 19, 2000, and September 24, 2000,
respectively.
800-
Net radiation
600-
400-
200-
Soil flux
0-
Sensible
heat
-200-
-400
Energy (watts per square meter)
00:00
Latent
heat
- 00:90
12:00-
- 00:81
- 00:00
March 19
Figure 3-5. Net surface radiation-Maun, Botswana,
March 19, 2000.
Lab 3 The Surface Energy Budget
14. Why is the peak net radiation approximately the same
on the two dates?
15. How does the net surface radiation pattern differ
between the two dates during daylight hours?
800
600-
400-
200
Energy (watts per square meter)
0-
-200-
-400-
Latent
heat
- 00:00
- 00:90
12:00
Net radiationobb
Soil flux
- 00:8
Sensible
heat
- 00:00
September 24
Figure 3-6. Net surface radiation-Maun, Botswana,
September 24, 2000.
31

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