Remember that Q* = QH + Qe + Qg. A curious thing can be seen in these graphed data. Mirny's latent heat flux (Qe) is greater than the available radiation (Q*). The sensible heat flux (Qr) is also greater than Q* during Mirny's winter. Explain where this sensible and latent heat comes from when Q* is negative. (Hint: think about global circulation of energy).
Remember that Q* = QH + Qe + Qg. A curious thing can be seen in these graphed data. Mirny's latent heat flux (Qe) is greater than the available radiation (Q*). The sensible heat flux (Qr) is also greater than Q* during Mirny's winter. Explain where this sensible and latent heat comes from when Q* is negative. (Hint: think about global circulation of energy).
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
Related questions
Question
Remember that Q* = QH + Qe + Qg. A curious thing can be seen in these graphed data. Mirny's latent heat flux
(Qe) is greater than the available radiation (Q*). The sensible heat flux (Qr) is also greater than Q* during Mirny's winter. Explain where this sensible and latent heat comes from when Q* is negative. (Hint: think about global circulation of energy).

Transcribed Image Text:Energy Flux Density (Wm-²)
Energy Flux Density (W m2)
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SHERATORER÷2÷¤
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Surface Energy Balance for Vancouver, BC, 49.16°N, 123.06°W
J F M A
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M
t.
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J
Time (Month)
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Surface Energy Budget for Mirny, Antarctica, 66.5°S, 90°E
Month
Q*
----- QE
<--QH
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that
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S O N D
Q
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F M A M J J A S O N D
Energy Flux Density (Wm²)
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Surface Energy Budget for Yuma, Arizona, 32.4°N, 114.4°W
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Energy Flux Density (W m2)
MA
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8 8 8 8
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Surface Energy Budget for Sao Gabriel da Cachoera, Brazil,
0.13°S, 67.08 W
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