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Why is the ground heat flux (QG) so much smaller in magnitude than the other fluxes?

Why is the ground heat flux (QG) so much smaller in magnitude than the other fluxes?

Applications and Investigations in Earth Science (9th Edition)
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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Why is the ground heat flux (QG) so much smaller in magnitude than the other fluxes? 

 

Energy Flux Density (Wm-²) Energy Flux Density (W m2) 160 150 140 130 120 110 100 90 80 70 60 50 40 30 20 10 0 -10 -20 -30 -40 SHERATORER÷2÷¤ 160 150 140 130 120 110 100 90 80 70 60 50 40 30 20 10 0 -10 -20 -30 -40 Surface Energy Balance for Vancouver, BC, 49.16°N, 123.06°W J F M A J M t. 1-14 J Time (Month) J A Surface Energy Budget for Mirny, Antarctica, 66.5°S, 90°E Month Q* ----- QE <--QH 10 that QG S O N D Q QE QH F M A M J J A S O N D Energy Flux Density (Wm²) 160 150 140 130 120 110 100 90 80 70 60 50 40 30 20 10 0 -10 -20 -30 -40 Surface Energy Budget for Yuma, Arizona, 32.4°N, 114.4°W J LL F Energy Flux Density (W m2) MA 160 150 140 130 120 110 100 90 80 70 60 50 8 8 8 8 10 0 10 20 Surface Energy Budget for Sao Gabriel da Cachoera, Brazil, 0.13°S, 67.08 W 30 40 M - J F J M J A A Time (Month) A 2 3 Month S J Q* A QE QH QG ON D Q QE <--QH S O N D
Transcribed Image Text:Energy Flux Density (Wm-²) Energy Flux Density (W m2) 160 150 140 130 120 110 100 90 80 70 60 50 40 30 20 10 0 -10 -20 -30 -40 SHERATORER÷2÷¤ 160 150 140 130 120 110 100 90 80 70 60 50 40 30 20 10 0 -10 -20 -30 -40 Surface Energy Balance for Vancouver, BC, 49.16°N, 123.06°W J F M A J M t. 1-14 J Time (Month) J A Surface Energy Budget for Mirny, Antarctica, 66.5°S, 90°E Month Q* ----- QE <--QH 10 that QG S O N D Q QE QH F M A M J J A S O N D Energy Flux Density (Wm²) 160 150 140 130 120 110 100 90 80 70 60 50 40 30 20 10 0 -10 -20 -30 -40 Surface Energy Budget for Yuma, Arizona, 32.4°N, 114.4°W J LL F Energy Flux Density (W m2) MA 160 150 140 130 120 110 100 90 80 70 60 50 8 8 8 8 10 0 10 20 Surface Energy Budget for Sao Gabriel da Cachoera, Brazil, 0.13°S, 67.08 W 30 40 M - J F J M J A A Time (Month) A 2 3 Month S J Q* A QE QH QG ON D Q QE <--QH S O N D
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