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2 Application of Heat Flux Balance 4P A 1000 m thick boundary layer is warmed from 10° C to 20° C within 6 h. How large is the heat flux near the ground (at the surface) if no heat flux occurs through the upper boundary of the boundary layer? Note: Use the vertical integral of the equation from la in exercise sheet #4 and show that the relation 1 Ztop 20 Ztop aw'' Əz w' Ꮎ' . "top - W'0' surface-layer dz Ztop Zo 20 is a reasonable estimation of the relationship between the warming rate of the boundary layer and the integral flux divergence. Discuss the assumptions made here and under what circumstances you consider them reasonable.

2 Application of Heat Flux Balance 4P A 1000 m thick boundary layer is warmed from 10° C to 20° C within 6 h. How large is the heat flux near the ground (at the surface) if no heat flux occurs through the upper boundary of the boundary layer? Note: Use the vertical integral of the equation from la in exercise sheet #4 and show that the relation 1 Ztop 20 Ztop aw'' Əz w' Ꮎ' . "top - W'0' surface-layer dz Ztop Zo 20 is a reasonable estimation of the relationship between the warming rate of the boundary layer and the integral flux divergence. Discuss the assumptions made here and under what circumstances you consider them reasonable.

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
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2 Application of Heat Flux Balance 4P A 1000 m thick boundary layer is warmed from 10° C to 20° C within 6 h. How large is the heat flux near the ground (at the surface) if no heat flux occurs through the upper boundary of the boundary layer? Note: Use the vertical integral of the equation from la in exercise sheet #4 and show that the relation 1 Ztop 20 Ztop aw'' Əz w' Ꮎ' . "top - W'0' surface-layer dz Ztop Zo 20 is a reasonable estimation of the relationship between the warming rate of the boundary layer and the integral flux divergence. Discuss the assumptions made here and under what circumstances you consider them reasonable.
Transcribed Image Text:2 Application of Heat Flux Balance 4P A 1000 m thick boundary layer is warmed from 10° C to 20° C within 6 h. How large is the heat flux near the ground (at the surface) if no heat flux occurs through the upper boundary of the boundary layer? Note: Use the vertical integral of the equation from la in exercise sheet #4 and show that the relation 1 Ztop 20 Ztop aw'' Əz w' Ꮎ' . "top - W'0' surface-layer dz Ztop Zo 20 is a reasonable estimation of the relationship between the warming rate of the boundary layer and the integral flux divergence. Discuss the assumptions made here and under what circumstances you consider them reasonable.
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