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English: Interactions between the carbon (green), water (blue) and heat (red) cycles in the coupled land–ABL system. Increased subsidence tends to reduce the boundary-layer height, which directly causes the ABL to warm up, dry and become CO2 -depleted. This in turn affects the land-surface, which feeds back on the ABL by shifting its Bowen ratio towards more evapotranspiration.
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M. Combe et. al. "Two perspectives on the coupled carbon, water and energy exchange in the planetary boundary layer", Biogeosciences doi:10.5194/bg-12-103-2015
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M. Combe, J. Vilà-Guerau de Arellano, H. G. Ouwersloot, C. M. J. Jacobs, W. Peters
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8 January 2015
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