Abstract
This paper studies the sensitivity of large-scale tropical convection to land surface changes in the general circulation model of the LMD. The method of analysis is based on a conceptual model of the energetics of convection applied every day of the simulation to the grid points within the region of interest. The synoptic events are then classified by their potential energy divergence. This allows for the distinction between the frequency and the characteristic energy and water cycle of the events. The difference in precipitation found in the tropical deforestation experiments is explained by changes in the number of intense convective events while their characteristic precipitation remains largely unchanged. With a series of ten deforestation experiments the relation between land surface processes changes and variations of the frequency of convection is studied. -from Author
| Original language | English |
|---|---|
| Pages (from-to) | 3143-3161 |
| Number of pages | 19 |
| Journal | Journal of the Atmospheric Sciences |
| Volume | 52 |
| Issue number | 17 |
| DOIs | |
| Publication status | Published - 1 Jan 1995 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 15 Life on Land
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