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In order to better understand the effects that mesoscale transport has on atmospheric CO 2 distributions, we have used the atmospheric WRF model coupled to the diagnostic biospheric model VPRM, which provides high resolution biospheric CO 2 fluxes based on MODIS satellite indices. We have run WRF-VPRM for the period from 16 May to 15 June in 2005 covering the intensive period of the CERES experiment, using the CO 2 fields from the global model LMDZ for initialization and lateral boundarydoi:10.5194/bg-6-807-2009 fatcat:43xdyjevtzbbhj4cfkj67hzr3e