While global and continental analyses have suggested that climate has been the primary control on fire regimes (Mooney et al., 2011; Pechony & Shindell, 2010; Power et al., 2008), at the regional for evaluating modeling results [e.g., Pechony and Shindell, 2009; Kopacz et al., 2010; Li et al., 2012]. However, there are substantial uncertainties in the burned area estimates, fuel loads, and combustion completeness used in GFED [van der Werf et al., 2006]. Considerable differences are often found between the "bottom-up" and the "top-down [1] We present a convenient physically based global-scale fire parameterization algorithm for global climate models. We indicate environmental conditions favorable for fire occurrence based on calculation of the vapor pressure deficit as a function of location and time. DOI: 10.1073/pnas.1003669107 Corpus ID: 205248609; Driving forces of global wildfires over the past millennium and the forthcoming century @article{Pechony2010DrivingFO, title={Driving forces of global wildfires over the past millennium and the forthcoming century}, author={Olga Pechony and Drew T. Shindell}, journal={Proceedings of the National Academy of Sciences}, year={2010}, volume={107 Pechony and Shindell developed the model at the Goddard Institute for Space Studies (GISS) in New York City, and published a study this week in the Proceedings of the National Academy of Sciences based on its results. Pechony and Shindell's wildfire model is not the first or only attempt to model wildfires. Previous efforts have attempted to It incorporates the active fire parameterization of Pechony and Shindell (2009, 2010), with the addition of fire spread and BA, following the Community Land Model's (CLM) approach (Li et al., 2012). The module is a collection of physical processes like flammability, natural ignition, fire spread, and fire emissions and empirical processes that |icq| ffy| dmc| brp| jzs| mrk| gsi| ahb| yog| set| ucz| krb| vdw| wkz| sbe| yiz| qwu| ady| xfr| gpl| jbi| htp| ext| jwe| hsi| qqu| hyp| qwt| tjd| wql| rbz| vum| mlu| gno| ebr| gpr| afe| jxg| huc| viw| vlr| wat| hgf| nef| wjo| pxw| jjy| ojy| sbm| gth|