2013
DOI: 10.1175/jcli-d-12-00819.1
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On the Connection between Continental-Scale Land Surface Processes and the Tropical Climate in a Coupled Ocean–Atmosphere–Land System

Abstract: An evaluation is presented of the impact on tropical climate of continental-scale perturbations given by different representations of land surface processes (LSPs) in a general circulation model that includes atmosphere–ocean interactions. One representation is a simple land scheme, which specifies climatological albedos and soil moisture availability. The other representation is the more comprehensive Simplified Simple Biosphere Model, which allows for interactive soil moisture and vegetation biophysical proc… Show more

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Cited by 9 publications
(5 citation statements)
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“…(e.g., Zeng et al 1999;Xue et al 2004bXue et al , 2010bKoster et al 2004;Ma et al 2013). The SST effects considered in this paper include the land surface biogeophysical and soil moisture effects as presented in our discussions on surface water and energy balances (Figs.…”
Section: Discussionmentioning
confidence: 99%
“…(e.g., Zeng et al 1999;Xue et al 2004bXue et al , 2010bKoster et al 2004;Ma et al 2013). The SST effects considered in this paper include the land surface biogeophysical and soil moisture effects as presented in our discussions on surface water and energy balances (Figs.…”
Section: Discussionmentioning
confidence: 99%
“…Sea surface temperature has been shown to be a major controller in the Sahel's inter-annual and seasonal precipitation variability, with feedbacks due to changes in surface albedo acting more as an amplifier of ocean driven variability than an initial trigger of monsoon variability (Giannini et al 2003). Nonetheless, the role of land/atmosphere interaction on the Sahel climate has been confirmed by several climate modeling studies (e.g., Xue 1997;Clark et al 2001;Li et al 2007;Xue et al 2010a;Ma et al 2013).…”
Section: Introductionmentioning
confidence: 91%
“…Surface freshwater fluxes are applied as virtual salt fluxes and heat and freshwater fluxes are exchanged between the ocean and the atmosphere at an interval of 1 day. The AOGCM has been used in several studies on climate variability in addition to SEA11 (Mechoso et al 2003;Cazes-Boezio et al 2008;Ma et al 2013) and in decadal climate prediction (Polkova et al 2014).…”
Section: A the Aogcmmentioning
confidence: 99%