Understanding Hydrometeorology Using Global Models

By A. Betts. 2004

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Role of continental recycling in intraseasonal variations of continental moisture as deduced from model simulations and water vapor isotopic measurements (2013, background): “Local feedbacks can also involve small-scale soil moisture gradients and associated mesoscale circulations [Taylor et al., 2007, 2009, 2011] and radiative effects of clouds [Sch€ar et al., 1999; Betts, 2004; Schlemmer et al., 2011, 2012].”
Land‐Surface‐Atmosphere Coupling in Observations and Models (2009, methodology): “Betts (2004) picked up this theme of soil moisture interactions, and addressed the issue of ‘‘Understanding hydrometeorology using global models’’ by mapping the coupling between different processes and observables at the land surface, using daily mean data from ERA-40.”
Late-summer carbon fluxes from Canadian forests and peatlands along an east-west continental transect (2006, background): “6) indicate the potential for significant feedback of disturbance on water flux to the planetary boundary layer, with consequent effects on cloud dynamics (Betts 2004).”