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    Soil Moisture–Atmosphere Interaction in a Moist Semigeostrophic Model of Baroclinic Instability 

    Source: Journal of the Atmospheric Sciences:;1995:;Volume( 052 ):;issue: 011:;page 2152
    Author(s): Castelli, Fabio; Rodriguez-Iturbe, Ignacio
    Publisher: American Meteorological Society
    Abstract: Attention is focused on the dynamical coupling between the soil moisture and atmospheric processes, such as in the presence of a growing moist baroclinic wave. A simplified scheme, representing the mass and energy exchanges ...
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    Vegetation Dynamics within the North American Monsoon Region 

    Source: Journal of Climate:;2010:;volume( 024 ):;issue: 006:;page 1763
    Author(s): Forzieri, Giovanni; Castelli, Fabio; Vivoni, Enrique R.
    Publisher: American Meteorological Society
    Abstract: The North American monsoon (NAM) leads to a large increase in summer rainfall and a seasonal change in vegetation in the southwestern United States and northwestern Mexico. Understanding the interactions between NAM rainfall ...
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    Estimation of Surface Turbulent Fluxes through Assimilation of Radiometric Surface Temperature Sequences 

    Source: Journal of Hydrometeorology:;2004:;Volume( 005 ):;issue: 001:;page 145
    Author(s): Caparrini, Francesca; Castelli, Fabio; Entekhabi, Dara
    Publisher: American Meteorological Society
    Abstract: A model of land surface energy balance is used as a constraint on the estimation of factors characterizing land surface influences on evaporation and turbulent heat transfer from sequences of radiometric surface temperature ...
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    An Analytical Approach to the Nonlinear Dynamics of Moist Frontogenesis 

    Source: Journal of the Atmospheric Sciences:;1993:;Volume( 050 ):;issue: 011:;page 1504
    Author(s): Castelli, Fabio; Bras, Rafael L.; Emanuel, Kerry A.
    Publisher: American Meteorological Society
    Abstract: The existence of analytical solutions for two-dimensional nonlinear semigeostrophic models of moist frontogenesis is investigated. Two different schemes for the modeling of stratiform cloud thermodynamics are taken into ...
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