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John E. Janowiak, Peter Bauer, Wanqiu Wang, Phillip A. Arkin, and Jon Gottschalck

to include the latest improvements for the model physics and analysis algorithms and to assimilate new observations to produce the best initial conditions. (Changes to the GFS and GDAS during the past years are documented online at http://www.emc.ncep.noaa.gov/gmb/STATS/html/model_changes.html .) The GFS is integrated at T382 horizontal resolution (∼35-km grid) for the first 180 h, after which a T190 resolution (∼70-km grid) is used. Sea surface temperatures (SSTs) in the GFS are represented as

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Benoît Vié, Olivier Nuissier, and Véronique Ducrocq

on the nonhydrostatic version of the adiabatic equations of the limited-area model Aire Limitée Adaptation Dynamique Développement International (ALADIN; Benard 2004 ; Bubnova et al. 1995 ), using physical parameterizations from the research model Méso-NH ( Lafore et al. 1998 ). The bulk microphysics scheme following Caniaux et al. (1994) governs the prognostic equations of the six water variables: water vapor, cloud water, rainwater, primary ice, graupel, and snow. Shallow convection is

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