The GFS_Noah has been incorporated into the framework of the NCEP GDAS in early 2003. A retroactive data assimilation run starting from 1 Aug 2002 is in progress. The Noah cycled GDAS run employs reduced resolution (T62 L28) with respect to the operational run (T254 L64). A low-resolution GDAS run using the operational version of GFS (with old LSM) is run in parallel with the Noah cycled GDAS run. These data assimilation efforts aim to evaluate the impact of LSM upgrade on GFS forecasts as well as to provide continuously cycled Noah LSM land states in GDAS.
In this study, the GFS_Noah is used for warm-season seasonal hindcasts for 2003. Initial conditions are taken from: (1) low resolution GDAS using the operational version of GFS, and (2) low resolution GDAS using the GFS_Noah. The length of integration is 3 months, starting from late spring/early summer. The ocean surface boundary fields are from observed 1-deg NCEP Reyolds/Stokes SST. Results from two sets of GFS_Noah summer time integrations are analyzed and compared against observed near-surface temperature from CPC 344 Climate Division data and precipitation fields from CPC gauge date. The impact of using Noah cycled GDAS (which provide initial land states that are strictly self consistent with GFS_Noah land physics) on warm season predictions is assessed.
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