Tuesday, 15 January 2002
Assessment of implementing satellite-derived land cover data in the Eta model
Nicole P. Kurkowski, University of Oklahoma and NOAA/NSSL, Norman, OK; and D. J. Stensrud
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One of the challenges in land surface modeling involves specifying accurately the initial state of the land surface. Most efforts have focused upon using multi-year climatologies to specify the fractional coverage of vegetation. For example, the National Center for Environmental Prediction (NCEP) Eta model uses a a five-year satellite climatology of monthly Normalized Difference Vegetation Index (NDVI) values to define the fractional vegetation coverage, or greenness, at 1/8 degree resolution.
These data are valid on the 15th of every month and are interpolated temporally for daily runs. Yet vegetation characteristics change from year-to-year and are influenced by short-lived events such as fires, crop harvesting, and hailstorms that will be missed using a climatological data
base.
To explore the importance of the initial state vegetation characteristics to numerical weather forecasts, we examine how the Eta model responds to a different method of initializing fractional vegetation coverage. Studies have shown that several vegetation metrics can be estimated from bi-weekly, 1-km resolution NDVI maximum-value composites derived from NOAA's Advanced Very High Resolution Radiometer (AVHRR). This approach may allow for near real-time estimations of fractional vegetation coverage to be used. Several numerical forecasts of the Eta model, using both climatological and near real-time values of fractional vegetation coverage, are compared to examine the potential importance of variations in vegetation to forecasts of 2 m temperatures and surface fluxes.
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