RAWS observations from the 2003-2004 winter season have been used in a data denial study to assess their impact on surface temperature and wind speed analyses over the western United States. The surface objective analyses were created using the ARPS Data Assimilation System (ADAS). A set of control analyses were created each day at 0000 and 1200 UTC by assimilating in ADAS all available observations (approximately 4000 observations from MesoWest). Analyses were also generated withholding all of the RAWS observations. In addition, 10 additional sets of analyses were generated by randomly withholding 1000 out of the 4000 observations from MesoWest.
The impact of RAWS observations on ADAS analysis error statistics is diagnosed as a function of location and synoptic regime. Estimates of the sensitivity of the ADAS analyses to the RAWS observations are examined. Results suggest that withholding RAWS observations is more detrimental to the analyses than randomly withholding a comparable number of observations from other sources. The results also indicate that the RAWS observations are particularly valuable to analyses during winter season cold pool events in the West.
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