However, to validate and verify the RAWS observations, we needed to find a "truth" with which to compare the RAWS data. Operational models were quickly discarded, as their relatively poor resolution (both spatially and temporally) and lack of site-specific measurements rendered them insufficient for this study. Satellite observations were limited to only calculated temperatures, so we couldn't test all of the instruments at a RAWS site. Plus, clouds could obscure surface readings, so satellite-derived observations were similarly deemed insufficient.
The best dataset for comparison with RAWS turned out to be the Real-Time Mesoscale Analysis prepared by NOAA/NCEP. Given the high temporal and spatial grid spacing of the RTMA (hourly and 5-km, respectively, for this study), we could better determine where the two data sets differed.
However, the RTMA has plenty of issues itself. It is the best mesoscale analysis of surface parameters currently available, but lacks verification where surface observations are not available. Thus, discrepancies between RAWS and RTMA could be caused by errors in either (or both) datasets. This fact must be kept in mind throughout the remainder of the analysis.
Data acquisition for each of these products is limited to very recent years, as the RTMA has only been produced operationally for the last few years. Thus, this study will look at two years of data, from 1 August 2008 to 31 July 2010. Expansion of our results to include more years is near the top of our to-do list.