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ABSTRACTThe NCEP Climate Forecast S
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1. IntroductionThe first reanalysis
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In this paper we only discuss globa
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the reanalysis was halted to addres
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online archive of data for reanalys
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density MESONET data is included in
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The 1B datasets were calibrated usi
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MetOp is Europe's first polar-orbit
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The third GSI feature enabled in th
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the hydrostatic assumption. Soon af
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esolution with 28 sigma layers in t
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SW and LW radiations at one-hour in
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SST data. The other uses AVHRR and
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y Gent and McWilliams (1990; see al
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from the Global Temperature-Salinit
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through the end of the data set in
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The passive microwave weather filte
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from the sea ice/ocean back to the
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weight is assigned to the gauge ana
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Stream 6: 1 Jan 1994 to 31 Mar 1999
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in the mid 1990’s, the period whe
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e due to a change over the oceans (
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In Figure 49, we show the temporal
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distributed in time and space. Desp
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forecast model at a lower resolutio
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Appendix A: AcronymsAER Atmospheric
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ONPCMDIPIRATAPROFLRQBOQuikSCATR1R2R
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TMP2M 2m air temperature 24 / 473TM
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Appendix C: The Data AccessTo addre
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Figure 26 shows the global total bi
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Argo Science Team, 2001: The global
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Compo, G.P., J.S. Whitaker, and P.D
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- Page 75 and 76: Global Forecast System. Manuscript
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- Page 85 and 86: Figure 21: Same as Figure 2, but fo
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- Page 89 and 90: Figure 1: Diagram illustrating CFSR
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- Page 103 and 104: Figure 15: Radiance instruments on
- Page 105 and 106: Figure 17: Same as in Figure 16, bu
- Page 107 and 108: Figure 19: Global average Tb first
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