The NCEP Climate Forecast System Reanalysis - NOAA National ...

More documents

Recommendations

Info

Figure 28: <strong>The</strong> yearly total of tropical storm reports stacked by the 8 geographical basinsfrom top to bottom, Western Pacific (W Pac), Southern Indian (S Ind), SouthernPacific (S Pac) , North Atlantic-Caribbean (Atl), Eastern Pacific (E Pac), CentralPacific (Cen Pac) , Bay of Bengal and Arabian Sea.- 116 -
Figure 29: Time series of the percentage of detected tropical storms plotted globally and forselected Northern Hemisphere basins: the Atlantic-Caribbean (ATL), WesternPacific (W Pac) and Eastern Pacific (E Pac) Oceans.- 117 -
Page 2 and 3:
ABSTRACTThe NCEP Climate Forecast S
Page 4 and 5:
1. IntroductionThe first reanalysis
Page 6 and 7:
In this paper we only discuss globa
Page 8 and 9:
the reanalysis was halted to addres
Page 10 and 11:
online archive of data for reanalys
Page 12 and 13:
density MESONET data is included in
Page 14 and 15:
The 1B datasets were calibrated usi
Page 16 and 17:
MetOp is Europe's first polar-orbit
Page 20 and 21:
The third GSI feature enabled in th
Page 22 and 23:
the hydrostatic assumption. Soon af
Page 24 and 25:
esolution with 28 sigma layers in t
Page 26 and 27:
SW and LW radiations at one-hour in
Page 28 and 29:
SST data. The other uses AVHRR and
Page 30 and 31:
y Gent and McWilliams (1990; see al
Page 32 and 33:
from the Global Temperature-Salinit
Page 34 and 35:
through the end of the data set in
Page 36 and 37:
The passive microwave weather filte
Page 39 and 40:
from the sea ice/ocean back to the
Page 41 and 42:
weight is assigned to the gauge ana
Page 43 and 44:
Stream 6: 1 Jan 1994 to 31 Mar 1999
Page 45 and 46:
in the mid 1990’s, the period whe
Page 47:
e due to a change over the oceans (
Page 52 and 53:
In Figure 49, we show the temporal
Page 54 and 55:
distributed in time and space. Desp
Page 56 and 57:
forecast model at a lower resolutio
Page 58 and 59:
Appendix A: AcronymsAER Atmospheric
Page 60 and 61:
ONPCMDIPIRATAPROFLRQBOQuikSCATR1R2R
Page 62 and 63:
TMP2M 2m air temperature 24 / 473TM
Page 64 and 65:
Appendix C: The Data AccessTo addre
Page 66 and 67: Figure 26 shows the global total bi
Page 68 and 69: Argo Science Team, 2001: The global
Page 70 and 71: Compo, G.P., J.S. Whitaker, and P.D
Page 72 and 73: ozone Mapping and Profiler Suite (O
Page 75 and 76: Global Forecast System. Manuscript
Page 77 and 78: and climate models. Atmos. Chem. Ph
Page 79 and 80: performance Earth system modeling w
Page 81 and 82: with mesoscale numerical weather pr
Page 83 and 84: experiments using SSM/I wind speed
Page 85 and 86: Figure 21: Same as Figure 2, but fo
Page 87 and 88: Figure 45: The fit of 6-hour foreca
Page 89 and 90: Figure 1: Diagram illustrating CFSR
Page 91 and 92: Figure 3: Same as in Figure 2, but
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
Page 109 and 110: Figure 21: Same as in Figure 16, bu
Page 111: Figure 23: Comparisons of the SSU b
Page 114 and 115: Figure 26: The global total bias fo
Page 118 and 119: Figure 30: The vertical structure o
Page 120 and 121: Figure 32: The global number of tem
Page 122 and 123: Figure 34: The same as Figure 33, b
Page 124 and 125: Figure 36: Monthly mean Sea ice ext
Page 126 and 127: Figure 38: 2-meter volumetric soil
Page 128 and 129: Figure 40: Schematic of the executi
Page 130 and 131: Figure 42: Yearly averaged Southern
Page 132 and 133: Figure 44: Monthly mean hourly surf
Page 134 and 135: Figure 46: Global mean temperature
Page 136 and 137: Figure 48: Zonal mean total ozone d
Page 138 and 139: Figure 50: The subsurface temperatu
Page 140 and 141: Figure 52: Vertical profiles of the
Page 142 and 143: Figure 54: Zonal surface velocities
Page 144 and 145: ProgramPREVENTSACQCACAR_CQCCQCCQCVA
Page 146: Satellite Starting date Ending Date
show all

The NCEP Climate Forecast System Reanalysis - NOAA National ...

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?