Good day, I want to obtain the moisture bugdet term P - E from the evapotranpiration and
Total precipitation data sets, and the evaporation values are negative.
Not exact matches
The corresponding studies were funded by the German Research Foundation (DFG) with a
total of EUR 600,000 for two years under the project «Integrating Microwave Link
Data for Analysis of
Precipitation in Complex Terrain: Theoretical Aspects and Hydrometeorological Applications» (IMAP).
To test the accuracy of these modeled
data, we compared values from the Verde ponderosa pine PRISM modeled
data to measurements of
total winter
precipitation recorded during the original Beaver Creek experiments [31].
I've presented videos and gif animations to show the impacts of ENSO on ISCCP
Total Cloud Amount
data (with cautions about that dataset), CAMS - OPI
precipitation data, NOAA's Trade Wind Index (5S - 5N, 135W - 180) anomaly
data, RSS MSU TLT anomaly
data, CLS (AVISO) Sea Level anomaly
data, NCEP / DOE Reanalysis - 2 Surface Downward Shortwave Radiation Flux (dswrfsfc) anomaly
data, Reynolds OI.v2 SST anomaly
data and the NODC's ocean heat content
data.
It was valuable because it was produced from easily available
data,
total monthly
precipitation (P) and evaporation (E) to produce a P / E Index.
All of these characteristics (except for the ocean temperature) have been used in SAR and TAR IPCC (Houghton et al. 1996; 2001) reports for model -
data inter-comparison: we considered as tolerable the following intervals for the annual means of the following climate characteristics which encompass corresponding empirical estimates: global SAT 13.1 — 14.1 °C (Jones et al. 1999); area of sea ice in the Northern Hemisphere 6 — 14 mil km2 and in the Southern Hemisphere 6 — 18 mil km2 (Cavalieri et al. 2003);
total precipitation rate 2.45 — 3.05 mm / day (Legates 1995); maximum Atlantic northward heat transport 0.5 — 1.5 PW (Ganachaud and Wunsch 2003); maximum of North Atlantic meridional overturning stream function 15 — 25 Sv (Talley et al. 2003), volume averaged ocean temperature 3 — 5 °C (Levitus 1982).
Correlation (color) and regression maps (contour) of SST (left) and SLP (right) associated with the first EOF modes of annual
precipitation (a, b), low - frequency
precipitation (c, d), and
total water storage (e, f), which are calculated using annual mean
data for the first EOF mode of annual
precipitation, 10 - year running mean for
precipitation, and 10 - year running mean leading with 5 - year for
total water storage.
Correlation coefficients are calculated using annual mean
data for the first EOF mode of annual
precipitation, 10 - year running mean
data for the low - frequency
precipitation, and 10 - year running mean
data leading with 5 - year for the
total water storage.
COOP
data usually consist of daily maximum and minimum temperatures, snowfall, and 24 - hour
precipitation totals.