CDXWRFout
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Revisión a fecha de 13:07 12 abr 2018; Lluis.fita (Discusión | contribuciones)
Table of variables as they appear in the `wrfcdx_d[nn]' files
CF variables
CF name | WRF name | description | units |
---|---|---|---|
2D | |||
lon | LON | LONGITUDE | degrees_east |
lat | LAT | LATITUDE | degrees_north |
capev | CDXCAPE | CONVECTIVE AVAILABLE POTENTIAL ENERGY | Jkg-1 |
cin | CIN | CONVECTIVE INHIBITION | Jkg-1 |
cltmean | CLTMEAN | MEAN TOTAL CLOUDINESS IN CORDEX OUTPUT | 1 |
cllmean | CLLMEAN | MEAN LOW-LEVEL CLOUDINESS (p >= 68000 Pa) IN CORDEX OUTPUT | 1 |
clmmean | CLMMEAN | MEAN MID-LEVEL CLOUDINESS (44000 <= p < 68000 Pa) IN CORDEX OUTPUT | 1 |
clhmean | CLHMEAN | MEAN HIGH-LEVEL CLOUDINESS (p < 44000 Pa) IN CORDEX OUTPUT | 1 |
mrso | MRSO | TOTAL SOIL CONTENT | kgm-2 |
prw | PRW | WATER VAPOR PATH | kgm-2 |
psl | PSL | SEA LEVEL PRESSURE | Pa |
clwvi | CLWVI | LIQUID WATER PATH | kgm-2 |
clivi | CLIVI | ICE WATER PATH | kgm-2 |
clgvi | CLGVI | GRAUPEL WATER PATH | kgm-2 |
clhvi | CLHVI | HAIL WATER PATH | kgm-2 |
hurs | HURS | 2M RELATIVE HUMIDITY | 1 |
huss | HUSS | 2M SPECIFIC HUMIDITY | 1 |
lfcp | LFCP | PRESSURE LEVEL FREE CONVECTION | Pa |
lfcz | LFCZ | HEIGHT LEVEL FREE CONVECTION | m |
li | LI | LIFTED INDEX | 1 |
slw | SLW | TOTAL SOIL LIQUID WATER CONTENT | kgm-2 |
uas | UAS | 10M EASTWARD WIND SPEED | ms-1 |
vas | VAS | 10M NORTHWARD WIND SPEED | ms-1 |
wsgsmax | WSGSMAX | Maximum near-surface wind speed of gust | ms-1 |
usgsmax | USGSMAX | Eastward maximum near-surface wind speed of gust | ms-1 |
vsgsmax | VSGSMAX | Northward maximum near-surface wind speed of gust | ms-1 |
wsgspercen | WSGSPERCEN | Percentage of time steps where grid point got wind gust | |
totwsgsmax | TOTWSGSMAX | Total (TKE + h. pr) Maximum near-surface wind speed of gust | ms-1 |
totugsmax | TOTUGSMAX | Total Eastward maximum near-surface wind speed of gust | ms-1 |
totvgsmax | TOTVGSMAX | Total Northward maximum near-surface wind speed of gust | ms-1 |
TOTWSGSPERCEN | Percentage of time steps where grid point got total wind gust | ||
zmlagen | ZMLAGEN | Generic boundary layer height theta(zmlagen) > min(theta[mix. layer]) + 1.5K | m |
wsz100max | WSZ100MAX | Maximum 100m nwind speed | ms-1 |
uz100max | UZ100MAX | Eastward maximum 100 m wind speed | ms-1 |
vz100max | VZ100MAX | Northward maximum 100 m wind speed | ms-1 |
sund | SUND | SUNSHINE LENGTH (ac. time SWDOWN > 120. Wm-2) | second |
tauu | TAUU | northward downward wind stress at 10 m | m2s-2 |
tauv | TAUV | eastward downward wind stress at 10 m | m2s-2 |
colspan="4" 3D | |||
HUR | HUR | AIR RELATIVE HUMIDITY | 1 |
HUS | HUS | AIR SPECIFIC HUMIDITY | 1 |
ZG | ZG | AIR GEOPOTENTIAL HEIGHT | m |
PRESS | PRESS | AIR PRSSURE | Pa |
TA | TA | AIR TEMPERATURE | K |
UA | UA | AIR EASTWARD WIND SPEED | ms-1 |
VA | VA | AIR NORTHWARD WIND SPEED | ms-1 |
Additional Water Budget variables
name | WRF name | description | units |
---|---|---|---|
Q_hac | WBACDIABH | Water Budget column integrated and time accumulation of diabatic heating from Micro-Physics | K |
∂tqvac | WBACPW | Water Budget column integrated and time accumulated for water vapor content | mm |
∂tqcac | WBACPWC | Water Budget col. int. & time accumulated for cloud content | mm |
∂tqrac | WBACPWR | Water Budget col. int. & time accumulated for rain content | mm |
∂tqsac | WBACPWS | Water Budget col. int. & time accumulated for snow content | mm |
∂tqiac | WBACPWI | Water Budget col. int. & time accumulated for ice content | mm |
∂tqhac | WBACPWH | Water Budget col. int. & time accumulated for hail content | mm |
∂tqgac | WBACPWG | Water Budget col. int. & time accumulated for graupel content | mm |
advhqvac | WBACF | W.B. c-int. acc. hor. convergence of water vapour (+, conv.; -, div.) | mm |
advhqcac | WBACFC | W.B. c-int. acc. hor. convergence of cloud (+, conv.; -, div.) | mm |
advhqrac | WBACFR | W.B. c-int. acc. hor. convergence of rain (+, conv.; -, div.) | mm |
advhqsac | WBACFS | W.B. c-int. acc. hor. convergence of snow (+, conv.; -, div.) | mm |
advhqiac | WBACFI | W.B. c-int. acc. hor. convergence of ice (+, conv.; -, div.) | mm |
advhqhac | WBACFH | W.B. c-int. acc. hor. convergence of hail (+, conv.; -, div.) | mm |
advhqgac | WBACFG | W.B. c-int. acc. hor. convergence of graupel (+, conv.; -, div.) | mm |
advzqvac | WBACZ | W.B. c-int. acc. ver. convergence of water vapour (+, conv.; -, div.), always 0 | mm |
advzqcac | WBACZC | W.B. c-int. acc. ver. convergence of cloud (+, conv.; -, div.) | mm |
advzqrac | WBACZR | W.B. c-int. acc. ver. convergence of rain (+, conv.; -, div.) | mm |
advzqsac | WBACZS | W.B. c-int. acc. ver. convergence of snow (+, conv.; -, div.) | mm |
advzqiac | WBACZI | W.B. c-int. acc. ver. convergence of ice (+, conv.; -, div.) | mm |
advzqhac | WBACZH | W.B. c-int. acc. ver. convergence of hail (+, conv.; -, div.) | mm |
advzqgac | WBACZG | W.B. c-int. acc. ver. convergence of graupel (+, conv.; -, div.) | mm |
Low-mid-level | |||
Qhlac | WBACDIABHL | W.B. low level acc. of diabatic heating from MP | K |
Qhmac | WBACDIABHM | W.B. mid-level acc. of diabatic heating from MP | K |
Qhmac | WBACDIABHH | W.B. high-level acc. of diabatic heating from MP | K |
∂tlqvac | WBACPWLV | W.B. low level (p >= 68000 Pa) acc. for QV | mm |
∂tmqvac | WBACPWMV | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QV | mm |
∂thqvac | WBACPWHV | W.B. high level (p < 44000 Pa) acc. for QV | mm |
advhlqvac | WBACFLV | W.B. low-lev. acc. hor. convergence of QV | mm |
advhmqvac | WBACFMV | W.B. mid-lev. acc. hor. convergence of QV | mm |
advhhqvac | WBACFHV | W.B. high-lev. acc. hor. convergence of QV | mm |
advzlqvac | WBACZLV | W.B. low level acc. ver. convergence of QV | mm |
advzmqvac | WBACZMV | W.B. mid level acc. ver. convergence of QV | mm |
advzhqvac | WBACZHV | W.B. high level acc. ver. convergence of QV | mm |
∂tlqcac | WBACPWLC | W.B. low level (p >= 68000 Pa) acc. for QC | mm |
∂tmqcac | WBACPWMC | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QC | mm |
∂thqcac | WBACPWHC | W.B. high level (p < 44000 Pa) acc. for QC | mm |
advhlqcac | WBACFLC | W.B. low-lev. acc. hor. convergence of QC | mm |
advhmqcac | WBACFMC | W.B. mid-lev. acc. hor. convergence of QC | mm |
advhhqcac | WBACFHC | W.B. high-lev. acc. hor. convergence of QC | mm |
advzlqcac | WBACZLC | W.B. low level acc. ver. convergence of QC | mm |
advzmqcac | WBACZMC | W.B. mid level acc. ver. convergence of QC | mm |
advzhqcac | WBACZHC | W.B. high level acc. ver. convergence of QC | mm |
∂tlqrac | WBACPWLR | W.B. low level (p >= 68000 Pa) acc. for QR | mm |
∂tmqrac | WBACPWMR | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QR | mm |
∂thqrac | WBACPWHR | W.B. high level (p < 44000 Pa) acc. for QR | mm |
advhlqrac | WBACFLR | W.B. low-lev. acc. hor. convergence of QR | mm |
advhmqrac | WBACFMR | W.B. mid-lev. acc. hor. convergence of QR | mm |
advhhqrac | WBACFHR | W.B. high-lev. acc. hor. convergence of QR | mm |
advzlqrac | WBACZLR | W.B. low level acc. ver. convergence of QR | mm |
advzmqrac | WBACZMR | W.B. mid level acc. ver. convergence of QR | mm |
advzhqrac | WBACZHR | W.B. high level acc. ver. convergence of QR | mm |
∂tlqsac | WBACPWLS | W.B. low level (p >= 68000 Pa) acc. for QS | mm |
∂tmqsac | WBACPWMS | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QS | mm |
∂thqsac | WBACPWHS | W.B. high level (p < 44000 Pa) acc. for QS | mm |
advhlqsac | WBACFLS | W.B. low-lev. acc. hor. convergence of QS | mm |
advhmqsac | WBACFMS | W.B. mid-lev. acc. hor. convergence of QS | mm |
advhhqsac | WBACFHS | W.B. high-lev. acc. hor. convergence of QS | mm |
advzlqsac | WBACZLS | W.B. low level acc. ver. convergence of QS | mm |
advzmqsac | WBACZMS | W.B. mid level acc. ver. convergence of QS | mm |
advzhqsac | WBACZHS | W.B. high level acc. ver. convergence of QS | mm |
∂tlqiac | WBACPWLI | W.B. low level (p >= 68000 Pa) acc. for QI | mm |
∂tmqiac | WBACPWMI | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QI | mm |
∂thqiac | WBACPWHI | W.B. high level (p < 44000 Pa) acc. for QI | mm |
advhlqiac | WBACFLI | W.B. low-lev. acc. hor. convergence of QI | mm |
advhmqiac | WBACFMI | W.B. mid-lev. acc. hor. convergence of QI | mm |
advhhqiac | WBACFHI | W.B. high-lev. acc. hor. convergence of QI | mm |
advzlqiac | WBACZLI | W.B. low level acc. ver. convergence of QI | mm |
advzmqiac | WBACZMI | W.B. mid level acc. ver. convergence of QI | mm |
advzhqiac | WBACZHI | W.B. high level acc. ver. convergence of QI | mm |
∂tlqgac | WBACPWLG | W.B. low level (p >= 68000 Pa) acc. for QG | mm |
∂tmqgac | WBACPWMG | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QG | mm |
∂thqgac | WBACPWHG | W.B. high level (p < 44000 Pa) acc. for QG | mm |
advhlqgac | WBACFLG | W.B. low-lev. acc. hor. convergence of QG | mm |
advhmqgac | WBACFMG | W.B. mid-lev. acc. hor. convergence of QG | mm |
advhhqgac | WBACFHG | W.B. high-lev. acc. hor. convergence of QG | mm |
advzlqgac | WBACZLG | W.B. low level acc. ver. convergence of QG | mm |
advzmqgac | WBACZMG | W.B. mid level acc. ver. convergence of QG | mm |
advzhqgac | WBACZHG | W.B. high level acc. ver. convergence of QG | mm |
∂tlqhac | WBACPWLH | W.B. low level (p >= 68000 Pa) acc. for QH | mm |
∂tmqhac | WBACPWMH | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QH | mm |
∂thqhac | WBACPWHH | W.B. high level (p < 44000 Pa) acc. for QH | mm |
advhlqhac | WBACFLH | W.B. low-lev. acc. hor. convergence of QH | mm |
advhmqhac | WBACFMH | W.B. mid-lev. acc. hor. convergence of QH | mm |
advhhqhac | WBACFHH | W.B. high-lev. acc. hor. convergence of QH | mm |
advzlqhac | WBACZLH | W.B. low level acc. ver. convergence of QH | mm |
advzmqhac | WBACZMH | W.B. mid level acc. ver. convergence of QH | mm |
advzhqhac | WBACZHH | W.B. high level acc. ver. convergence of QH | mm |