CDXWRFout
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Revisión de 13:04 12 abr 2018
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 |
| colspaen="4" | 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 |
| ∂t</sub>lqvac | WBACPWLV | W.B. low level (p >= 68000 Pa) acc. for QV | mm |
| ∂t</sub>mqvac | WBACPWMV | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QV | mm |
| ∂t</sub>hqvac | 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 |
| ∂t</sub>lqcac | WBACPWLC | W.B. low level (p >= 68000 Pa) acc. for QC | mm |
| ∂t</sub>mqcac | WBACPWMC | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QC | mm |
| ∂t</sub>hqcac | 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 |
| ∂t</sub>lqrac | WBACPWLR | W.B. low level (p >= 68000 Pa) acc. for QR | mm |
| ∂t</sub>mqrac | WBACPWMR | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QR | mm |
| ∂t</sub>hqrac | 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 |
| ∂t</sub>lqsac | WBACPWLS | W.B. low level (p >= 68000 Pa) acc. for QS | mm |
| ∂t</sub>mqsac | WBACPWMS | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QS | mm |
| ∂t</sub>hqsac | 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 |
| ∂t</sub>lqiac | WBACPWLI | W.B. low level (p >= 68000 Pa) acc. for QI | mm |
| ∂t</sub>mqiac | WBACPWMI | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QI | mm |
| ∂t</sub>hqiac | 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 |
| ∂t</sub>lqgac | WBACPWLG | W.B. low level (p >= 68000 Pa) acc. for QG | mm |
| ∂t</sub>mqgac | WBACPWMG | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QG | mm |
| ∂t</sub>hqgac | 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 |
| ∂t</sub>lqhac | WBACPWLH | W.B. low level (p >= 68000 Pa) acc. for QH | mm |
| ∂t</sub>mqhac | WBACPWMH | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QH | mm |
| ∂t</sub>hqhac | 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 |
