CDXWRFout

! CF name ! WRF name ! description ! units |-

| colspan="4" 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 |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 |-

|}

{|

name ! WRF name ! description ! units |-

| Q_hac | WBACDIABH | Water Budget column integrated and time accumulation of diabatic heating from Micro-Physics | K |-

&part;_tqvac | WBACPW | Water Budget column integrated and time accumulated for water vapor content | mm |-

&part;_tqcac | WBACPWC | Water Budget col. int. & time accumulated for cloud content | mm |-

&part;_tqrac | WBACPWR | Water Budget col. int. & time accumulated for rain content | mm |-

&part;_tqsac | WBACPWS | Water Budget col. int. & time accumulated for snow content | mm |-

&part;_tqiac | WBACPWI | Water Budget col. int. & time accumulated for ice content | mm |-

&part;_tqhac | WBACPWH | Water Budget col. int. & time accumulated for hail content | mm |-

&part;_tqgac | WBACPWG | Water Budget col. int. & time accumulated for graupel content | mm |-

adv_hqvac | WBACF | W.B. c-int. acc. hor. convergence of water vapour (+, conv.; -, div.) | mm |-

adv_hqcac | WBACFC | W.B. c-int. acc. hor. convergence of cloud (+, conv.; -, div.) | mm |-

adv_hqrac | WBACFR | W.B. c-int. acc. hor. convergence of rain (+, conv.; -, div.) | mm |-

adv_hqsac | WBACFS | W.B. c-int. acc. hor. convergence of snow (+, conv.; -, div.) | mm |-

adv_hqiac | WBACFI | W.B. c-int. acc. hor. convergence of ice (+, conv.; -, div.) | mm |-

adv_hqhac | WBACFH | W.B. c-int. acc. hor. convergence of hail (+, conv.; -, div.) | mm |-

adv_hqgac | WBACFG | W.B. c-int. acc. hor. convergence of graupel (+, conv.; -, div.) | mm |-

adv_zqvac | WBACZ | W.B. c-int. acc. ver. convergence of water vapour (+, conv.; -, div.), always 0 | mm |-

adv_zqcac | WBACZC | W.B. c-int. acc. ver. convergence of cloud (+, conv.; -, div.) | mm |-

adv_zqrac | WBACZR | W.B. c-int. acc. ver. convergence of rain (+, conv.; -, div.) | mm |-

adv_zqsac | WBACZS | W.B. c-int. acc. ver. convergence of snow (+, conv.; -, div.) | mm |-

adv_zqiac | WBACZI | W.B. c-int. acc. ver. convergence of ice (+, conv.; -, div.) | mm |-

adv_zqhac | WBACZH | W.B. c-int. acc. ver. convergence of hail (+, conv.; -, div.) | mm |-

adv_zqgac | WBACZG | W.B. c-int. acc. ver. convergence of graupel (+, conv.; -, div.) | mm |-

|-multicolumn{4}{l}{Low-mid-level} |-

Q_h^lac | WBACDIABHL | W.B. low level acc. of diabatic heating from MP | K |-

Q_h^mac | WBACDIABHM | W.B. mid-level acc. of diabatic heating from MP | K |-

Q_h^mac | WBACDIABHH | W.B. high-level acc. of diabatic heating from MP | K |-

&part;t</sub>^lqvac | WBACPWLV | W.B. low level (p >= 68000 Pa) acc. for QV | mm |-

&part;t</sub>^mqvac | WBACPWMV | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QV | mm |-

&part;t</sub>^hqvac | WBACPWHV | W.B. high level (p < 44000 Pa) acc. for QV | mm |-

adv_h^lqvac | WBACFLV | W.B. low-lev. acc. hor. convergence of QV | mm |-

adv_h^mqvac | WBACFMV | W.B. mid-lev. acc. hor. convergence of QV | mm |-

adv_h^hqvac | WBACFHV | W.B. high-lev. acc. hor. convergence of QV | mm |-

adv_z^lqvac | WBACZLV | W.B. low level acc. ver. convergence of QV | mm |-

$adv_z^mqvac | WBACZMV | W.B. mid level acc. ver. convergence of QV | mm |-

$adv_z^hqvac | WBACZHV | W.B. high level acc. ver. convergence of QV | mm |-

&part;t</sub>^lqcac | WBACPWLC | W.B. low level (p >= 68000 Pa) acc. for QC | mm |-

&part;t</sub>^mqcac | WBACPWMC | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QC | mm |-

&part;t</sub>^hqcac | WBACPWHC | W.B. high level (p < 44000 Pa) acc. for QC | mm |-

adv_h^lqcac | WBACFLC | W.B. low-lev. acc. hor. convergence of QC | mm |-

adv_h^mqcac | WBACFMC | W.B. mid-lev. acc. hor. convergence of QC | mm |-

adv_h^hqcac | WBACFHC | W.B. high-lev. acc. hor. convergence of QC | mm |-

adv_z^lqcac | WBACZLC | W.B. low level acc. ver. convergence of QC | mm |-

adv_z^mqcac | WBACZMC | W.B. mid level acc. ver. convergence of QC | mm |-

adv_z^hqcac | WBACZHC | W.B. high level acc. ver. convergence of QC | mm |-

&part;t</sub>^lqrac | WBACPWLR | W.B. low level (p >= 68000 Pa) acc. for QR | mm |-

&part;t</sub>^mqrac | WBACPWMR | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QR | mm |-

&part;t</sub>^hqrac | WBACPWHR | W.B. high level (p < 44000 Pa) acc. for QR | mm |-

adv_h^lqrac | WBACFLR | W.B. low-lev. acc. hor. convergence of QR | mm |-

adv_h^mqrac | WBACFMR | W.B. mid-lev. acc. hor. convergence of QR | mm |-

adv_h^hqrac | WBACFHR | W.B. high-lev. acc. hor. convergence of QR | mm |-

adv_z^lqrac | WBACZLR | W.B. low level acc. ver. convergence of QR | mm |-

adv_z^mqrac | WBACZMR | W.B. mid level acc. ver. convergence of QR | mm |-

adv_z^hqrac | WBACZHR | W.B. high level acc. ver. convergence of QR | mm |-

&part;t</sub>^lqsac | WBACPWLS | W.B. low level (p >= 68000 Pa) acc. for QS | mm |-

&part;t</sub>^mqsac | WBACPWMS | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QS | mm |-

&part;t</sub>^hqsac | WBACPWHS | W.B. high level (p < 44000 Pa) acc. for QS | mm |-

adv_h^lqsac | WBACFLS | W.B. low-lev. acc. hor. convergence of QS | mm |-

adv_h^mqsac | WBACFMS | W.B. mid-lev. acc. hor. convergence of QS | mm |-

adv_h^hqsac | WBACFHS | W.B. high-lev. acc. hor. convergence of QS | mm |-

adv_z^lqsac | WBACZLS | W.B. low level acc. ver. convergence of QS | mm |-

adv_z^mqsac | WBACZMS | W.B. mid level acc. ver. convergence of QS | mm |-

adv_z^hqsac | WBACZHS | W.B. high level acc. ver. convergence of QS | mm |-

&part;t</sub>^lqiac | WBACPWLI | W.B. low level (p >= 68000 Pa) acc. for QI | mm |-

&part;t</sub>^mqiac | WBACPWMI | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QI | mm |-

&part;t</sub>^hqiac | WBACPWHI | W.B. high level (p < 44000 Pa) acc. for QI | mm |-

adv_h^lqiac | WBACFLI | W.B. low-lev. acc. hor. convergence of QI | mm |-

adv_h^mqiac | WBACFMI | W.B. mid-lev. acc. hor. convergence of QI | mm |-

adv_h^hqiac | WBACFHI | W.B. high-lev. acc. hor. convergence of QI | mm |-

adv_z^lqiac | WBACZLI | W.B. low level acc. ver. convergence of QI | mm |-

adv_z^mqiac | WBACZMI | W.B. mid level acc. ver. convergence of QI | mm |-

adv_z^hqiac | WBACZHI | W.B. high level acc. ver. convergence of QI | mm |-

&part;t</sub>^lqgac | WBACPWLG | W.B. low level (p >= 68000 Pa) acc. for QG | mm |-

&part;t</sub>^mqgac | WBACPWMG | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QG | mm |-

&part;t</sub>^hqgac | WBACPWHG | W.B. high level (p < 44000 Pa) acc. for QG | mm |-

adv_h^lqgac | WBACFLG | W.B. low-lev. acc. hor. convergence of QG | mm |-

adv_h^mqgac | WBACFMG | W.B. mid-lev. acc. hor. convergence of QG | mm |-

adv_h^hqgac | WBACFHG | W.B. high-lev. acc. hor. convergence of QG | mm |-

adv_z^lqgac | WBACZLG | W.B. low level acc. ver. convergence of QG | mm |-

adv_z^mqgac | WBACZMG | W.B. mid level acc. ver. convergence of QG | mm |-

adv_z^hqgac | WBACZHG | W.B. high level acc. ver. convergence of QG | mm |-

&part;t</sub>^lqhac | WBACPWLH | W.B. low level (p >= 68000 Pa) acc. for QH | mm |-

&part;t</sub>^mqhac | WBACPWMH | W.B. mid level (44000 Pa <= p < 68000 Pa) acc. for QH | mm |-

&part;t</sub>^hqhac | WBACPWHH | W.B. high level (p < 44000 Pa) acc. for QH | mm |-

adv_h^lqhac | WBACFLH | W.B. low-lev. acc. hor. convergence of QH | mm |-

adv_h^mqhac | WBACFMH | W.B. mid-lev. acc. hor. convergence of QH | mm |-

adv_h^hqhac | WBACFHH | W.B. high-lev. acc. hor. convergence of QH | mm |-

adv_z^lqhac | WBACZLH | W.B. low level acc. ver. convergence of QH | mm |-

adv_z^mqhac | WBACZMH | W.B. mid level acc. ver. convergence of QH | mm |-

adv_z^hqhac | WBACZHH | W.B. high level acc. ver. convergence of QH | mm |-