Lapse rate is the vertical rate of temperature decrease with height. It is a key stability metric for convection and boundary-layer mixing.
- Units: K/m.
Code GribStream: cfsipvf
CFS Isentropic fournit des champs du Climate Forecast System sur surfaces de température potentielle constante. Ces surfaces isentropiques aident à suivre transport de masses d'air et dynamique d'altitude sous un angle différent des niveaux de pression classiques.
Le dataset cfsipvf contient des champs comme vorticité potentielle, fonction de courant et lapse rate, c'est-à-dire le gradient thermique vertical. Ces signaux sont utiles pour jet-streams, talwegs, fronts, stabilité et couplages entre troposphère et basse stratosphère.
Dans GribStream, CFS Isentropic est utile quand une application a besoin de contexte dynamique à très long horizon sans télécharger des fichiers GRIB complets : planification aviation, diagnostics d'altitude, recherche ou comparaison avec les champs CFS Pressure.
Le schéma API reste le même que pour les autres datasets GribStream : choisissez coordonnées ou requête sur grille, plage temporelle et sélecteurs du catalogue ; les codes et valeurs de sélecteur de la source restent inchangés.
Cliquez sur un paramètre pour voir ses variantes dans une table compacte avec des sélecteurs JSON prêts à copier. Les codes, niveaux et valeurs de sélecteur restent exactement tels que l'API les expose.
Lapse rate is the vertical rate of temperature decrease with height. It is a key stability metric for convection and boundary-layer mixing.
| Level | Info | Horizon | Introduced | Selector |
|---|---|---|---|---|
1000 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"1000 K isentropic level","info":""}
|
|
1250 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"1250 K isentropic level","info":""}
|
|
1500 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"1500 K isentropic level","info":""}
|
|
270 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"270 K isentropic level","info":""}
|
|
280 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"280 K isentropic level","info":""}
|
|
290 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"290 K isentropic level","info":""}
|
|
300 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"300 K isentropic level","info":""}
|
|
310 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"310 K isentropic level","info":""}
|
|
320 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"320 K isentropic level","info":""}
|
|
330 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"330 K isentropic level","info":""}
|
|
350 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"350 K isentropic level","info":""}
|
|
400 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"400 K isentropic level","info":""}
|
|
450 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"450 K isentropic level","info":""}
|
|
550 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"550 K isentropic level","info":""}
|
|
650 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"650 K isentropic level","info":""}
|
|
850 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"LAPR","level":"850 K isentropic level","info":""}
|
Montgomery stream function is used on isentropic surfaces to diagnose balanced flow and thermal structure, especially in tropical dynamics.
| Level | Info | Horizon | Introduced | Selector |
|---|---|---|---|---|
1000 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"1000 K isentropic level","info":""}
|
|
1250 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"1250 K isentropic level","info":""}
|
|
1500 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"1500 K isentropic level","info":""}
|
|
270 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"270 K isentropic level","info":""}
|
|
280 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"280 K isentropic level","info":""}
|
|
290 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"290 K isentropic level","info":""}
|
|
300 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"300 K isentropic level","info":""}
|
|
310 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"310 K isentropic level","info":""}
|
|
320 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"320 K isentropic level","info":""}
|
|
330 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"330 K isentropic level","info":""}
|
|
350 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"350 K isentropic level","info":""}
|
|
400 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"400 K isentropic level","info":""}
|
|
450 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"450 K isentropic level","info":""}
|
|
550 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"550 K isentropic level","info":""}
|
|
650 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"650 K isentropic level","info":""}
|
|
850 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"MNTSF","level":"850 K isentropic level","info":""}
|
Pressure is the atmospheric pressure at the specified level. It is a fundamental mass-field variable for dynamics and thermodynamics.
| Level | Info | Horizon | Introduced | Selector |
|---|---|---|---|---|
surface |
0h-5160h | 2018-10-31 |
{"name":"PRES","level":"surface","info":""}
|
Vorticity measures rotation of the flow. It highlights dynamical forcing, shear, and potential for cyclonic development.
| Level | Info | Horizon | Introduced | Selector |
|---|---|---|---|---|
1000 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"1000 K isentropic level","info":""}
|
|
1250 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"1250 K isentropic level","info":""}
|
|
1500 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"1500 K isentropic level","info":""}
|
|
270 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"270 K isentropic level","info":""}
|
|
280 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"280 K isentropic level","info":""}
|
|
290 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"290 K isentropic level","info":""}
|
|
300 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"300 K isentropic level","info":""}
|
|
310 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"310 K isentropic level","info":""}
|
|
320 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"320 K isentropic level","info":""}
|
|
330 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"330 K isentropic level","info":""}
|
|
350 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"350 K isentropic level","info":""}
|
|
400 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"400 K isentropic level","info":""}
|
|
450 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"450 K isentropic level","info":""}
|
|
550 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"550 K isentropic level","info":""}
|
|
650 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"650 K isentropic level","info":""}
|
|
850 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"PVORT","level":"850 K isentropic level","info":""}
|
Relative humidity describes how close the air is to saturation at the specified level. High values favor cloud formation.
| Level | Info | Horizon | Introduced | Selector |
|---|---|---|---|---|
1000 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"1000 K isentropic level","info":""}
|
|
1250 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"1250 K isentropic level","info":""}
|
|
1500 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"1500 K isentropic level","info":""}
|
|
270 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"270 K isentropic level","info":""}
|
|
280 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"280 K isentropic level","info":""}
|
|
290 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"290 K isentropic level","info":""}
|
|
300 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"300 K isentropic level","info":""}
|
|
310 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"310 K isentropic level","info":""}
|
|
320 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"320 K isentropic level","info":""}
|
|
330 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"330 K isentropic level","info":""}
|
|
350 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"350 K isentropic level","info":""}
|
|
400 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"400 K isentropic level","info":""}
|
|
450 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"450 K isentropic level","info":""}
|
|
550 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"550 K isentropic level","info":""}
|
|
650 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"650 K isentropic level","info":""}
|
|
850 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"RH","level":"850 K isentropic level","info":""}
|
Air temperature is the thermal state of the atmosphere at the specified level. It influences density, stability, and energy exchange.
| Level | Info | Horizon | Introduced | Selector |
|---|---|---|---|---|
1000 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"1000 K isentropic level","info":""}
|
|
1250 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"1250 K isentropic level","info":""}
|
|
1500 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"1500 K isentropic level","info":""}
|
|
270 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"270 K isentropic level","info":""}
|
|
280 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"280 K isentropic level","info":""}
|
|
290 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"290 K isentropic level","info":""}
|
|
300 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"300 K isentropic level","info":""}
|
|
310 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"310 K isentropic level","info":""}
|
|
320 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"320 K isentropic level","info":""}
|
|
330 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"330 K isentropic level","info":""}
|
|
350 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"350 K isentropic level","info":""}
|
|
400 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"400 K isentropic level","info":""}
|
|
450 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"450 K isentropic level","info":""}
|
|
550 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"550 K isentropic level","info":""}
|
|
650 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"650 K isentropic level","info":""}
|
|
850 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"850 K isentropic level","info":""}
|
|
surface |
0h-5160h | 2018-10-31 |
{"name":"TMP","level":"surface","info":""}
|
U‑component of wind is the east‑west component of the horizontal wind. Combine with v for speed and direction.
| Level | Info | Horizon | Introduced | Selector |
|---|---|---|---|---|
1000 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"1000 K isentropic level","info":""}
|
|
1250 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"1250 K isentropic level","info":""}
|
|
1500 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"1500 K isentropic level","info":""}
|
|
270 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"270 K isentropic level","info":""}
|
|
280 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"280 K isentropic level","info":""}
|
|
290 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"290 K isentropic level","info":""}
|
|
300 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"300 K isentropic level","info":""}
|
|
310 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"310 K isentropic level","info":""}
|
|
320 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"320 K isentropic level","info":""}
|
|
330 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"330 K isentropic level","info":""}
|
|
350 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"350 K isentropic level","info":""}
|
|
400 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"400 K isentropic level","info":""}
|
|
450 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"450 K isentropic level","info":""}
|
|
550 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"550 K isentropic level","info":""}
|
|
650 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"650 K isentropic level","info":""}
|
|
850 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"UGRD","level":"850 K isentropic level","info":""}
|
V‑component of wind is the north‑south component of the horizontal wind. Combine with u for speed and direction.
| Level | Info | Horizon | Introduced | Selector |
|---|---|---|---|---|
1000 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"1000 K isentropic level","info":""}
|
|
1250 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"1250 K isentropic level","info":""}
|
|
1500 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"1500 K isentropic level","info":""}
|
|
270 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"270 K isentropic level","info":""}
|
|
280 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"280 K isentropic level","info":""}
|
|
290 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"290 K isentropic level","info":""}
|
|
300 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"300 K isentropic level","info":""}
|
|
310 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"310 K isentropic level","info":""}
|
|
320 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"320 K isentropic level","info":""}
|
|
330 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"330 K isentropic level","info":""}
|
|
350 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"350 K isentropic level","info":""}
|
|
400 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"400 K isentropic level","info":""}
|
|
450 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"450 K isentropic level","info":""}
|
|
550 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"550 K isentropic level","info":""}
|
|
650 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"650 K isentropic level","info":""}
|
|
850 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VGRD","level":"850 K isentropic level","info":""}
|
Vertical velocity in pressure coordinates (omega). Negative values indicate upward motion (rising air); positive values indicate subsidence.
| Level | Info | Horizon | Introduced | Selector |
|---|---|---|---|---|
1000 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"1000 K isentropic level","info":""}
|
|
1250 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"1250 K isentropic level","info":""}
|
|
1500 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"1500 K isentropic level","info":""}
|
|
270 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"270 K isentropic level","info":""}
|
|
280 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"280 K isentropic level","info":""}
|
|
290 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"290 K isentropic level","info":""}
|
|
300 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"300 K isentropic level","info":""}
|
|
310 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"310 K isentropic level","info":""}
|
|
320 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"320 K isentropic level","info":""}
|
|
330 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"330 K isentropic level","info":""}
|
|
350 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"350 K isentropic level","info":""}
|
|
400 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"400 K isentropic level","info":""}
|
|
450 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"450 K isentropic level","info":""}
|
|
550 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"550 K isentropic level","info":""}
|
|
650 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"650 K isentropic level","info":""}
|
|
850 K isentropic level |
0h-5160h | 2018-10-31 |
{"name":"VVEL","level":"850 K isentropic level","info":""}
|
Aucun paramètre ne correspond à la recherche.