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.
Código GribStream: cfsipvf
CFS ipvf expõe campos especializados do Climate Forecast System ligados a vorticidade potencial e estrutura isentrópica.
Ele é mais útil para diagnóstico dinâmico e pesquisa do que para produtos finais de usuário comum. Use quando seu workflow precisa de variáveis atmosféricas de larga escala além de temperatura, vento ou precipitação.
No GribStream, cfsipvf mantém os seletores técnicos do catálogo, permitindo consultas pontuais ou em grade sem processar arquivos completos.
Para campos mais gerais da família CFS, consulte cfspgbf e cfsflxf.
Clique em um parâmetro para ver as variantes em uma tabela compacta, com seletores JSON prontos para copiar. Códigos, níveis e valores do seletor ficam exatamente como a API expõe.
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":""}
|
Nenhum parâmetro corresponde à busca.