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.
cfsipvf
The Climate Forecast System (CFS), developed by NOAA’s National Centers for Environmental Prediction (NCEP), is a state-of-the-art global weather and climate model designed for medium- to long-range forecasting—spanning from days up to several seasons. CFS integrates atmospheric, oceanic, land surface, and sea ice components into a fully coupled modeling framework, delivering highly detailed and reliable forecasts for climate trends, seasonal outlooks, and extended-range weather events. By assimilating real-time observations from satellites, ocean buoys, and weather stations worldwide, CFS ensures its predictions reflect the current state of the Earth system, making it an essential tool for researchers, meteorologists, and organizations that rely on accurate climate guidance.
The CFS Isentropic Levels product delivers forecasts on surfaces of constant potential temperature (isentropic surfaces), which are particularly valuable for understanding atmospheric transport, air mass movements, and large-scale weather patterns. Meteorologists and researchers use isentropic data to track the movement of air parcels, analyze stability, and study the dynamics of fronts and jet streams with greater clarity than standard pressure-based analyses.
Click a parameter to reveal variants in a compact table with ready-to-copy JSON selectors.
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":""}
|
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