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
CFS Isentropic provides Climate Forecast System fields on surfaces of constant potential temperature. These isentropic surfaces are useful for following air-mass transport and upper-air dynamics in a way that complements standard pressure-level analysis.
The cfsipvf dataset includes fields such as potential vorticity, stream function, and lapse rate. Those signals help diagnose jet streams, troughs, fronts, stability, and links between the troposphere and lower stratosphere.
In GribStream, CFS Isentropic is useful when a workflow needs extended-range dynamic context without downloading full GRIB files: aviation planning, upper-air diagnostics, research signals, or comparison against CFS pressure-level fields.
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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