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.
GribStreamコード: cfsipvf
CFS Isentropicは、一定の温位の面に沿ったClimate Forecast Systemフィールドを提供します。標準的な気圧面解析を補い、気塊輸送や上空力学を追いやすくします。
cfsipvfデータセットには、渦位、流線関数、気温減率などのフィールドが含まれます。これらはジェット気流、トラフ、前線、安定度、対流圏と下部成層圏のつながりを診断する助けになります。
GribStreamでは、GRIBファイル全体を処理せずに、長い予報範囲の力学的な背景場を取得したい用途に向いています。航空計画、上空診断、研究用途、CFS Pressureとの比較で使えます。
より一般的な大気変数にはCFS Pressureを、地表面やエネルギー収支の文脈にはCFS Radiative Fluxesを使ってください。
パラメータをクリックすると、コピーしやすいJSONセレクタ付きのコンパクトな表で候補を確認できます。コード、level、selector値はAPIが公開する値をそのまま保持します。
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":""}
|
検索に一致するパラメータはありません。