SWEAT
Term · Meteorology and atmospheric science · MLC-T-MET-002727
Severe Weather ThrEAT index; a stability index developed by the Air Force which incorporates instability, wind shear, and wind speeds as follows:
SWEAT=(12 Td 850 ) + (20 [TT-49]) +( 2 f 850) + f 500 + (125 [s+0.2]) where
• Td 850 is the dew point temperature at 850 mb,
• TT is the total-totals index,
• f 850 is the 850-mb wind speed (in knots),
• f 500 is the 500-mb wind speed (in knots), and
• s is the sine of the angle between the wind directions at 500 mb and 850 mb (thus representing the directional shear in this layer).
SWEAT values of about 250-300 or more indicate a greater potential for severe weather, but as with all stability indices, there are no magic numbers.
The SWEAT index has the advantage (and disadvantage) of using only mandatory-level data (i.e., 500 mb and 850 mb), but has fallen into relative disuse with the advent of more detailed upper air sounding analysis programs.
| Identifier | MLC-T-MET-002727 |
|---|---|
| Field | Meteorology and atmospheric science |
| References | NWS Glossary |
Record as JSON
{
"id": "MLC-T-MET-002727",
"term": "SWEAT",
"field": "Meteorology and atmospheric science",
"definition": "Severe Weather ThrEAT index; a stability index developed by the Air Force which incorporates instability, wind shear, and wind speeds as follows:\n\nSWEAT=(12 Td 850 ) + (20 [TT-49]) +( 2 f 850) + f 500 + (125 [s+0.2]) where\n\n• Td 850 is the dew point temperature at 850 mb,\n\n• TT is the total-totals index,\n\n• f 850 is the 850-mb wind speed (in knots),\n\n• f 500 is the 500-mb wind speed (in knots), and\n\n• s is the sine of the angle between the wind directions at 500 mb and 850 mb (thus representing the directional shear in this layer).\n\nSWEAT values of about 250-300 or more indicate a greater potential for severe weather, but as with all stability indices, there are no magic numbers.\n\nThe SWEAT index has the advantage (and disadvantage) of using only mandatory-level data (i.e., 500 mb and 850 mb), but has fallen into relative disuse with the advent of more detailed upper air sounding analysis programs.",
"references": [
"NWS Glossary"
],
"url": "https://mlchart.com/terminology/meteorology/sweat/"
}
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