Tropical upper-tropospheric trough
Term · Meteorology and atmospheric science · MLC-T-MET-009810
A trough of low pressure situated in the upper levels of the troposphere, typically between 200 and 300 millibars, over tropical and subtropical latitudes. These cold-core systems, with the coldest temperatures at their center, are most common during the summer and early autumn in their respective hemispheres. A tropical upper-tropospheric trough can create vertical wind shear that hinders tropical cyclone formation, or it can provide an outflow channel that supports a storm's intensification.
| Identifier | MLC-T-MET-009810 |
|---|---|
| Field | Meteorology and atmospheric science |
Record as JSON
{
"id": "MLC-T-MET-009810",
"term": "Tropical upper-tropospheric trough",
"field": "Meteorology and atmospheric science",
"definition": "A trough of low pressure situated in the upper levels of the troposphere, typically between 200 and 300 millibars, over tropical and subtropical latitudes. These cold-core systems, with the coldest temperatures at their center, are most common during the summer and early autumn in their respective hemispheres. A tropical upper-tropospheric trough can create vertical wind shear that hinders tropical cyclone formation, or it can provide an outflow channel that supports a storm's intensification.",
"url": "https://mlchart.com/terminology/meteorology/tropical-upper-tropospheric-trough/"
}
Record 9,854 of 10,703 in Meteorology and atmospheric science terminology (MLC-0110). Request the full dataset.