Antarctic Bottom Water
Term · Meteorology and atmospheric science · MLC-T-MET-003538
AABW is a very cold, dense, and saline water mass that forms in the Weddell Sea and Ross Sea around Antarctica. It sinks to the deepest parts of the ocean basins and spreads northward, influencing global ocean circulation patterns. This water mass is characterized by temperatures near freezing and high oxygen content.
| Identifier | MLC-T-MET-003538 |
|---|---|
| Field | Meteorology and atmospheric science |
| Abbreviation | AABW |
Record as JSON
{
"id": "MLC-T-MET-003538",
"term": "Antarctic Bottom Water",
"field": "Meteorology and atmospheric science",
"definition": "AABW is a very cold, dense, and saline water mass that forms in the Weddell Sea and Ross Sea around Antarctica. It sinks to the deepest parts of the ocean basins and spreads northward, influencing global ocean circulation patterns. This water mass is characterized by temperatures near freezing and high oxygen content.",
"abbreviation": "AABW",
"url": "https://mlchart.com/terminology/meteorology/antarctic-bottom-water/"
}
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