Ocean Cooling Pattern at the Last Glacial Maximum
Ocean temperature and ocean heat content change are analyzed based on four PMIP3 model results at the Last Glacial Maximum relative to the prehistorical run. Ocean cooling mostly occurs in the upper 1000 m depth and varies spatially in the tropical and temperate zones. The Atlantic Ocean experiences...
| Hlavní autoři: | , |
|---|---|
| Médium: | Článek |
| Jazyk: | English |
| Vydáno: |
Wiley
2012-01-01
|
| Edice: | Advances in Meteorology |
| On-line přístup: | http://dx.doi.org/10.1155/2012/213743 |