Thermohaline circulations and global climate change. Annual progress report No. 2, [15 January 1991--14 January 1992]
``Thermohaline Circulations and Global Climate Change`` is concerned with investigating the hypothesis that changes in surface thermal and hydrological forcing of the North Atlantic, changes that might be expected to accompany CO{sub 2}-induced global warming, could result in ocean-atmosphere interactions` exerting a positive feedback on the climate system. Because the North Atlantic is the source of much of the global ocean`s reservoir of deep water, and because this deep water could sequester large amounts of anthropogenically produced Co{sub 2}, changes in the rate of deep-water production are important to future climates. Since deep-water production is controlled, in part, by the annual cycle of the atmospheric forcing of the North Atlantic, and since this forcing depends strongly on both hydrological and thermal processes as well as the windstress, there is the potential for feedback between the relatively short-term response of the atmosphere to changing radiative forcing and the longer-term processes in the oceans. Work over the past 12 months has proceeded in several directions.
- Research Organization:
- Colorado Univ., Boulder, CO (United States). Cooperative Inst. for Research in Environmental Sciences
- Sponsoring Organization:
- USDOE, Washington, DC (United States)
- DOE Contract Number:
- FG02-90ER61019
- OSTI ID:
- 10126906
- Report Number(s):
- DOE/ER/61019-2; ON: DE92008796
- Resource Relation:
- Other Information: PBD: [1992]
- Country of Publication:
- United States
- Language:
- English
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