Mechanisms controlling the SST air-sea heat flux feedback and its dependence on spatial scale
The turbulent air-sea heat flux feedback (α, in W m[superscript −2] K[superscript −1]) is a major contributor to setting the damping timescale of sea surface temperature (SST) anomalies. In this study we compare the spatial distribution and magnitude of αα in the North Atlantic and the Southern Oc...
| 主要な著者: | , , |
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| その他の著者: | |
| フォーマット: | 論文 |
| 言語: | English |
| 出版事項: |
Springer Berlin Heidelberg
2017
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| オンライン･アクセス: | http://hdl.handle.net/1721.1/107385 https://orcid.org/0000-0002-8195-5938 https://orcid.org/0000-0001-9230-3591 |