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DOI | https://doi.org/10.1594/PANGAEA.726958 |
Biogeochemistry of the Eastern Weddell Gyre | |
Geibert; Walter; Assmy; Philipp; Bakker; Dorothee C E; Hanfland; Claudia; Hoppema; Mario; Pichevin; Laetitia; Schröder; Michael; Schwarz; Jill Nicola; Stimac; Ingrid; Usbeck; Regina; Webb; Adrian | |
发布日期 | 2010-02-25 |
数据集类型 | dataset |
英文简介 | The Southern Ocean (SO) plays a key role in modulating atmospheric CO2 via physical and biological processes. However, over much of the SO, biological activity is iron-limited. New in situ data from the Antarctic zone south of Africa in a region centered at -20°E - 25°E reveal a previously overlooked region of high primary production, comparable in size to the northwest African upwelling region. Here, sea ice together with enclosed icebergs is channeled by prevailing winds to the eastern boundary of the Weddell Gyre, where a sharp transition to warmer waters causes melting. This cumulative melting provides a steady source of iron, fuelling an intense phytoplankton bloom that is not fully captured by monthly satellite production estimates. These findings imply that future changes in sea-ice cover and dynamics could have a significant effect on carbon sequestration in the SO. |
空间范围 | Median Latitude: -58.318302 * Median Longitude: 13.626925 * South-bound Latitude: -69.889000 * West-bound Longitude: -0.112300 * North-bound Latitude: -35.963800 * East-bound Longitude: 25.233800 |
时间范围 | 2002-11-26T06:08:00 - 2003-01-21T15:02:00 |
语种 | 英语 |
国家 | 国际 |
学科大类 | 气候变化 |
学科子类 | 气候变化 |
文献类型 | 数据集 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/219991 |
推荐引用方式 GB/T 7714 | Geibert,Walter,Assmy,et al. Biogeochemistry of the Eastern Weddell Gyre.2010-02-25.https://doi.org/10.1594/PANGAEA.726958. |
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