Satellite remote sensing of primary production in the Bering Sea
| dc.contributor.author | Anugerahanti, P. | |
| dc.date.accessioned | 2019-05-16T15:49:32Z | |
| dc.date.available | 2019-05-16T15:49:32Z | |
| dc.date.issued | 2014 | |
| dc.identifier.citation |
Anugerahanti, P. (2014) 'Satellite remote sensing of primary production in the Bering Sea', The Plymouth Student Scientist, 7(2), p. 195-202. | en_US |
| dc.identifier.issn | 1754-2383 | |
| dc.identifier.uri | http://hdl.handle.net/10026.1/14075 | |
| dc.description | The Bering Sea covers over 2 million square kilometres of the northernmost region of the Pacific Ocean (NPO, 2008), and is considered to be one of the most productive seas in the world (Walsh et al., 1989). Linking the Pacific and Arctic Oceans, the Bering Sea is almost entirely surrounded by the landmasses of Alaska and Russia. A steep continental slope divides this sea between the expansive continental shelf (<200 m depth) on its eastern waters and the deep basin (>2000 m depth) to the west (Brown et al., 2011)... | en_US |
| dc.language.iso | en | en_US |
| dc.publisher | University of Plymouth | |
| dc.rights | Attribution 3.0 United States | * |
| dc.rights.uri | http://creativecommons.org/licenses/by/3.0/us/ | * |
| dc.subject | Bering Sea | en_US |
| dc.subject | satellite remote sensing | en_US |
| dc.subject | sea-ice loss | en_US |
| dc.title | Satellite remote sensing of primary production in the Bering Sea | en_US |
| dc.type | Article | |
| plymouth.issue | 2 | |
| plymouth.volume | 7 | |
| plymouth.journal | The Plymouth Student Scientist |
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