Shelf basin exchange along the Siberian continental margin: Modification of Atlantic Water and Lower Halocline Water
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- 作者：Dorothea Baucha ; dbauch@geomar.de" class="auth_mail" title="E-mail the corresponding author ; Ekaterina Cherniavskaiaa ; b ; Leonid Timokhovb
- 关键词：Arctic Ocean ; Siberian shelves ; Shelf basin exchange ; Stable oxygen isotopes ; Water masses ; Principal Component Analysis ; Arctic Halocline ; Lower Halocline Water ; Atlantic Water ; Arctic Circumpolar Boundary Current
- 刊名：Deep Sea Research Part I: Oceanographic Research Papers
- 出版年：2016
- 出版时间：September 2016
- 年：2016
- 卷：115
- 期：Complete
- 页码：188-198
- 全文大小：2334 K
文摘
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Atlantic Water modified by sea-ice melt and meteoric water at Barents Sea slope.
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LHW may be divided into different types by Principal Component Analysis (PCA).
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High salinity LHW-type forms in the Barents and Kara seas.
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Low salinity LHW-types form in the western Laptev Sea or enter via Vilkitsky Strait.
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PCA does not support a distinction between onshore and offshore LHW branches.