Unusual Baltic inflow activity in 2002-2003 and varying deep-water properties
Unusual Baltic inflow activity in 2002-2003 and varying deep-water properties
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2002-2003 年不寻常的波罗的海流入活动和不同的深水特性
DOI：
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发表时间：
2006
期刊：
影响因子：
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通讯作者：
E. Hagen
中科院分区：
文献类型：
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作者：
R. Feistel;G. Nausch;E. Hagen
2002年和2003年发生的波罗的海入流事件的不寻常序列包括首次描述的重要斜压入流（2002年8月），主要的波罗的海流入（2003年1月），这导致了自20世纪30年代以来哥特兰深海最高的氧气水平，斜压入流（2003年8月）使哥特兰盆地深水盐度升高到1977年最后观测到的值，并导致表面盐度再次上升。根据这些趋势变化，盐的停留时间估计在深水沃茨中约为20年，在密度跃层以上约为30年。直到2005年，在流入事件发生两年后，偏远的卡尔索深海的通风才得以恢复，当时博恩霍尔姆和东哥特兰盆地已经恢复停滞。* 本文于2005年在波兰索波特举行的波罗的海科学大会上发表。它引用了几个相关的BSSC演示文稿为“未发布”。其中一些可能在BSSC程序中发表，但在本文完成时这些作者不知道。该论文的全文可在http://www.iopan.gda.pl/oceanologia/上查阅。Feistel，G. Nausch，E.哈根
The unusual sequence of inflow events into the Baltic Sea that occurred in 2002 and 2003 includes the first ever important baroclinic inflow to be described (August 2002), the Major Baltic Inflow (January 2003), which gave rise to the highest oxygen levels in the Gotland Deep since the 1930s, and the baroclinic inflow (August 2003) that elevated the Gotland Basin deep water salinity to values last observed in 1977, and caused the surface salinity to rise again. From these trend changes, salt residence times were estimated at about 20 years in the deep waters and 30 years above the pycnocline. Ventilation of the remote Karlsö Deep took until 2005, two years after the inflow event responsible, at a time when the Bornholm and Eastern Gotland Basins were already returning to stagnation. * This paper was presented at the Baltic Sea Science Congress in Sopot, Poland, 2005(BSSC). It references several related BSSC presentations as ‘unpublished’. Some of those may be published in the BSSC proceedings, yet unknown to these authors at the time this paper was completed. The complete text of the paper is available at http://www.iopan.gda.pl/oceanologia/ 22 R. Feistel, G. Nausch, E. Hagen