1981
DOI: 10.1016/0025-326x(81)90168-5
|View full text |Cite
|
Sign up to set email alerts
|

The Baltic Sea: an outline of its physical oceanography

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
29
0

Year Published

1985
1985
2018
2018

Publication Types

Select...
7
2
1

Relationship

0
10

Authors

Journals

citations
Cited by 56 publications
(29 citation statements)
references
References 7 publications
0
29
0
Order By: Relevance
“…In the eastern Baltic Sea, circulation patterns in the upper layer of the Baltic are dominated by wind conditions (Kullenberg & Jacobsen 1981, Moller & Hansen 1994. However, cod eggs are generally located near the permanent halocline at depths of 50 to 70 m and below the sill depths (Wieland et al 1994).…”
Section: Effects Of Wind-induced Transport On Egg and Larval Distribumentioning
confidence: 99%
“…In the eastern Baltic Sea, circulation patterns in the upper layer of the Baltic are dominated by wind conditions (Kullenberg & Jacobsen 1981, Moller & Hansen 1994. However, cod eggs are generally located near the permanent halocline at depths of 50 to 70 m and below the sill depths (Wieland et al 1994).…”
Section: Effects Of Wind-induced Transport On Egg and Larval Distribumentioning
confidence: 99%
“…Below this exists a 10 m layer, termed the upper deep-water pycnocline, which overlies the deep saline (10 to 18 ‰) waters of the Baltic. A seasonal thermocline is found at 30 to 40 m in July to September, with relatively homogeneous surface mixed layer down to the halocline during fall/winter (Kullenberg & Jacobsen 1981, Matthäus & Franck 1992, Møller & Hansen 1994, Schinke & Matthäus 1998.…”
Section: Introductionmentioning
confidence: 98%
“…Since the residence time of the water in the Baltic is as long as 25-35 years, and the average depth is not more than about 60 m, sediments here play an essential role in the biogeochemical cycles of nutrient elements and carbon. The semi-permanent anoxic conditions in the Baltic are due to the limited water exchange with the Kattegat and the strong vertical stratification (e.g., Kullenberg and Jacobsen, 1981;Stigebrandt, 2001). These physical characteristics in combination with an increased nutrient supply have led to an increased frequency of cyanobacteria blooms in the Baltic proper since the 1960s (e.g.…”
Section: Introductionmentioning
confidence: 99%