Hypoxic and anoxic regions in the Baltic Sea, 1993

The content of this webpage is part of the Marine Science Report No 100 2016 and should be cited as:

Susanne Feistel, Rainer Feistel, Dietwart Nehring, Wolfgang Matthäus, Günther Nausch, Michael Naumann: Hypoxic and anoxic regions in the Baltic Sea, 1969 - 2015. Meereswiss. Ber., Warnemünde, 100 (2016) doi: 10.12754/msr-2016-0100

All version information and information on further technical development are available via the website https://www.io-warnemuende.de/msr-2016-0100.html

Jan/Feb, 1993: download SVG (computed 2016)	Mar/Apr, 1993
Apr/May, 1993: download SVG (computed 2016)	Jul/Aug, 1993: download SVG (computed 2016)
Oct/Nov, 1993: download SVG (computed 2016)	Apr/May & Oct/Nov, 1993: download SVG (computed 2016)
In January 1993, a very strong MBI occurred (see Table 1) which was of great importance for the oxygen conditions in the whole central Baltic deep water. The event caused an increase in oxygen concentrations in the deep water of the Bornholm and Gdańsk Basins. Favoured by pulsations of the inflow through the Słupsk Furrow short-term fluctuations between oxic and anoxic conditions occurred during the deep water renewal in the eastern Gotland Basin (NEHRING et al., 1994a, 1994b).

References:

• NEHRING, D., MATTHÄUS, W., LASS, H. U., NAUSCH, G., 1994a: Hydrographisch-chemische Zustandseinschätzung der Ostsee 1993. – Meereswiss. Ber., Warnemünde, 7, 1-68, doi: 10.12754/msr-1993-0007
• NEHRING, D., MATTHÄUS, W., LASS, H. U., NAUSCH, G., 1994b: Die hydrographisch-chemischen Bedingungen in der westlichen und zentralen Ostsee im Jahre 1993. – Dtsch. Hydrogr. Z., 46, 151-162.