Investigations in the Szczecin Lagoon during the Oder Flood (July – August 1997) from a biogeochemical perspective
Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a...
Ausführliche Beschreibung
Autor*in: |
Fenske, Christiane [verfasserIn] |
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Artikel |
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Sprache: |
Englisch |
Erschienen: |
1998 |
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Anmerkung: |
© BSH, Hamburg und Rostock 1998 |
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Übergeordnetes Werk: |
Enthalten in: Deutsche hydrographische Zeitschrift - Springer-Verlag, 1948, 50(1998), 2-3 vom: Juni, Seite 231-243 |
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Übergeordnetes Werk: |
volume:50 ; year:1998 ; number:2-3 ; month:06 ; pages:231-243 |
Links: |
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DOI / URN: |
10.1007/BF02764489 |
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Katalog-ID: |
OLC2070854043 |
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520 | |a Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a third of the normal annual Oder discharge of 17 $ km^{3} $. The flow was strongly enhanced by the large difference (approx. 30 cm) between the water levels of the Szczecin Lagoon and the Baltic Sea. However, the Szczecin Lagoon (=Oderhaff) was not as much affected as the upper course of the river. The substances transported, such as nutrients and pollutants, did not cause much harm, due to strong dilution. Hygienic investigations proved the water to have bathing quality during the whole flood. In this paper results of biogeochemical investigations in the period of the Oder flood (July/August 1997) are presented and compared with long-term data. | ||
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10.1007/BF02764489 doi (DE-627)OLC2070854043 (DE-He213)BF02764489-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Fenske, Christiane verfasserin aut Investigations in the Szczecin Lagoon during the Oder Flood (July – August 1997) from a biogeochemical perspective 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © BSH, Hamburg und Rostock 1998 Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a third of the normal annual Oder discharge of 17 $ km^{3} $. The flow was strongly enhanced by the large difference (approx. 30 cm) between the water levels of the Szczecin Lagoon and the Baltic Sea. However, the Szczecin Lagoon (=Oderhaff) was not as much affected as the upper course of the river. The substances transported, such as nutrients and pollutants, did not cause much harm, due to strong dilution. Hygienic investigations proved the water to have bathing quality during the whole flood. In this paper results of biogeochemical investigations in the period of the Oder flood (July/August 1997) are presented and compared with long-term data. Atrazine Suspended Particulate Matter Particulate Organic Carbon Suspended Particulate Matter Concentration German Journal Westphal, Helmut aut Bachor, Alexander aut Breitenbach, Elke aut Meyer, Hinrich aut Buchholz, Wladyslaw aut Jülich, Wolf-Dieter aut Enthalten in Deutsche hydrographische Zeitschrift Springer-Verlag, 1948 50(1998), 2-3 vom: Juni, Seite 231-243 (DE-627)129464031 (DE-600)201122-0 (DE-576)014829320 0012-0308 nnns volume:50 year:1998 number:2-3 month:06 pages:231-243 https://doi.org/10.1007/BF02764489 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_160 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_201 GBV_ILN_235 GBV_ILN_600 GBV_ILN_601 GBV_ILN_608 GBV_ILN_2010 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4305 AR 50 1998 2-3 06 231-243 |
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10.1007/BF02764489 doi (DE-627)OLC2070854043 (DE-He213)BF02764489-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Fenske, Christiane verfasserin aut Investigations in the Szczecin Lagoon during the Oder Flood (July – August 1997) from a biogeochemical perspective 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © BSH, Hamburg und Rostock 1998 Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a third of the normal annual Oder discharge of 17 $ km^{3} $. The flow was strongly enhanced by the large difference (approx. 30 cm) between the water levels of the Szczecin Lagoon and the Baltic Sea. However, the Szczecin Lagoon (=Oderhaff) was not as much affected as the upper course of the river. The substances transported, such as nutrients and pollutants, did not cause much harm, due to strong dilution. Hygienic investigations proved the water to have bathing quality during the whole flood. In this paper results of biogeochemical investigations in the period of the Oder flood (July/August 1997) are presented and compared with long-term data. Atrazine Suspended Particulate Matter Particulate Organic Carbon Suspended Particulate Matter Concentration German Journal Westphal, Helmut aut Bachor, Alexander aut Breitenbach, Elke aut Meyer, Hinrich aut Buchholz, Wladyslaw aut Jülich, Wolf-Dieter aut Enthalten in Deutsche hydrographische Zeitschrift Springer-Verlag, 1948 50(1998), 2-3 vom: Juni, Seite 231-243 (DE-627)129464031 (DE-600)201122-0 (DE-576)014829320 0012-0308 nnns volume:50 year:1998 number:2-3 month:06 pages:231-243 https://doi.org/10.1007/BF02764489 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_160 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_201 GBV_ILN_235 GBV_ILN_600 GBV_ILN_601 GBV_ILN_608 GBV_ILN_2010 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4305 AR 50 1998 2-3 06 231-243 |
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10.1007/BF02764489 doi (DE-627)OLC2070854043 (DE-He213)BF02764489-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Fenske, Christiane verfasserin aut Investigations in the Szczecin Lagoon during the Oder Flood (July – August 1997) from a biogeochemical perspective 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © BSH, Hamburg und Rostock 1998 Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a third of the normal annual Oder discharge of 17 $ km^{3} $. The flow was strongly enhanced by the large difference (approx. 30 cm) between the water levels of the Szczecin Lagoon and the Baltic Sea. However, the Szczecin Lagoon (=Oderhaff) was not as much affected as the upper course of the river. The substances transported, such as nutrients and pollutants, did not cause much harm, due to strong dilution. Hygienic investigations proved the water to have bathing quality during the whole flood. In this paper results of biogeochemical investigations in the period of the Oder flood (July/August 1997) are presented and compared with long-term data. Atrazine Suspended Particulate Matter Particulate Organic Carbon Suspended Particulate Matter Concentration German Journal Westphal, Helmut aut Bachor, Alexander aut Breitenbach, Elke aut Meyer, Hinrich aut Buchholz, Wladyslaw aut Jülich, Wolf-Dieter aut Enthalten in Deutsche hydrographische Zeitschrift Springer-Verlag, 1948 50(1998), 2-3 vom: Juni, Seite 231-243 (DE-627)129464031 (DE-600)201122-0 (DE-576)014829320 0012-0308 nnns volume:50 year:1998 number:2-3 month:06 pages:231-243 https://doi.org/10.1007/BF02764489 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_160 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_201 GBV_ILN_235 GBV_ILN_600 GBV_ILN_601 GBV_ILN_608 GBV_ILN_2010 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4305 AR 50 1998 2-3 06 231-243 |
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10.1007/BF02764489 doi (DE-627)OLC2070854043 (DE-He213)BF02764489-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Fenske, Christiane verfasserin aut Investigations in the Szczecin Lagoon during the Oder Flood (July – August 1997) from a biogeochemical perspective 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © BSH, Hamburg und Rostock 1998 Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a third of the normal annual Oder discharge of 17 $ km^{3} $. The flow was strongly enhanced by the large difference (approx. 30 cm) between the water levels of the Szczecin Lagoon and the Baltic Sea. However, the Szczecin Lagoon (=Oderhaff) was not as much affected as the upper course of the river. The substances transported, such as nutrients and pollutants, did not cause much harm, due to strong dilution. Hygienic investigations proved the water to have bathing quality during the whole flood. In this paper results of biogeochemical investigations in the period of the Oder flood (July/August 1997) are presented and compared with long-term data. Atrazine Suspended Particulate Matter Particulate Organic Carbon Suspended Particulate Matter Concentration German Journal Westphal, Helmut aut Bachor, Alexander aut Breitenbach, Elke aut Meyer, Hinrich aut Buchholz, Wladyslaw aut Jülich, Wolf-Dieter aut Enthalten in Deutsche hydrographische Zeitschrift Springer-Verlag, 1948 50(1998), 2-3 vom: Juni, Seite 231-243 (DE-627)129464031 (DE-600)201122-0 (DE-576)014829320 0012-0308 nnns volume:50 year:1998 number:2-3 month:06 pages:231-243 https://doi.org/10.1007/BF02764489 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_160 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_201 GBV_ILN_235 GBV_ILN_600 GBV_ILN_601 GBV_ILN_608 GBV_ILN_2010 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4305 AR 50 1998 2-3 06 231-243 |
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10.1007/BF02764489 doi (DE-627)OLC2070854043 (DE-He213)BF02764489-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Fenske, Christiane verfasserin aut Investigations in the Szczecin Lagoon during the Oder Flood (July – August 1997) from a biogeochemical perspective 1998 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © BSH, Hamburg und Rostock 1998 Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a third of the normal annual Oder discharge of 17 $ km^{3} $. The flow was strongly enhanced by the large difference (approx. 30 cm) between the water levels of the Szczecin Lagoon and the Baltic Sea. However, the Szczecin Lagoon (=Oderhaff) was not as much affected as the upper course of the river. The substances transported, such as nutrients and pollutants, did not cause much harm, due to strong dilution. Hygienic investigations proved the water to have bathing quality during the whole flood. In this paper results of biogeochemical investigations in the period of the Oder flood (July/August 1997) are presented and compared with long-term data. Atrazine Suspended Particulate Matter Particulate Organic Carbon Suspended Particulate Matter Concentration German Journal Westphal, Helmut aut Bachor, Alexander aut Breitenbach, Elke aut Meyer, Hinrich aut Buchholz, Wladyslaw aut Jülich, Wolf-Dieter aut Enthalten in Deutsche hydrographische Zeitschrift Springer-Verlag, 1948 50(1998), 2-3 vom: Juni, Seite 231-243 (DE-627)129464031 (DE-600)201122-0 (DE-576)014829320 0012-0308 nnns volume:50 year:1998 number:2-3 month:06 pages:231-243 https://doi.org/10.1007/BF02764489 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_23 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_154 GBV_ILN_160 GBV_ILN_170 GBV_ILN_171 GBV_ILN_183 GBV_ILN_201 GBV_ILN_235 GBV_ILN_600 GBV_ILN_601 GBV_ILN_608 GBV_ILN_2010 GBV_ILN_2315 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4029 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4305 AR 50 1998 2-3 06 231-243 |
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investigations in the szczecin lagoon during the oder flood (july – august 1997) from a biogeochemical perspective |
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Investigations in the Szczecin Lagoon during the Oder Flood (July – August 1997) from a biogeochemical perspective |
abstract |
Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a third of the normal annual Oder discharge of 17 $ km^{3} $. The flow was strongly enhanced by the large difference (approx. 30 cm) between the water levels of the Szczecin Lagoon and the Baltic Sea. However, the Szczecin Lagoon (=Oderhaff) was not as much affected as the upper course of the river. The substances transported, such as nutrients and pollutants, did not cause much harm, due to strong dilution. Hygienic investigations proved the water to have bathing quality during the whole flood. In this paper results of biogeochemical investigations in the period of the Oder flood (July/August 1997) are presented and compared with long-term data. © BSH, Hamburg und Rostock 1998 |
abstractGer |
Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a third of the normal annual Oder discharge of 17 $ km^{3} $. The flow was strongly enhanced by the large difference (approx. 30 cm) between the water levels of the Szczecin Lagoon and the Baltic Sea. However, the Szczecin Lagoon (=Oderhaff) was not as much affected as the upper course of the river. The substances transported, such as nutrients and pollutants, did not cause much harm, due to strong dilution. Hygienic investigations proved the water to have bathing quality during the whole flood. In this paper results of biogeochemical investigations in the period of the Oder flood (July/August 1997) are presented and compared with long-term data. © BSH, Hamburg und Rostock 1998 |
abstract_unstemmed |
Summary Caused by both an exceptional meteorological situation, especially high precipitation, and anthropogenic factors (melioration), the level of the river Oder rose quickly within a few days in July 97. An additional 5 $ km^{3} $ of water were discharged during the flood. This represents about a third of the normal annual Oder discharge of 17 $ km^{3} $. The flow was strongly enhanced by the large difference (approx. 30 cm) between the water levels of the Szczecin Lagoon and the Baltic Sea. However, the Szczecin Lagoon (=Oderhaff) was not as much affected as the upper course of the river. The substances transported, such as nutrients and pollutants, did not cause much harm, due to strong dilution. Hygienic investigations proved the water to have bathing quality during the whole flood. In this paper results of biogeochemical investigations in the period of the Oder flood (July/August 1997) are presented and compared with long-term data. © BSH, Hamburg und Rostock 1998 |
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