Upper ocean climate of the Eastern Mediterranean Sea during the Holocene Insolation Maximum – a model study
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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Online-Ressource
- Language
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Englisch
- Bibliographic citation
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Upper ocean climate of the Eastern Mediterranean Sea during the Holocene Insolation Maximum – a model study ; volume:7 ; number:4 ; year:2011 ; pages:1103-1122
Climate of the past ; 7, Heft 4 (2011), 1103-1122
- Creator
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Adloff, F.
Mikolajewicz, U.
Kučera, M.
Grimm, R.
Maier-Reimer, E.
Schmiedl, G.
Emeis, K.-C.
- DOI
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10.5194/cp-7-1103-2011
- URN
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urn:nbn:de:101:1-201710276648
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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15.08.2025, 7:36 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Adloff, F.
- Mikolajewicz, U.
- Kučera, M.
- Grimm, R.
- Maier-Reimer, E.
- Schmiedl, G.
- Emeis, K.-C.
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Corrigendum to "Upper ocean climate of the Eastern Mediterranean Sea during the Holocene Insolation Maximum – a model study" published in Clim. Past, 7, 1103–1122, 2011
Modelling Mediterranean ocean biogeochemistry of the Last Glacial Maximum
Modeling Mediterranean Ocean climate of the Last Glacial Maximum
Early Holocene Eastern Mediterranean ocean climate and the stability of its overturning circulation
Simulating the early Holocene eastern Mediterranean sapropel formation using an ocean biogeochemical model
Deglacial to holocene changes in Eastern Equatorial Pacific upper-ocean dynamics- indications from foraminiferal (isotope) geochemistry
Deglacial to Holocene Changes in Eastern Equatorial Pacific Upper‐Ocean Dynamics – Indications from Foraminiferal (Isotope) Geochemistry
Complex spatio-temporal structure of the Holocene Thermal Maximum
Upper holocene tephro-chronostratigraphy of Irazú Volcano, Costa Rica
Mid-Holocene ocean and vegetation feedbacks over East Asia
Surface signature of Mediterranean water eddies in the Northeastern Atlantic: effect of the upper ocean stratification
Western Mediterranean hydro-climatic consequences of Holocene iceberg advances (Bond events)
Corrigendum to "Upper ocean climate of the Eastern Mediterranean Sea during the Holocene Insolation Maximum – a model study" published in Clim. Past, 7, 1103–1122, 2011
Modelling Mediterranean ocean biogeochemistry of the Last Glacial Maximum
Modeling Mediterranean Ocean climate of the Last Glacial Maximum
Early Holocene Eastern Mediterranean ocean climate and the stability of its overturning circulation
Simulating the early Holocene eastern Mediterranean sapropel formation using an ocean biogeochemical model
Deglacial to holocene changes in Eastern Equatorial Pacific upper-ocean dynamics- indications from foraminiferal (isotope) geochemistry
Deglacial to Holocene Changes in Eastern Equatorial Pacific Upper‐Ocean Dynamics – Indications from Foraminiferal (Isotope) Geochemistry
Complex spatio-temporal structure of the Holocene Thermal Maximum
Upper holocene tephro-chronostratigraphy of Irazú Volcano, Costa Rica
Mid-Holocene ocean and vegetation feedbacks over East Asia
Surface signature of Mediterranean water eddies in the Northeastern Atlantic: effect of the upper ocean stratification