Changes in Seasonality of Saltwater Inflows Caused Exceptional Warming Trends in the Western Baltic Sea

Autor: Barghorn, L., Meier, H. E. M., Radtke, H.

During the last decades, the Baltic Sea has been among the fastest warming seas in the world. The warming is mainly driven by increasing air temperatures but deeper water layers can also be warmed by lateral advection of heat. By analyzing a 159 year

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______2497::546afd4a5963748c1bfba7d341b6ac05
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10846

Rhine flood stories: Spatio‐temporal analysis of historic and projected flood genesis in the Rhine River basin

Autor: Rottler, Erwin, Bronstert, Axel, Bürger, Gerd, Rakovec, Oldrich

The genesis of floods in large river basins often is complex. Streamflow originating from precipitation and snowmelt and different tributaries can superimpose and cause high water levels, threatening cities and communities along the riverbanks. For b

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______2497::b3474fe952cfb88bcaf0163e36b1f6fb
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10853

Holocene variability in sea‐ice conditions in the eastern Baffin Bay‐Labrador Sea – A north–south biomarker transect study

Autor: Saini, Jeetendra, Stein, Ruediger, Fahl, Kirsten, Weiser, Jens, Hebbeln, Dierk, Madaj, Lina, 1 Alfred‐Wegener‐Institute Helmholtz Centre for Polar and Marine Research Am Alten Hafen 26 27568 Bremerhaven Germany, 2 MARUM‐Center for Marine Environmental Sciences University of Bremen Leobener Str. 8 28359 Bremen Germany

Publikováno v: Boreas. 51:553-572

Reconstructions of sea‐surface conditions during the Holocene were achieved using three sediment cores from northeastern Baffin Bay (GeoB19948‐3 and GeoB19927‐3) and the Labrador Sea (GeoB19905‐1) along a north–south transect based on sea�

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3ed98bc29a01d3953672e1964301ec44
https://doi.org/10.1111/bor.12583

Evolution of Global Ocean Tide Levels Since the Last Glacial Maximum

Autor: Sulzbach, R., Klemann, V., Knorr, G., Dobslaw, H., Dümpelmann, H., Lohmann, G., Thomas, M.

Publikováno v: Paleoceanography and Paleoclimatology
Paleoceanography and paleoclimatology 38(5), e2022PA004556 (2023). doi:10.1029/2022PA004556

This study addresses the evolution of global tidal dynamics since the Last Glacial Maximum focusing on the extraction of tidal levels that are vital for the interpretation of geologic sea‐level markers. For this purpose, we employ a truly‐global

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f819118204ab52240d2667c6cca8fe26
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5016678_2/component/file_5019733/5016678.pdf

Surface Wave and Roller Dissipation Observed With Shore‐Based Doppler Marine Radar

Autor: Streßer, Michael, Horstmann, Jochen, Baschek, Burkard, 1 Helmholtz‐Zentrum Hereon Geesthacht Germany

Publikováno v: Streßer, M.; Horstmann, J.; Baschek, B.: Surface Wave and Roller Dissipation Observed With Shore-Based Doppler Marine Radar. In: Journal of Geophysical Research : Oceans. Vol. 127 (2022) 8, e2022JC018437. (DOI: /10.1029/2022JC018437)

Surface wave energy and dissipation are observed across the surf zone. Utilizing the concept of surface rollers, a new scaling is introduced to obtain the energy flux and dissipation related to rollers from Doppler velocities measured by a shore‐ba

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::080cd1c321bd1363aa057086906ddd9b
http://resolver.sub.uni-goettingen.de/purl?gldocs-11858/10407