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  • 1
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    IFM-GEOMAR
    In:  In: IFM-GEOMAR [Annual] Report 2002-2004 From the Seafloor to the Atmosphere - Marine Sciences at IFM-GEOMAR Kiel -. , ed. by Villwock, A. IFM-GEOMAR, Kiel, Germany, pp. 21-24.
    Publication Date: 2019-03-08
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 2
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    IFM-GEOMAR
    In:  In: IFM-GEOMAR [Annual] Report 2002-2004 From the Seafloor to the Atmosphere - Marine Sciences at IFM-GEOMAR Kiel -. , ed. by Villwock, A. IFM-GEOMAR, Kiel, Germany, pp. 17-20.
    Publication Date: 2019-03-08
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 3
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    IFM-GEOMAR
    In:  In: IFM-GEOMAR Report: From the Seafloor to the Atmosphere - Marine Sciences at IFM-GEOMAR Kiel -. , ed. by Villwock, A. IFM-GEOMAR, Kiel, Germany, pp. 19-20.
    Publication Date: 2019-09-23
    Type: Book chapter , NonPeerReviewed
    Format: text
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  • 4
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    IFM-GEOMAR
    In:  IFM-GEOMAR Annual Report, 2010 . pp. 22-23.
    Publication Date: 2018-10-16
    Description: Globally averaged sea level has risen by just under 10 cm during the last 50 years as a consequence of global warming. The rise, however, is not uniform, neither in time nor in space. Natural climate fluctuations and associated changes in the ocean currents have contributed to the inhomogeneity and is an important factor which will determine the pattern of future sea level rise. While research in the past years has focused on the global-mean trend and its attribution to the melting of glaciers and the thermal expansion of sea water under global warming, attention is shifting to the geographical pattern of sea level change. This is essential for coastal impact assessments, but has not been practical yet because ocean projections from current climate models widely diverge. The improvement of regional sea level prediction requires a better understanding of the underlying dynamical causes.
    Type: Article , NonPeerReviewed
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  • 5
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    IFM-GEOMAR
    In:  IFM-GEOMAR Annual Report, 2009 . pp. 22-23.
    Publication Date: 2018-10-16
    Description: El Niño-Southern Oscillation (ENSO) is the strongest natural climate phenomenon on timescales from months to a few years. Sucessfully modelling and subsequently forecasting ENSO is still a challenge although significant progess has been made during the past decades. IFM-GEOMAR scientists developed a new model which is currently being tested for ENSO applications.
    Type: Article , NonPeerReviewed
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  • 6
    Publication Date: 2018-10-30
    Description: People on the Indian sub-continent are not the only ones to rely on monsoon-induced changes. West Africa has highly variable seasonal rainfalls as well. Whether certain regions in West Africa will be exposed to major rainfall or near-drought conditions is largely determined by water temperatures in the central and eastern equatorial Atlantic. A comprehensive oceanic and atmospheric measurement and modeling program at IFM-GEOMAR is aimed at improving the seasonal predictability of precipitation patterns in countries adjacent to the Gulf of Guinea and the northeastern regions of Brazil. This in turn might lead to early preventive measures in the fight against climate-related diseases, such as dengue fever, malaria, cholera, and meningitis, and might lead to an improved adaptation of agricultural usage to regional climate conditions.
    Type: Article , NonPeerReviewed
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  • 7
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    IFM-GEOMAR
    In:  IFM-GEOMAR [Annual] Report, 2007 . pp. 22-24.
    Publication Date: 2018-10-30
    Description: The strong hurricane activity observed during the last decade fuelled the debate whether global warming is a major force. The crux of the recent debate is the limited length of the reliable instrumental record that exacerbates the detection of possible long-term changes in hurricane activity, which naturally exhibits strong multidecadal variations in association with the Atlantic Multidecadal Oscillation (AMO). We analysed the stable oxygen (δ18O) of a Caribbean brain coral which records both hurricane activity and AMO. This proxy record is equally sensitive to variations in sea surface temperature (SST) and seawater δ18O, with the latter being strongly linked to precipitation and evaporation. The SST and precipitation signals in the coral provide the longest continuous proxybased record of hurricane activity that interestingly exhibits a long-term increase over the last century.
    Type: Article , NonPeerReviewed
    Format: text
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