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  • 1
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    In:  [Poster] In: 1. PhD students conference: Integrated climate and earth system sciences in Northern Germany, 04.-06.10.2010, Hamburg, Germany .
    Publication Date: 2012-07-06
    Description: Knowledge of the parameter K (turbulent diffusivity/"mixing intensity") is a key to understand transport processes of matter and energy in the ocean. Especially the almost vertical component of K across the ocean stratification (diapycnal diffusivity) is vital for research on biogeochemical cycles or greenhouse gas budgets. Recent boost in precision of water velocity data that can be obtained from vessel-mounted acoustic instruments (vmADCP) allows identifying ocean regions of elevated diapycnal diffusivity during research cruises - in high horizontal resolution and without extra ship time needed. This contribution relates acoustic data from two cruises in the Tropical North East Atlantic Oxygen Minimum Zone to simultaneous field observations of diapycnal diffusivity: pointwise measurements by a microstructure profiler as well as one integrative value from a large scale Tracer Release Experiment.
    Type: Conference or Workshop Item , NonPeerReviewed
    Format: text
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  • 2
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    Alfred-Wegener-Institut für Polar- und Meeresforschung
    In:  [Poster] In: Joint Russian-German Workshop on Research in the Laptev Sea Region, 08.11.-11.11.2010, St. Petersburg, Russia . Research in the Laptev Sea region : proceedings of the Joint Russian-German Workshop, November 8-11, 2010, St. Petersburg, Russia / ed. by Sebastian Wetterich ... ; p. 46 .
    Publication Date: 2016-06-03
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 3
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    Universität Bremen
    In:  [Poster] In: Biogeochemical Cycles: German contribution to International JGOFS, 18.-21.09.2000, Bremen, Germany . Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen ; pp. 32-33 .
    Publication Date: 2019-09-11
    Description: We observed variations in primary nutrients and phytoplankton biomass in an upwelling event off Oman during the strong SW-monsoon 1997. A so called filament, originating in the coastal upwelling, was tracked, marked with a drifter and followed for 19 days while intensive water sampling took place. The first stations in this upwelling event showed a severe silicate limitation. With the silicate limitation a diverse diatom community vanished. Although after a couple of days new silicate became available, another phytoplankton community of smaller organisms 〈 20 flm) with nearly no diatoms bloomed. These results raise fundamental questions about the interactions between silicate limitation and the control of carbon export in the worlds most productive areas. It is discussed, whether these limitation events might be typical short term features of coastal upwelling ecosystems, not described as yet.
    Type: Conference or Workshop Item , PeerReviewed
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