T
Tapani Stipa
Researcher at Finnish Meteorological Institute
Publications - 25
Citations - 1031
Tapani Stipa is an academic researcher from Finnish Meteorological Institute. The author has contributed to research in topics: Halocline & Baroclinity. The author has an hindex of 16, co-authored 25 publications receiving 865 citations. Previous affiliations of Tapani Stipa include University of Helsinki & Finnish Institute of Marine Research.
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A modelling system for the exhaust emissions of marine traffic and its application in the Baltic Sea area
TL;DR: In this paper, a method is presented for the evaluation of the exhaust emissions of marine traffic, based on the messages provided by the Automatic Identification System (AIS), which enable the identification and location determination of ships.
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Extension of an assessment model of ship traffic exhaust emissions for particulate matter and carbon monoxide
TL;DR: In this paper, the authors presented a method for the evaluation of the exhaust emissions of marine traffic, based on the messages provided by the Automatic Identification System (AIS), which enable the positioning of ship emissions with a high spatial resolution (typically a few tens of metres).
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A dynamic Biologically-Active Layer for numerical studies of the sea ice ecosystem.
TL;DR: In this article, a simple but comprehensive physical model of the sea ice thermo-halodynamics is coupled to a novel sea ice microalgal model of growth in the framework of the Biogeochemical Flux Model.
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On the creation and maintenance of stratification in the Gulf of Riga
TL;DR: In this article, the authors studied the role of buoyancy forcing in the creation and maintenance of stratification in a boreal estuary (Gulf of Riga, Baltic Sea).
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Generation of subsurface cyclonic eddies in the southeast Baltic Sea: Observations and numerical experiments
Victor Zhurbas,Tapani Stipa,Pentti Mälkki,V. T. Paka,Nikolai Golenko,Inga Hense,Vladimir Sklyarov +6 more
TL;DR: In this paper, a numerical simulation based on the Princeton Ocean Model (POM) has been initiated to examine processes capable of forming the observed cyclonic eddies, which may be interpreted as geostrophically balanced cyclonic edges in the intermediate layer.