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Christian M. Grams

Researcher at Karlsruhe Institute of Technology

Publications -  78
Citations -  2665

Christian M. Grams is an academic researcher from Karlsruhe Institute of Technology. The author has contributed to research in topics: Extratropical cyclone & Middle latitudes. The author has an hindex of 23, co-authored 59 publications receiving 1931 citations. Previous affiliations of Christian M. Grams include ETH Zurich.

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Balancing Europe’s wind-power output through spatial deployment informed by weather regimes

TL;DR: It is shown that weather regimes provide a meteorological explanation for multi-day fluctuations in Europe’s wind power and can help guide new deployment pathways which minimise this variability.
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The key role of diabatic processes in modifying the upper-tropospheric wave guide: a North Atlantic case-study

TL;DR: In this article, the authors highlight the importance of diabatic processes for the complex interaction of weather systems in the North Atlantic-European sector during the week of 7-14 September 2008.
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Importance of latent heat release in ascending air streams for atmospheric blocking

TL;DR: In this paper, a Lagrangian approach applied to reanalysis data shows that a large fraction of air masses are heated before entering a blocking system, pointing to a role for latent heating.
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Atmospheric processes triggering the central European floods in June 2013

TL;DR: In this paper, the authors investigated the key atmospheric processes that caused the 2013 Danube and Elbe flood in central Europe and found that the continuous large-scale slantwise ascent in so-called "equatorward ascending" warm conveyor belts (WCBs) associated with these cyclones was the key process that caused a 4 day heavy precipitation period.
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Uplift of Saharan dust south of the intertropical discontinuity

TL;DR: In situ observations from a flight made during the Geostationary Earth Radiation (GERBILS) field campaign (June 2007) show significant dust uplift into the monsoon flow immediately south of the intertropical discontinuity in the western Sahara.