Simulation of the katabatic flow near the Greenland ice margin using a high-resolution nonhydrostatic model

Simulations of the katabatic wind system in the stable boundary layer near the margin of the Greenland ice sheet are presented using the high-resolution (2.8 km) non-hydrostatic Lokal-Modell (LM) of the Deutscher Wetterdienst (DWD). The LM is nested into numerical forecasts provided by the hydrostat...

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Bibliographic Details
Published in:Meteorologische Zeitschrift
Main Authors: Thomas Klein, Günther Heinemann, Patrick Gross
Format: Article in Journal/Newspaper
Language:English
Published: Borntraeger 2001
Subjects:
Online Access:https://doi.org/10.1127/0941-2948/2001/0010-0331
https://doaj.org/article/1ef4be91233a47f08594e571f755b899