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...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Borntraeger
2001-10-01
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| Series: | Meteorologische Zeitschrift |
| Online Access: | http://dx.doi.org/10.1127/0941-2948/2001/0010-0331 |