The effect of different k- closures on the results of a micro-scale model for the flow in the obstacle layer
A non-hydrostatic micro-scale model (MITRAS) is used to simulate the flow field over a beam. The model is run with a constant grid size of 1/5 times the beam height representing a relatively coarse resolution. Different types of k-ε closures are used, the standard-k-ε-closure and modified ones. A co...
Main Authors: | Simon Domingo López, Christof Lüpkes, Katharina Heinke Schlünzen |
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Format: | Article |
Language: | English |
Published: |
Borntraeger
2005-12-01
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Series: | Meteorologische Zeitschrift |
Online Access: | http://dx.doi.org/10.1127/0941-2948/2005/0084 |
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