Details
| Original language | English |
|---|---|
| Pages (from-to) | 379-394 |
| Number of pages | 16 |
| Journal | Boundary-Layer Meteorology |
| Volume | 77 |
| Issue number | 3-4 |
| Publication status | Published - Feb 1996 |
Abstract
A three-dimensional nonhydrostatic model is used to calculate the complex wind field in a coastal and a hilly region. These results are used to test the applicability of a mass-consistent wind model for different numbers of input wind data. While for the coastal area the mass consistent model calculates reasonable results even for a small number of input wind data, this number increases significantly in complex terrain.
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Atmospheric Science
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In: Boundary-Layer Meteorology, Vol. 77, No. 3-4, 02.1996, p. 379-394.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - On the applicability of numerical mass-consistent wind field models
AU - Gross, G.
PY - 1996/2
Y1 - 1996/2
N2 - A three-dimensional nonhydrostatic model is used to calculate the complex wind field in a coastal and a hilly region. These results are used to test the applicability of a mass-consistent wind model for different numbers of input wind data. While for the coastal area the mass consistent model calculates reasonable results even for a small number of input wind data, this number increases significantly in complex terrain.
AB - A three-dimensional nonhydrostatic model is used to calculate the complex wind field in a coastal and a hilly region. These results are used to test the applicability of a mass-consistent wind model for different numbers of input wind data. While for the coastal area the mass consistent model calculates reasonable results even for a small number of input wind data, this number increases significantly in complex terrain.
UR - http://www.scopus.com/inward/record.url?scp=0030473017&partnerID=8YFLogxK
U2 - 10.1007/BF00123533
DO - 10.1007/BF00123533
M3 - Article
AN - SCOPUS:0030473017
VL - 77
SP - 379
EP - 394
JO - Boundary-Layer Meteorology
JF - Boundary-Layer Meteorology
SN - 0006-8314
IS - 3-4
ER -