Many general circulation models (GCMs) predict that high latitude environments will experience substantial warming over the next 100 years, which will be particularly pronounced during the winter months. Precipitation is also expected to increase but there is uncertainty as to the amount and spatial
Calculations on the wind climate in northern Finland: the importance of inversions and roughness variations during the seasons
✍ Scribed by Helmut P. Frank; Erik L. Petersen; Reijo Hyvönen; Bengt Tammelin
- Publisher
- John Wiley and Sons
- Year
- 1999
- Tongue
- English
- Weight
- 517 KB
- Volume
- 2
- Category
- Article
- ISSN
- 1095-4244
No coin nor oath required. For personal study only.
✦ Synopsis
The wind power potential around Pyha Ètunturi Fell in northern Finland is calculated with WAsP and the Karlsruhe Atmospheric Mesoscale Model (KAMM) using a climatology of the geostrophic wind from the global reanalysis of NCEP/NCAR. The importance of roughness variations between summer and winter due to snow cover and of strong, lowlevel inversions during winter is investigated. At the position of a telemast on the fell the changing roughness led to an increase in the predicted wind power density of only 1% at 61 m. However, frequent inversions in winter have a major in¯uence on the wind potential on the fell areas. Accounting for them increased the predicted wind power density by 10%±16%, giving better agreement with the observations. As expected, the wind in the plains is reduced during conditions with inversions. The simulations with KAMM were performed for a grid map with a resolution of 350 m. This is too rough to resolve the steep slopes of Pyha Ètunturi Fell. Therefore the predicted wind speed on the summit is underestimated by up to 15% depending on the wind direction.
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