Abstract
The wake zone behind the escarpment of the Bolund peninsula in the Roskilde
Fjord, Denmark, has been investigated with the help of a continuous-wave Doppler lidar. The
instrument measures the line-of-sight wind speed 390 times per second in highly resolved 7-
m tall profiles by rapidly changing the focus distance and beam direction. The profiles reveal
the detailed and rapidly changing structure of the wake induced by the Bolund escarpment.
The wake grows with distance from the escarpment, with the wake height depending strongly
on the wind direction, such that the minimum height appears when the flow is perpendicular
to the escarpment. The wake increases by 10–70 % when the wind direction deviates ±15◦
from perpendicular depending on the distance to the edge and to a lesser degree on the method
by which the wake height is determined. This finding is supported by a comparison with in
situ measurements acquired on the Bolund peninsula.
Original language | English |
---|---|
Journal | Boundary-Layer Meteorology |
Volume | 159 |
Pages (from-to) | 147–159 |
ISSN | 0006-8314 |
DOIs | |
Publication status | Published - 2016 |
Bibliographical note
© The Author(s) 2015. This article is published with open access at Springerlink.comKeywords
- Bolund
- Complex flow
- Wake height
- WindScanner