Observing crosswind over urban terrain using scintillometer and Doppler lidar
In this study, the crosswind (wind component perpendicular to a path, <i>U</i><sub>⊥</sub>) is measured by a scintillometer and estimated with Doppler lidar above the urban environment of Helsinki, Finland, for 15 days. The scintillometer allows acquisition of a path-...
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doaj-666fff386a004094b05574f7c729bea92020-11-24T22:17:58ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482015-04-01841901191110.5194/amt-8-1901-2015Observing crosswind over urban terrain using scintillometer and Doppler lidarD. van Dinther0C. R. Wood1O. K. Hartogensis2A. Nordbo3E. J. O'Connor4Meteorology and Air Quality Group, Wageningen University, Wageningen, the NetherlandsFinnish Meteorological Institute, Helsinki, FinlandMeteorology and Air Quality Group, Wageningen University, Wageningen, the NetherlandsDepartment of Physics, University of Helsinki, Helsinki, FinlandFinnish Meteorological Institute, Helsinki, FinlandIn this study, the crosswind (wind component perpendicular to a path, <i>U</i><sub>⊥</sub>) is measured by a scintillometer and estimated with Doppler lidar above the urban environment of Helsinki, Finland, for 15 days. The scintillometer allows acquisition of a path-averaged value of <i>U</i><sub>⊥</sub> (<span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span>), while the lidar allows acquisition of path-resolved <i>U</i><sub>⊥</sub> (<i>U</i><sub>⊥</sub> (<i>x</i>), where <i>x</i> is the position along the path). The goal of this study is to evaluate the performance of scintillometer <span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> estimates for conditions under which <i>U</i><sub>⊥</sub> (<i>x</i>) is variable. Two methods are applied to estimate <span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> from the scintillometer signal: the cumulative-spectrum method (relies on scintillation spectra) and the look-up-table method (relies on time-lagged correlation functions). The values of <span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> of both methods compare well with the lidar estimates, with root-mean-square deviations of 0.71 and 0.73 m s<sup>−1</sup>. This indicates that, given the data treatment applied in this study, both measurement technologies are able to obtain estimates of <span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> in the complex urban environment. The detailed investigation of four cases indicates that the cumulative-spectrum method is less susceptible to a variable <i>U</i><sub>⊥</sub> (<i>x</i>) than the look-up-table method. However, the look-up-table method can be adjusted to improve its capabilities for estimating <span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> under conditions under for which <i>U</i><sub>⊥</sub> (<i>x</i>) is variable.http://www.atmos-meas-tech.net/8/1901/2015/amt-8-1901-2015.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
D. van Dinther C. R. Wood O. K. Hartogensis A. Nordbo E. J. O'Connor |
spellingShingle |
D. van Dinther C. R. Wood O. K. Hartogensis A. Nordbo E. J. O'Connor Observing crosswind over urban terrain using scintillometer and Doppler lidar Atmospheric Measurement Techniques |
author_facet |
D. van Dinther C. R. Wood O. K. Hartogensis A. Nordbo E. J. O'Connor |
author_sort |
D. van Dinther |
title |
Observing crosswind over urban terrain using scintillometer and Doppler lidar |
title_short |
Observing crosswind over urban terrain using scintillometer and Doppler lidar |
title_full |
Observing crosswind over urban terrain using scintillometer and Doppler lidar |
title_fullStr |
Observing crosswind over urban terrain using scintillometer and Doppler lidar |
title_full_unstemmed |
Observing crosswind over urban terrain using scintillometer and Doppler lidar |
title_sort |
observing crosswind over urban terrain using scintillometer and doppler lidar |
publisher |
Copernicus Publications |
series |
Atmospheric Measurement Techniques |
issn |
1867-1381 1867-8548 |
publishDate |
2015-04-01 |
description |
In this study, the crosswind (wind component perpendicular to a path,
<i>U</i><sub>⊥</sub>) is measured by a scintillometer and estimated with Doppler
lidar above the urban environment of Helsinki, Finland, for 15 days. The
scintillometer allows acquisition of a path-averaged value of <i>U</i><sub>⊥</sub> (<span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span>), while the lidar allows acquisition of path-resolved
<i>U</i><sub>⊥</sub> (<i>U</i><sub>⊥</sub> (<i>x</i>), where <i>x</i> is the position along the path). The
goal of this study is to evaluate the performance of scintillometer
<span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> estimates for conditions under which <i>U</i><sub>⊥</sub> (<i>x</i>) is
variable. Two methods are applied to estimate <span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> from the
scintillometer signal: the cumulative-spectrum method (relies on
scintillation spectra) and the look-up-table method (relies on time-lagged
correlation functions). The values of <span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> of both methods
compare well with the lidar estimates, with root-mean-square deviations of
0.71 and 0.73 m s<sup>−1</sup>. This indicates that, given the data treatment
applied in this study, both measurement technologies are able to obtain
estimates of <span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> in the complex urban environment. The
detailed investigation of four cases indicates that the cumulative-spectrum
method is less susceptible to a variable <i>U</i><sub>⊥</sub> (<i>x</i>) than the look-up-table
method. However, the look-up-table method can be adjusted to improve its
capabilities for estimating <span style="border-top: 1px solid #000; color: #000;"><i>U</i><sub>⊥</sub></span> under conditions under for
which <i>U</i><sub>⊥</sub> (<i>x</i>) is variable. |
url |
http://www.atmos-meas-tech.net/8/1901/2015/amt-8-1901-2015.pdf |
work_keys_str_mv |
AT dvandinther observingcrosswindoverurbanterrainusingscintillometeranddopplerlidar AT crwood observingcrosswindoverurbanterrainusingscintillometeranddopplerlidar AT okhartogensis observingcrosswindoverurbanterrainusingscintillometeranddopplerlidar AT anordbo observingcrosswindoverurbanterrainusingscintillometeranddopplerlidar AT ejoconnor observingcrosswindoverurbanterrainusingscintillometeranddopplerlidar |
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1725783630841643008 |