Evaluation of convective boundary layer height estimates using radars operating at different frequency bands

<p>Knowledge of the atmospheric boundary layer state and evolution is important for understanding air pollution and low-level cloud development, among other things. There are a number of instruments and methods that are currently used to estimate boundary layer height (BLH). However, no single...

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Autores principales: A. Franck, D. Moisseev, V. Vakkari, M. Leskinen, J. Lampilahti, V.-M. Kerminen, E. O'Connor
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Publicado: Copernicus Publications 2021
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spelling oai:doaj.org-article:dcacaef7b2034882b3e246dcb6cba6e52021-11-24T10:45:34ZEvaluation of convective boundary layer height estimates using radars operating at different frequency bands10.5194/amt-14-7341-20211867-13811867-8548https://doaj.org/article/dcacaef7b2034882b3e246dcb6cba6e52021-11-01T00:00:00Zhttps://amt.copernicus.org/articles/14/7341/2021/amt-14-7341-2021.pdfhttps://doaj.org/toc/1867-1381https://doaj.org/toc/1867-8548<p>Knowledge of the atmospheric boundary layer state and evolution is important for understanding air pollution and low-level cloud development, among other things. There are a number of instruments and methods that are currently used to estimate boundary layer height (BLH). However, no single instrument is capable of providing BLH measurements in all weather conditions. We proposed a method to derive a daytime convective BLH using clear air echoes in radar observations and investigated the consistency of these retrievals between different radar frequencies. We utilized data from three vertically pointing radars that are available at the SMEAR II station in Finland, i.e. the C band (5 GHz), Ka band (35 GHz) and W band (94 GHz). The Ka- or W-band cloud radars are an integral part of cloud profiling stations of pan-European Aerosol, Clouds and Trace Gases Research Infrastructure (ACTRIS). Our method will be utilized at ACTRIS stations to serve as an additional estimate of the BLH during summer months. During this period, insects and Bragg scatter are often responsible for clear air echoes recorded by weather and cloud radars. To retrieve a BLH, we suggested a mechanism to separate passive and independently flying insects that works for all analysed frequency bands. At the lower frequency (the C band) insect scattering has been separated from Bragg scattering using a combination of the radar reflectivity factor and linear depolarization ratio. Retrieved values of the BLH from all radars are in a good agreement when compared to the BLH obtained with the co-located HALO Doppler lidar and ERA5 reanalysis data set. Our method showed some underestimation of the BLH after nighttime heavy precipitation yet demonstrated a potential to serve as a reliable method to obtain a BLH during clear-sky days. Additionally, the entrainment zone was observed by the C-band radar above the CBL in the form of a Bragg scatter layer. Aircraft observations of vertical profiles of potential temperature and water vapour concentration, collected in the vicinity of the radar, demonstrated some agreement with the Bragg scatter layer.</p>A. FranckD. MoisseevD. MoisseevV. VakkariV. VakkariM. LeskinenJ. LampilahtiV.-M. KerminenE. O'ConnorCopernicus PublicationsarticleEnvironmental engineeringTA170-171Earthwork. FoundationsTA715-787ENAtmospheric Measurement Techniques, Vol 14, Pp 7341-7353 (2021)
institution DOAJ
collection DOAJ
language EN
topic Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
spellingShingle Environmental engineering
TA170-171
Earthwork. Foundations
TA715-787
A. Franck
D. Moisseev
D. Moisseev
V. Vakkari
V. Vakkari
M. Leskinen
J. Lampilahti
V.-M. Kerminen
E. O'Connor
Evaluation of convective boundary layer height estimates using radars operating at different frequency bands
description <p>Knowledge of the atmospheric boundary layer state and evolution is important for understanding air pollution and low-level cloud development, among other things. There are a number of instruments and methods that are currently used to estimate boundary layer height (BLH). However, no single instrument is capable of providing BLH measurements in all weather conditions. We proposed a method to derive a daytime convective BLH using clear air echoes in radar observations and investigated the consistency of these retrievals between different radar frequencies. We utilized data from three vertically pointing radars that are available at the SMEAR II station in Finland, i.e. the C band (5 GHz), Ka band (35 GHz) and W band (94 GHz). The Ka- or W-band cloud radars are an integral part of cloud profiling stations of pan-European Aerosol, Clouds and Trace Gases Research Infrastructure (ACTRIS). Our method will be utilized at ACTRIS stations to serve as an additional estimate of the BLH during summer months. During this period, insects and Bragg scatter are often responsible for clear air echoes recorded by weather and cloud radars. To retrieve a BLH, we suggested a mechanism to separate passive and independently flying insects that works for all analysed frequency bands. At the lower frequency (the C band) insect scattering has been separated from Bragg scattering using a combination of the radar reflectivity factor and linear depolarization ratio. Retrieved values of the BLH from all radars are in a good agreement when compared to the BLH obtained with the co-located HALO Doppler lidar and ERA5 reanalysis data set. Our method showed some underestimation of the BLH after nighttime heavy precipitation yet demonstrated a potential to serve as a reliable method to obtain a BLH during clear-sky days. Additionally, the entrainment zone was observed by the C-band radar above the CBL in the form of a Bragg scatter layer. Aircraft observations of vertical profiles of potential temperature and water vapour concentration, collected in the vicinity of the radar, demonstrated some agreement with the Bragg scatter layer.</p>
format article
author A. Franck
D. Moisseev
D. Moisseev
V. Vakkari
V. Vakkari
M. Leskinen
J. Lampilahti
V.-M. Kerminen
E. O'Connor
author_facet A. Franck
D. Moisseev
D. Moisseev
V. Vakkari
V. Vakkari
M. Leskinen
J. Lampilahti
V.-M. Kerminen
E. O'Connor
author_sort A. Franck
title Evaluation of convective boundary layer height estimates using radars operating at different frequency bands
title_short Evaluation of convective boundary layer height estimates using radars operating at different frequency bands
title_full Evaluation of convective boundary layer height estimates using radars operating at different frequency bands
title_fullStr Evaluation of convective boundary layer height estimates using radars operating at different frequency bands
title_full_unstemmed Evaluation of convective boundary layer height estimates using radars operating at different frequency bands
title_sort evaluation of convective boundary layer height estimates using radars operating at different frequency bands
publisher Copernicus Publications
publishDate 2021
url https://doaj.org/article/dcacaef7b2034882b3e246dcb6cba6e5
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