Investigation of the Mixing Height in the Planetary Boundary Layer by Using Sodar and Microwave Radiometer Data

The height of the mixing layer is a significant parameter for describing the dynamics of the planetary boundary layer (PBL), especially for air quality control and for the parametrizations in numerical modeling. The problem is that the heights of the mixing layer cannot be measured directly. The val...

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Autores principales: Sergey Odintsov, Eugene Miller, Andrey Kamardin, Irina Nevzorova, Arkady Troitsky, Mathias Schröder
Formato: article
Lenguaje:EN
Publicado: MDPI AG 2021
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MWR
Acceso en línea:https://doaj.org/article/fd46bb34389743ff9a4c8639760bff93
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spelling oai:doaj.org-article:fd46bb34389743ff9a4c8639760bff932021-11-25T17:31:01ZInvestigation of the Mixing Height in the Planetary Boundary Layer by Using Sodar and Microwave Radiometer Data10.3390/environments81101152076-3298https://doaj.org/article/fd46bb34389743ff9a4c8639760bff932021-10-01T00:00:00Zhttps://www.mdpi.com/2076-3298/8/11/115https://doaj.org/toc/2076-3298The height of the mixing layer is a significant parameter for describing the dynamics of the planetary boundary layer (PBL), especially for air quality control and for the parametrizations in numerical modeling. The problem is that the heights of the mixing layer cannot be measured directly. The values of this parameter are depending both on the applied algorithms for calculation and on the measuring instruments which have been used by the data source. To determine the height of a layer of intense turbulent heat exchange, data were used from acoustic meteorological locator (sodar) and from a passive single-channel scanning microwave radiometer MTP-5 (MWR) to measure the temperature profile in a layer of up to 1 km. Sodar can provide information on the structure of temperature turbulence in the PBL directly. These data have been compared with the mixing layer height calculated with the Parcel method by using the MTP-5 data. For the analysis, July and September 2020 were selected in the city of Tomsk in Siberia as characteristic periods of mid-summer and the transition period to autumn. The measurement results, calculations and inter-comparisons are shown and discussed in this work. During temperature inversions in the boundary layer, it was observed that turbulent heat transfer (increased dispersion of air temperature) is covering the inversion layers and the overlying ones. Moreover, this phenomenon is not only occurring during the morning destruction of inversions, but also in the process of their formation and development.Sergey OdintsovEugene MillerAndrey KamardinIrina NevzorovaArkady TroitskyMathias SchröderMDPI AGarticleplanetary boundary layersodarMWRmixing heighttemperature inversionEnvironmental technology. Sanitary engineeringTD1-1066ENEnvironments, Vol 8, Iss 115, p 115 (2021)
institution DOAJ
collection DOAJ
language EN
topic planetary boundary layer
sodar
MWR
mixing height
temperature inversion
Environmental technology. Sanitary engineering
TD1-1066
spellingShingle planetary boundary layer
sodar
MWR
mixing height
temperature inversion
Environmental technology. Sanitary engineering
TD1-1066
Sergey Odintsov
Eugene Miller
Andrey Kamardin
Irina Nevzorova
Arkady Troitsky
Mathias Schröder
Investigation of the Mixing Height in the Planetary Boundary Layer by Using Sodar and Microwave Radiometer Data
description The height of the mixing layer is a significant parameter for describing the dynamics of the planetary boundary layer (PBL), especially for air quality control and for the parametrizations in numerical modeling. The problem is that the heights of the mixing layer cannot be measured directly. The values of this parameter are depending both on the applied algorithms for calculation and on the measuring instruments which have been used by the data source. To determine the height of a layer of intense turbulent heat exchange, data were used from acoustic meteorological locator (sodar) and from a passive single-channel scanning microwave radiometer MTP-5 (MWR) to measure the temperature profile in a layer of up to 1 km. Sodar can provide information on the structure of temperature turbulence in the PBL directly. These data have been compared with the mixing layer height calculated with the Parcel method by using the MTP-5 data. For the analysis, July and September 2020 were selected in the city of Tomsk in Siberia as characteristic periods of mid-summer and the transition period to autumn. The measurement results, calculations and inter-comparisons are shown and discussed in this work. During temperature inversions in the boundary layer, it was observed that turbulent heat transfer (increased dispersion of air temperature) is covering the inversion layers and the overlying ones. Moreover, this phenomenon is not only occurring during the morning destruction of inversions, but also in the process of their formation and development.
format article
author Sergey Odintsov
Eugene Miller
Andrey Kamardin
Irina Nevzorova
Arkady Troitsky
Mathias Schröder
author_facet Sergey Odintsov
Eugene Miller
Andrey Kamardin
Irina Nevzorova
Arkady Troitsky
Mathias Schröder
author_sort Sergey Odintsov
title Investigation of the Mixing Height in the Planetary Boundary Layer by Using Sodar and Microwave Radiometer Data
title_short Investigation of the Mixing Height in the Planetary Boundary Layer by Using Sodar and Microwave Radiometer Data
title_full Investigation of the Mixing Height in the Planetary Boundary Layer by Using Sodar and Microwave Radiometer Data
title_fullStr Investigation of the Mixing Height in the Planetary Boundary Layer by Using Sodar and Microwave Radiometer Data
title_full_unstemmed Investigation of the Mixing Height in the Planetary Boundary Layer by Using Sodar and Microwave Radiometer Data
title_sort investigation of the mixing height in the planetary boundary layer by using sodar and microwave radiometer data
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/fd46bb34389743ff9a4c8639760bff93
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