Radiosonde temperature measurements in strong inversions: Correction for thermal lag based on an experiment at the South Pole

Very steep shallow temperature inversions occur during most of the year in the near-surface layer on the Antarctic Plateau. A radiosonde carried by a balloon rising at a few meters per second does not measure such inversions accurately because the response time of the thermistor is several seconds....

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Main Authors: Ashwin Mahesh, Von P. Walden, Stephen, G. Warren
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1997
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.5744
http://www.atmos.washington.edu/~sgw/PAPERS/1997_JAOT.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.546.5744 2023-05-15T13:38:07+02:00 Radiosonde temperature measurements in strong inversions: Correction for thermal lag based on an experiment at the South Pole Ashwin Mahesh Von P. Walden Stephen G. Warren The Pennsylvania State University CiteSeerX Archives 1997 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.5744 http://www.atmos.washington.edu/~sgw/PAPERS/1997_JAOT.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.5744 http://www.atmos.washington.edu/~sgw/PAPERS/1997_JAOT.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.atmos.washington.edu/~sgw/PAPERS/1997_JAOT.pdf text 1997 ftciteseerx 2021-11-21T01:23:33Z Very steep shallow temperature inversions occur during most of the year in the near-surface layer on the Antarctic Plateau. A radiosonde carried by a balloon rising at a few meters per second does not measure such inversions accurately because the response time of the thermistor is several seconds. To quantify this error, the authors flew a radiosonde on a tethered kite on several occasions in winter at South Pole Station immediately prior to the routine launch of the same sonde on a weather balloon. In all cases, the equilibrated temperatures measured by the tethered sonde at a given pressure level were higher than those from the balloon-borne sonde throughout most of the inversion layer. Assuming that the tethered sonde data represent the true atmospheric temperature profile, a procedure can be developed to correct the temperature data from routine radiosonde soundings for the finite response time of the thermistor. The authors devise an accurate deconvolution method to retrieve the true atmospheric temperature profile from the radiosonde data when the thermistor response time is known. However, a simple technique of shifting the profile a few seconds back in time gives results that are nearly equivalent to the deconvolution. Additional temperature errors result at the South Pole because the radiosonde is launched immediately after being brought out of a warm room, making it necessary to further adjust data from the lowest few tens of meters. It is found that the temperature errors cause a 0.3 W m22 error Text Antarc* Antarctic South pole South pole Unknown Antarctic South Pole The Antarctic
institution Open Polar
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language English
description Very steep shallow temperature inversions occur during most of the year in the near-surface layer on the Antarctic Plateau. A radiosonde carried by a balloon rising at a few meters per second does not measure such inversions accurately because the response time of the thermistor is several seconds. To quantify this error, the authors flew a radiosonde on a tethered kite on several occasions in winter at South Pole Station immediately prior to the routine launch of the same sonde on a weather balloon. In all cases, the equilibrated temperatures measured by the tethered sonde at a given pressure level were higher than those from the balloon-borne sonde throughout most of the inversion layer. Assuming that the tethered sonde data represent the true atmospheric temperature profile, a procedure can be developed to correct the temperature data from routine radiosonde soundings for the finite response time of the thermistor. The authors devise an accurate deconvolution method to retrieve the true atmospheric temperature profile from the radiosonde data when the thermistor response time is known. However, a simple technique of shifting the profile a few seconds back in time gives results that are nearly equivalent to the deconvolution. Additional temperature errors result at the South Pole because the radiosonde is launched immediately after being brought out of a warm room, making it necessary to further adjust data from the lowest few tens of meters. It is found that the temperature errors cause a 0.3 W m22 error
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author Ashwin Mahesh
Von P. Walden
Stephen
G. Warren
spellingShingle Ashwin Mahesh
Von P. Walden
Stephen
G. Warren
Radiosonde temperature measurements in strong inversions: Correction for thermal lag based on an experiment at the South Pole
author_facet Ashwin Mahesh
Von P. Walden
Stephen
G. Warren
author_sort Ashwin Mahesh
title Radiosonde temperature measurements in strong inversions: Correction for thermal lag based on an experiment at the South Pole
title_short Radiosonde temperature measurements in strong inversions: Correction for thermal lag based on an experiment at the South Pole
title_full Radiosonde temperature measurements in strong inversions: Correction for thermal lag based on an experiment at the South Pole
title_fullStr Radiosonde temperature measurements in strong inversions: Correction for thermal lag based on an experiment at the South Pole
title_full_unstemmed Radiosonde temperature measurements in strong inversions: Correction for thermal lag based on an experiment at the South Pole
title_sort radiosonde temperature measurements in strong inversions: correction for thermal lag based on an experiment at the south pole
publishDate 1997
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.546.5744
http://www.atmos.washington.edu/~sgw/PAPERS/1997_JAOT.pdf
geographic Antarctic
South Pole
The Antarctic
geographic_facet Antarctic
South Pole
The Antarctic
genre Antarc*
Antarctic
South pole
South pole
genre_facet Antarc*
Antarctic
South pole
South pole
op_source http://www.atmos.washington.edu/~sgw/PAPERS/1997_JAOT.pdf
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