Comparison of Local Mean Temperature Equations for GPS-based Precipitable Water Vapor Determination

The mean temperature equation is a key factor in calculating GPS meteorological information. A local mean temperature equation should be used to improve accuracy of GPS PWV (Precipitable Water Vapor). In this paper, four local mean temperature equations, HP, HP_M, HPt_Y, and HPt_M from Ha & Park...

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Main Authors: Jihyun Ha, Kwan-Dong Park
Format: Article
Language:English
Published: Korean Space Science Society (KSSS) 2008-12-01
Series:Journal of Astronomy and Space Sciences
Subjects:
GPS
Online Access:http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/2008/v25n4/OJOOBS_2008_v25n4_425.pdf
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spelling doaj-a45da12de1fa4c0ba25ae6e7db8f11e52020-11-24T21:34:28ZengKorean Space Science Society (KSSS)Journal of Astronomy and Space Sciences2093-55872093-14092008-12-0125442543410.5140/JASS.2008.25.4.425Comparison of Local Mean Temperature Equations for GPS-based Precipitable Water Vapor DeterminationJihyun Ha0Kwan-Dong Park1Department of Geoinformatic Engineering, Inha University, Incheon 402-751, KoreaDepartment of Geoinformatic Engineering, Inha University, Incheon 402-751, KoreaThe mean temperature equation is a key factor in calculating GPS meteorological information. A local mean temperature equation should be used to improve accuracy of GPS PWV (Precipitable Water Vapor). In this paper, four local mean temperature equations, HP, HP_M, HPt_Y, and HPt_M from Ha & Park (2008) were used to analyze the effects of local models in determining GPS PWV. Four different sets of GPS PWVs were compared with radiosonde PWV to validate the accuracies of local models. GPS PWVs of four local models have similar trends compared against radiosonde PWV. The bias and RMS error were the same level: the bias is ˜ 3 mm and the RMS is ˜ 3.6 mm after the bias was removed. Especially, with HPt_Y and HPt_M models one can obtain accurate PWVs even without surface temperature measurements. And we investigated dry bias of radiosonde measurements depending on sensor types and observation time at Sokcho weather station. After the radiosonde sensor equipment was changed from RS80-15L to GRS DFM-06, dry bias of radiosonde PWV decreased about 18.2 % during daytime (KST 09:00), and 16.1 during nighttime (KST 21:00).http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/2008/v25n4/OJOOBS_2008_v25n4_425.pdfGPSlocal mean temperature equationprecipitable water vaporradiosondedry bias
collection DOAJ
language English
format Article
sources DOAJ
author Jihyun Ha
Kwan-Dong Park
spellingShingle Jihyun Ha
Kwan-Dong Park
Comparison of Local Mean Temperature Equations for GPS-based Precipitable Water Vapor Determination
Journal of Astronomy and Space Sciences
GPS
local mean temperature equation
precipitable water vapor
radiosonde
dry bias
author_facet Jihyun Ha
Kwan-Dong Park
author_sort Jihyun Ha
title Comparison of Local Mean Temperature Equations for GPS-based Precipitable Water Vapor Determination
title_short Comparison of Local Mean Temperature Equations for GPS-based Precipitable Water Vapor Determination
title_full Comparison of Local Mean Temperature Equations for GPS-based Precipitable Water Vapor Determination
title_fullStr Comparison of Local Mean Temperature Equations for GPS-based Precipitable Water Vapor Determination
title_full_unstemmed Comparison of Local Mean Temperature Equations for GPS-based Precipitable Water Vapor Determination
title_sort comparison of local mean temperature equations for gps-based precipitable water vapor determination
publisher Korean Space Science Society (KSSS)
series Journal of Astronomy and Space Sciences
issn 2093-5587
2093-1409
publishDate 2008-12-01
description The mean temperature equation is a key factor in calculating GPS meteorological information. A local mean temperature equation should be used to improve accuracy of GPS PWV (Precipitable Water Vapor). In this paper, four local mean temperature equations, HP, HP_M, HPt_Y, and HPt_M from Ha & Park (2008) were used to analyze the effects of local models in determining GPS PWV. Four different sets of GPS PWVs were compared with radiosonde PWV to validate the accuracies of local models. GPS PWVs of four local models have similar trends compared against radiosonde PWV. The bias and RMS error were the same level: the bias is ˜ 3 mm and the RMS is ˜ 3.6 mm after the bias was removed. Especially, with HPt_Y and HPt_M models one can obtain accurate PWVs even without surface temperature measurements. And we investigated dry bias of radiosonde measurements depending on sensor types and observation time at Sokcho weather station. After the radiosonde sensor equipment was changed from RS80-15L to GRS DFM-06, dry bias of radiosonde PWV decreased about 18.2 % during daytime (KST 09:00), and 16.1 during nighttime (KST 21:00).
topic GPS
local mean temperature equation
precipitable water vapor
radiosonde
dry bias
url http://ocean.kisti.re.kr/downfile/volume/kosss/OJOOBS/2008/v25n4/OJOOBS_2008_v25n4_425.pdf
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