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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2008-12-01
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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 |
work_keys_str_mv |
AT jihyunha comparisonoflocalmeantemperatureequationsforgpsbasedprecipitablewatervapordetermination AT kwandongpark comparisonoflocalmeantemperatureequationsforgpsbasedprecipitablewatervapordetermination |
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1725949342406148096 |