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Hourly PWV Dataset Derived from GNSS Observations in China

The rapid variation of atmospheric water vapor is important for a regional hydrologic cycle and climate change. However, it is rarely investigated in China, due to the lack of a precipitable water vapor (PWV) dataset with high temporal resolution. Therefore, this study focuses on the generation of a...

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Autores principales: Zhao, Qingzhi, Yang, Pengfei, Yao, Wanqiang, Yao, Yibin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: MDPI 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6982703/
https://www.ncbi.nlm.nih.gov/pubmed/31906146
http://dx.doi.org/10.3390/s20010231
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author Zhao, Qingzhi
Yang, Pengfei
Yao, Wanqiang
Yao, Yibin
author_facet Zhao, Qingzhi
Yang, Pengfei
Yao, Wanqiang
Yao, Yibin
author_sort Zhao, Qingzhi
collection PubMed
description The rapid variation of atmospheric water vapor is important for a regional hydrologic cycle and climate change. However, it is rarely investigated in China, due to the lack of a precipitable water vapor (PWV) dataset with high temporal resolution. Therefore, this study focuses on the generation of an hourly PWV dataset using Global Navigation Satellite System (GNSS) observations derived from the Crustal Movement Observation Network of China. The zenith total delay parameters estimated by GAMIT/GLOBK software are used and validated with an average root mean square (RMS) error of 4–5 mm. The pressure (P) and temperature (T) parameters used to calculate the zenith hydrostatic delay (ZHD) and weighted average temperature of atmospheric water vapor (T(m)) are derived from the fifth-generation reanalysis dataset of the European Centre for Medium-Range Weather Forecasting (ECMWF ERA5) products. The values of P and T at the GNSS stations are obtained by interpolation in the horizontal and vertical directions using empirical formulas. T(m) is calculated at the GNSS stations using the improved global pressure and temperature 2 wet (IGPT2w) model in China with an RMS of 3.32 K. The interpolated P and T are validated by interpolating the grid-based ERA5 data into radiosonde stations. The average RMS and bias of P and T in China are 2.71/−1.11 hPa and 1.88/−0.51 K, respectively. Therefore, the error in PWV with a theoretical RMS of 1.85 mm over the period of 2011–2017 in China can be obtained. Finally, the hourly PWV dataset in China is generated and the practical accuracy of the generated PWV dataset is validated using the corresponding AERONET and radiosonde data at specific stations. Numerical results reveal that the average RMS values of the PWV dataset in the four geographical regions of China are less than 3 mm. A case analysis of the PWV diurnal variations as a response to the EI Niño event of 2015–2016 is performed. Results indicate the capability of the hourly PWV dataset of monitoring the rapid water vapor changes in China.
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spelling pubmed-69827032020-02-28 Hourly PWV Dataset Derived from GNSS Observations in China Zhao, Qingzhi Yang, Pengfei Yao, Wanqiang Yao, Yibin Sensors (Basel) Article The rapid variation of atmospheric water vapor is important for a regional hydrologic cycle and climate change. However, it is rarely investigated in China, due to the lack of a precipitable water vapor (PWV) dataset with high temporal resolution. Therefore, this study focuses on the generation of an hourly PWV dataset using Global Navigation Satellite System (GNSS) observations derived from the Crustal Movement Observation Network of China. The zenith total delay parameters estimated by GAMIT/GLOBK software are used and validated with an average root mean square (RMS) error of 4–5 mm. The pressure (P) and temperature (T) parameters used to calculate the zenith hydrostatic delay (ZHD) and weighted average temperature of atmospheric water vapor (T(m)) are derived from the fifth-generation reanalysis dataset of the European Centre for Medium-Range Weather Forecasting (ECMWF ERA5) products. The values of P and T at the GNSS stations are obtained by interpolation in the horizontal and vertical directions using empirical formulas. T(m) is calculated at the GNSS stations using the improved global pressure and temperature 2 wet (IGPT2w) model in China with an RMS of 3.32 K. The interpolated P and T are validated by interpolating the grid-based ERA5 data into radiosonde stations. The average RMS and bias of P and T in China are 2.71/−1.11 hPa and 1.88/−0.51 K, respectively. Therefore, the error in PWV with a theoretical RMS of 1.85 mm over the period of 2011–2017 in China can be obtained. Finally, the hourly PWV dataset in China is generated and the practical accuracy of the generated PWV dataset is validated using the corresponding AERONET and radiosonde data at specific stations. Numerical results reveal that the average RMS values of the PWV dataset in the four geographical regions of China are less than 3 mm. A case analysis of the PWV diurnal variations as a response to the EI Niño event of 2015–2016 is performed. Results indicate the capability of the hourly PWV dataset of monitoring the rapid water vapor changes in China. MDPI 2019-12-31 /pmc/articles/PMC6982703/ /pubmed/31906146 http://dx.doi.org/10.3390/s20010231 Text en © 2019 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).
spellingShingle Article
Zhao, Qingzhi
Yang, Pengfei
Yao, Wanqiang
Yao, Yibin
Hourly PWV Dataset Derived from GNSS Observations in China
title Hourly PWV Dataset Derived from GNSS Observations in China
title_full Hourly PWV Dataset Derived from GNSS Observations in China
title_fullStr Hourly PWV Dataset Derived from GNSS Observations in China
title_full_unstemmed Hourly PWV Dataset Derived from GNSS Observations in China
title_short Hourly PWV Dataset Derived from GNSS Observations in China
title_sort hourly pwv dataset derived from gnss observations in china
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6982703/
https://www.ncbi.nlm.nih.gov/pubmed/31906146
http://dx.doi.org/10.3390/s20010231
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AT yaoyibin hourlypwvdatasetderivedfromgnssobservationsinchina