On the dynamic variability of global positioning system (GPS) derived precipitable water vapour (PWV) over three geographical regions of Nepal

IF 1.8 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Nisarga Sharma, Arnav Subedi, Basudev Ghimire, Shreeram Nagarkoti, Balaram Khadka
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引用次数: 0

Abstract

We study the variation of zenith total delay (ZTD) and precipitable water vapour (PWV) using global positioning system (GPS) data and observed meteorological information over three different topographical zones of Nepal: Terai, Hilly and Himalayan region. Eight GPS stations scattered across these regions were utilized for data collection. Two alternate years, 2015 and 2017 were taken as the study period and the data obtained were analysed to compare trends. Findings indicate that the average PWV levels are higher in the Terai region in comparison to the Hilly and Himalayan region, explaining the precipitation patterns over Nepal. Additionally, the daily PWV patterns show peak levels during mid-day and a decline during the night. The findings highlight the significant variability of PWV across different regions of Nepal and its implications for evaluating PWV variability across regions.

尼泊尔三个地理区域全球定位系统(GPS)衍生可降水量(PWV)的动态变率
本文利用全球定位系统(GPS)数据和观测气象资料,研究了尼泊尔三个不同地形区(特赖、丘陵和喜马拉雅地区)的天顶总延迟(ZTD)和可降水量(PWV)的变化。分散在这些地区的8个GPS站被用来收集数据。以2015年和2017年为研究周期,对获得的数据进行分析以比较趋势。研究结果表明,与丘陵和喜马拉雅地区相比,德莱地区的平均PWV水平更高,这解释了尼泊尔的降水模式。此外,每日PWV模式显示中午达到峰值水平,夜间下降。研究结果强调了尼泊尔不同地区PWV的显著变异性及其对评估不同地区PWV变异性的影响。
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来源期刊
Acta Geodaetica et Geophysica
Acta Geodaetica et Geophysica GEOCHEMISTRY & GEOPHYSICS-
CiteScore
3.10
自引率
7.10%
发文量
26
期刊介绍: The journal publishes original research papers in the field of geodesy and geophysics under headings: aeronomy and space physics, electromagnetic studies, geodesy and gravimetry, geodynamics, geomathematics, rock physics, seismology, solid earth physics, history. Papers dealing with problems of the Carpathian region and its surroundings are preferred. Similarly, papers on topics traditionally covered by Hungarian geodesists and geophysicists (e.g. robust estimations, geoid, EM properties of the Earth’s crust, geomagnetic pulsations and seismological risk) are especially welcome.
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