利用全球导航卫星系统数据确定可降水量特征:越南 Nghia Do 地区案例研究

IF 2.4 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Khuong Pham Le, Anh Nguyen Xuan, Hiep Van Nguyen, Son Hoang Hai, Vinh Nguyen Nhu, Minh Bui Ngoc
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引用次数: 0

摘要

本文利用全球定位系统(GPS)数据和加拿大空间参照系统-精确点定位(CSRS-PPP)处理技术和计算工具,对河内 Nghia Do 地区的可降水总量(TPW)估算值进行了评估,并研究了其特征。利用加拿大自然资源部提供的 CSRS-PPP,根据 2022 年 9 月 22 日至 2023 年 3 月 31 日的 GPS 数据估算出了热压带。计算出的 TPW 与来自 Aeronet 数据和无线电探空仪数据的 TPW 产品进行了验证。利用全球定位系统数据的高时间分辨率优势,对影响 Nghia Do 地区的寒潮期间的 TPW 时间变化进行了分析。结果表明,全球定位系统数据估算的 TPW 与 Aeronet 和无线电探空仪数据得出的 TPW 结果非常吻合。全球定位系统数据估算的热压带平均误差(ME)、均方根误差(RMSE)和相关系数分别为 0.68 毫米、2.05 毫米和 0.988。根据全球定位系统数据估算的 TPW 与无线电探空仪得出的结果之间的相应值分别为-3.01 毫米、3.24 毫米和 0.996。对研究期间义渡地区的 TPW 变化的研究表明,一般来说,12 月和 1 月的 TPW 值低于其他月份。在特定的寒潮到达某个站点之前,随着冷锋前方对流活动的加强,12 小时内的 TPW 往往会增加约 6 毫米。冷空气经过该站后,由于盛行风带来的冬季干冷空气的涌入,12 小时内的脉动温值下降了约 8 毫米。这种明显的TPW变化模式表明,可以有效地利用GPS数据来确定寒潮在该站区域的到达时间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Precipitable water characterization using global navigation satellite system data: A case study in Nghia Do area, Vietnam
This paper evaluates the estimated total precipitable water (TPW) and studies its characteristics in the Nghia Do area (Hanoi) using Global Positioning System (GPS) data and the Canadian Spatial Reference System-Precise Point Positioning (CSRS-PPP) processing technique and calculation tool. The TPW was estimated from GPS data from September 22, 2022 to March 31, 2023 using CSRS-PPP provided by Natural Resources Canada. The calculated TPW was validated with TPW products from Aeronet data and radiosonde data. Taking advantage of its high time resolution, the TPW estimated from GPS data was used to analyze the temporal variation of TPW during cold surges affecting the Nghia Do area. The results indicate a strong agreement between the estimated TPW from GPS data and TPW products derived from Aeronet and radiosonde data. The mean error (ME), root mean square error (RMSE), and correlation coefficient between the estimated TPW from GPS data and the Aeronet-derived product are 0.68 mm, 2.05 mm, and 0.988, respectively. The corresponding values between the estimated TPW and the radiosonde-derived product are -3.01 mm, 3.24 mm, and 0.996, respectively. The study of TPW variation over the Nghia Do area during the research period revealed that, generally, TPW values in December and January were lower than those in the other months. Before the arrival of a specific cold surge at a station, TPW tends to increase by about 6 mm within 12 hours as convection activities ahead of the cold front intensify. After the cold air passes over the station, the TPW value decreases by about 8 mm within 12 hours due to the influx of cold and dry winter air brought by the prevailing winds. This distinct TPW variation pattern suggests that GPS data can be effectively employed to define the arrival of cold surges in the station area.
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来源期刊
VIETNAM JOURNAL OF EARTH SCIENCES
VIETNAM JOURNAL OF EARTH SCIENCES GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
3.60
自引率
20.00%
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