首页> 外文期刊>Journal of atmospheric and solar-terrestrial physics >Estimation of integrated water vapor derived from Global Navigation Satellite System observations over Central-Western Argentina (2015-2018). Validation and usefulness for the understanding of regional precipitation events
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Estimation of integrated water vapor derived from Global Navigation Satellite System observations over Central-Western Argentina (2015-2018). Validation and usefulness for the understanding of regional precipitation events

机译:中西部地区全球导航卫星系统观察综合水蒸气估算(2015-2018)。 理解区域降水事件的验证和实用性

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摘要

This study assesses the possibility of using Global Navigation Satellite System (GNSS) observations in combination with measurements of surface pressure and temperature to derive Integrated Water Vapor (IWVGNSS) estimates in Central-Western Argentina (CWA), a semi-arid region with complex topography. A significant agreement (coefficient of determination > 0.9) is observed between IWVGNSS and IWV estimates from radiosonde measurements, highlighting the capability of the GNSS stations to provide IWVGNSS estimates for a denser network. The variability of the IWV estimates, the atmospheric pressure and precipitation totals for a case study are compared. The results show that the occurrence of the increase in IWV values (positive IWV anomalies) precedes abundant precipitation over the CWA, in conjunction with the presence of mid-troposphere low-pressure anomalies acting as synoptic forcing. This kind of information provides a more comprehensive picture about the atmospheric processes involved in the development of deep convection, and it can be used for the development of contingency plans in the region. Heavy precipitation events and the difference in timing between positive IWV anomalies, both on-site and for their surroundings, should be considered.
机译:本研究评估了使用全球导航卫星系统(GNSS)观察的可能性与表面压力和温度的测量结果,以导出中西部阿根廷(CWA)的综合水蒸气(IWVGNSS)估计,具有复杂地形的半干旱区域。从无线电电视测量的IWVGNSS和IWV估计之间观察到重大协议(确定结果> 0.9),突出显示GNSS站的能力为更密集网络提供IWVGNSS估计。比较了IWV估计的可变性,进行了案例研究的大气压和降水总量。结果表明,IWV值增加(阳性IWV异常)的发生在CWA上的丰富沉淀后,结合对流层中层低压异常的存在,其具有概要强迫。这种信息提供了关于在深度对流发展中涉及的大气流程的更全面的图景,可用于该地区的应急计划的发展。应考虑重度降水事件和阳性IWV异常之间的时间差异,包括在现场和周围环境中。

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