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
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...
| Autores: | , , , , |
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| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2020 |
| País: | Argentina |
| Institución: | Consejo Nacional de Investigaciones Científicas y Técnicas |
| Repositorio: | CONICET Digital (CONICET) |
| Idioma: | inglés |
| OAI Identifier: | oai:ri.conicet.gov.ar:11336/156753 |
| Acceso en línea: | http://hdl.handle.net/11336/156753 |
| Access Level: | acceso abierto |
| Palabra clave: | INTEGRATED WATER VAPOR GNSS STATIONS RADIOSONDE VALIDATION PRECIPITATION ARGENTINA https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| Sumario: | 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 significantagreement (coefficient of determination > 0.9) is observed between IWVGNSS and IWV estimates from radiosondemeasurements, highlighting the capability of the GNSS stations to provide IWVGNSS estimates for a densernetwork. The variability of the IWV estimates, the atmospheric pressure and precipitation totals for a case studyare 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 aboutthe 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 betweenpositive IWV anomalies, both on-site and for their surroundings, should be considered. |
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