Show simple item record

dc.contributor.authorGraffigna, Victoria
dc.contributor.authorHernández Pajares, Manuel
dc.contributor.authorGende, Mauricio
dc.contributor.authorAzpilicueta, Francisco
dc.contributor.authorAntico, Pablo
dc.contributor.otherUniversitat Politècnica de Catalunya. Departament de Matemàtiques
dc.date.accessioned2020-01-30T13:00:51Z
dc.date.available2020-01-30T13:00:51Z
dc.date.issued2019-01-01
dc.identifier.citationGraffigna, V. [et al.]. Interpretation of the tropospheric gradients estimated with GPS during hurricane Harvey. "Earth and Space Science", 1 Gener 2019, vol. 6, núm. 8, p. 1348-1365.
dc.identifier.issn2333-5084
dc.identifier.urihttp://hdl.handle.net/2117/176202
dc.description.abstractDuring the last decade Global Positioning System (GPS) Continuous Operating Reference Stations networks have become a new important data source for meteorology. This has dramatically improved the ability to remotely sense the atmosphere under the influence of severe mesoscale and synoptic systems. The zenith tropospheric delay (ZTD) is one of the atmospheric variables continuously observed, and its horizontal variations, the horizontal tropospheric gradients, are routinely computed nowadays within the dual-frequency GPS processing, but their interpretation and relationship with the weather is still an open question. The purpose of this paper is to contribute in this direction by studying the effect that Hurricane Harvey had on the spatial and temporal behavior of the ZTDs and gradients, when it reached Texas coast, during 18–31 August 2017. The results show that ZTD time series present a clear and rapid increase larger than 10 cm in a few hours when the hurricane reached the area. Gradients behaviors show that the hurricane also produced significant changes on them, since the magnitude and predominant directions before and after the hurricane arrived are completely different. Noticeably, the gradient vectors before the landing are consistently related to the horizontal winds and pressure fields. In this manuscript we demonstrate that the ZTD gradients can show a consistent signature under severe weather events, strongly suggesting their potential application for short-term weather forecasting.
dc.format.extent18 p.
dc.language.isoeng
dc.subjectÀrees temàtiques de la UPC::Matemàtiques i estadística::Matemàtica aplicada a les ciències
dc.subject.lcshGeophysics
dc.titleInterpretation of the tropospheric gradients estimated with GPS during hurricane Harvey
dc.typeArticle
dc.subject.lemacGeofísica
dc.contributor.groupUniversitat Politècnica de Catalunya. IonSAT - Grup de determinació Ionosfèrica i navegació per SAtèl·lit i sistemes Terrestres
dc.identifier.doi10.1029/2018EA000527
dc.description.peerreviewedPeer Reviewed
dc.subject.amsClassificació AMS::86 Geophysics
dc.relation.publisherversionhttps://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2018EA000527
dc.rights.accessOpen Access
local.identifier.drac25816150
dc.description.versionPostprint (published version)
local.citation.authorGraffigna, V.; Hernandez, M.; Gende, M.; Azpilicueta, F.; Antico, P.
local.citation.publicationNameEarth and Space Science
local.citation.volume6
local.citation.number8
local.citation.startingPage1348
local.citation.endingPage1365


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record