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dc.contributor.authorNascimento, A.A.
dc.contributor.authorAwange, Joseph
dc.contributor.authorGonçalves, R.M.
dc.contributor.authorKhandu
dc.date.accessioned2021-11-25T02:37:47Z
dc.date.available2021-11-25T02:37:47Z
dc.date.issued2020
dc.identifier.citationNascimento, A.A. and Awange, J.L. and Gonçalves, R.M. and Khandu. 2020. South America's tropopause variability in relation to global teleconnection (2001–2017): A GNSS-radio occultation assessment. Journal of Atmospheric and Solar-Terrestrial Physics. 209: ARTN 105379.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/86608
dc.identifier.doi10.1016/j.jastp.2020.105379
dc.description.abstract

Analysing tropopause variability is widely acknowledged to inform the understanding of global/regional warming. Tropopause variability studies are generally undertaken where radiosonde data abound. For the radiosonde data deficient South American continent, taking advantage of atmospheric remote sensing using Global Navigation Satellite Systems - Radio Occultation (GNSS-RO) could offer the means to understand its tropopause variability. In this study, 622,914 GNSS-RO measurements of Challenging Minisatellite Payload (CHAMP), Gravity Recovery and Climate Experiment (GRACE) and Constellation Observing System for Meteorology Ionosphere & Climate (FORMOSAT-3/COSMIC), from 2001 to 2017 are used to analyze the annual variability patterns of tropopause heights and temperatures over South America and its relation to global teleconnections. Firstly, the RO measurements are validated using atmospheric profiles for 54 radiosonde stations across the continent. The results show increased trend of 13.450 ± 39.577 m/dec for the tropopause height and a corresponding slow decrease in temperature of −0.021 ± 0.115 K/dec, both statistically insignificant (i.e., p-value test) at 95% of confidence level (two-tailed student's t-test). The first mode of PCA (Principal Component Analysis) of the tropopause anomalies (of temperatures and heights) present significant temporal correlation (at 95% confidence level) with the ENSO 1 + 2 (El Niño–Southern Oscillation) index (i.e., a correlation coefficient of 0.6). The South America tropopause, therefore, varies over time albeit with slow changes and trends. This contribution highlights the importance of its monitoring.

dc.languageEnglish
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD
dc.subjectScience & Technology
dc.subjectPhysical Sciences
dc.subjectGeochemistry & Geophysics
dc.subjectMeteorology & Atmospheric Sciences
dc.subjectGNSS radio occultation
dc.subjectTropopause
dc.subjectTeleconnections
dc.subjectClimate variability
dc.subjectSouth America
dc.subjectCLIMATE-CHANGE
dc.subjectTEMPERATURE TRENDS
dc.subjectEL-NINO
dc.subjectATMOSPHERIC-TEMPERATURE
dc.subjectUPPER TROPOSPHERE
dc.subjectLA-NINA
dc.subjectSTRATOSPHERE
dc.subjectHEIGHT
dc.subjectIMPACTS
dc.subjectCHAMP
dc.titleSouth America's tropopause variability in relation to global teleconnection (2001–2017): A GNSS-radio occultation assessment
dc.typeJournal Article
dcterms.source.volume209
dcterms.source.issn1364-6826
dcterms.source.titleJournal of Atmospheric and Solar-Terrestrial Physics
dc.date.updated2021-11-25T02:37:46Z
curtin.departmentSchool of Earth and Planetary Sciences (EPS)
curtin.accessStatusIn process
curtin.facultyFaculty of Science and Engineering
curtin.contributor.orcidAwange, Joseph [0000-0003-3533-613X]
curtin.contributor.researcheridAwange, Joseph [A-3998-2008]
curtin.identifier.article-numberARTN 105379
dcterms.source.eissn1879-1824
curtin.contributor.scopusauthoridAwange, Joseph [6603092635]


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