ENSO-related moisture and temperature anomalies over South America derived from GPS radio occultation profiles

El Niño Southern Oscillation- (ENSO) related anomaly patterns of monthly specific humidity (q), precipitable water content (PW) and temperature (T) over South America are analysed using the FORMOSAT-3/COSMIC mission data (August 2006–December 2013). The Global Positioning System radio occultation (G...

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Autores principales: Llamedo, P., Hierro, R., de la Torre, A., Alexander, P.
Formato: JOUR
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GPS
Acceso en línea:http://hdl.handle.net/20.500.12110/paper_08998418_v37_n1_p268_Llamedo
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spelling todo:paper_08998418_v37_n1_p268_Llamedo2023-10-03T15:44:28Z ENSO-related moisture and temperature anomalies over South America derived from GPS radio occultation profiles Llamedo, P. Hierro, R. de la Torre, A. Alexander, P. ENSO FORMOSAT-3/COSMIC precipitable water South America Atmospheric humidity Atmospheric pressure Atmospheric temperature Global positioning system Nickel Oceanography Time series analysis Wavelet transforms Continuous Wavelet Transform ENSO Equatorial Pacific Ocean FORMOSAT-3/COSMIC High vertical resolution Precipitable water Precipitable water content South America Climatology air temperature atmospheric moisture COSMIC El Nino-Southern Oscillation FORMOSAT GPS precipitable water temperature anomaly South America El Niño Southern Oscillation- (ENSO) related anomaly patterns of monthly specific humidity (q), precipitable water content (PW) and temperature (T) over South America are analysed using the FORMOSAT-3/COSMIC mission data (August 2006–December 2013). The Global Positioning System radio occultation (GPS RO) technique provides high vertical resolution profiles of atmospheric properties (refractivity, density, temperature and water vapour pressure) with a global coverage under any weather condition. During the ENSO warm phase (or El Niño), positive PW anomalies are found over the equatorial Pacific Ocean, southeastern Brazil, Bolivia, Paraguay and northern Argentina. Negative anomalies are found in the northern part of South America, but covering a smaller area. During the ENSO cold phase (or La Niña), positive anomalies are found in the northern part of the continent whereas negative anomalies are found over the Amazon Basin region. A Morlet continuous wavelet transform analysis is applied to deseasonalized PW anomaly time series. Over the areas showing PW anomalies related to ENSO, main modes of oscillation between 35 and 38 months are found, similar to the main oscillation mode of the Oceanic Niño index. Consistent with previous studies, PW anomalies in almost all these areas show a general behaviour towards opposite signals during the opposite ENSO phases. q patterns show a linear (in phase with Oceanic Niño Index) response to ENSO along the equator below 8 km height. The Andes mountains separate positive (west) from negative (east) anomalies during El Niño (EN) events (reversing during LN). The higher q positive anomalies are found over the equatorial Pacific Ocean and over 60°–50°W, 35°–20°S during EN months. T patterns show positive anomalies in the whole tropical troposphere during EN months, with higher values over the equatorial Pacific, west of the Andes between 7 and 15 km height. © 2016 Royal Meteorological Society Fil:Hierro, R. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. JOUR info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/2.5/ar http://hdl.handle.net/20.500.12110/paper_08998418_v37_n1_p268_Llamedo
institution Universidad de Buenos Aires
institution_str I-28
repository_str R-134
collection Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA)
topic ENSO
FORMOSAT-3/COSMIC
precipitable water
South America
Atmospheric humidity
Atmospheric pressure
Atmospheric temperature
Global positioning system
Nickel
Oceanography
Time series analysis
Wavelet transforms
Continuous Wavelet Transform
ENSO
Equatorial Pacific Ocean
FORMOSAT-3/COSMIC
High vertical resolution
Precipitable water
Precipitable water content
South America
Climatology
air temperature
atmospheric moisture
COSMIC
El Nino-Southern Oscillation
FORMOSAT
GPS
precipitable water
temperature anomaly
South America
spellingShingle ENSO
FORMOSAT-3/COSMIC
precipitable water
South America
Atmospheric humidity
Atmospheric pressure
Atmospheric temperature
Global positioning system
Nickel
Oceanography
Time series analysis
Wavelet transforms
Continuous Wavelet Transform
ENSO
Equatorial Pacific Ocean
FORMOSAT-3/COSMIC
High vertical resolution
Precipitable water
Precipitable water content
South America
Climatology
air temperature
atmospheric moisture
COSMIC
El Nino-Southern Oscillation
FORMOSAT
GPS
precipitable water
temperature anomaly
South America
Llamedo, P.
Hierro, R.
de la Torre, A.
Alexander, P.
ENSO-related moisture and temperature anomalies over South America derived from GPS radio occultation profiles
topic_facet ENSO
FORMOSAT-3/COSMIC
precipitable water
South America
Atmospheric humidity
Atmospheric pressure
Atmospheric temperature
Global positioning system
Nickel
Oceanography
Time series analysis
Wavelet transforms
Continuous Wavelet Transform
ENSO
Equatorial Pacific Ocean
FORMOSAT-3/COSMIC
High vertical resolution
Precipitable water
Precipitable water content
South America
Climatology
air temperature
atmospheric moisture
COSMIC
El Nino-Southern Oscillation
FORMOSAT
GPS
precipitable water
temperature anomaly
South America
description El Niño Southern Oscillation- (ENSO) related anomaly patterns of monthly specific humidity (q), precipitable water content (PW) and temperature (T) over South America are analysed using the FORMOSAT-3/COSMIC mission data (August 2006–December 2013). The Global Positioning System radio occultation (GPS RO) technique provides high vertical resolution profiles of atmospheric properties (refractivity, density, temperature and water vapour pressure) with a global coverage under any weather condition. During the ENSO warm phase (or El Niño), positive PW anomalies are found over the equatorial Pacific Ocean, southeastern Brazil, Bolivia, Paraguay and northern Argentina. Negative anomalies are found in the northern part of South America, but covering a smaller area. During the ENSO cold phase (or La Niña), positive anomalies are found in the northern part of the continent whereas negative anomalies are found over the Amazon Basin region. A Morlet continuous wavelet transform analysis is applied to deseasonalized PW anomaly time series. Over the areas showing PW anomalies related to ENSO, main modes of oscillation between 35 and 38 months are found, similar to the main oscillation mode of the Oceanic Niño index. Consistent with previous studies, PW anomalies in almost all these areas show a general behaviour towards opposite signals during the opposite ENSO phases. q patterns show a linear (in phase with Oceanic Niño Index) response to ENSO along the equator below 8 km height. The Andes mountains separate positive (west) from negative (east) anomalies during El Niño (EN) events (reversing during LN). The higher q positive anomalies are found over the equatorial Pacific Ocean and over 60°–50°W, 35°–20°S during EN months. T patterns show positive anomalies in the whole tropical troposphere during EN months, with higher values over the equatorial Pacific, west of the Andes between 7 and 15 km height. © 2016 Royal Meteorological Society
format JOUR
author Llamedo, P.
Hierro, R.
de la Torre, A.
Alexander, P.
author_facet Llamedo, P.
Hierro, R.
de la Torre, A.
Alexander, P.
author_sort Llamedo, P.
title ENSO-related moisture and temperature anomalies over South America derived from GPS radio occultation profiles
title_short ENSO-related moisture and temperature anomalies over South America derived from GPS radio occultation profiles
title_full ENSO-related moisture and temperature anomalies over South America derived from GPS radio occultation profiles
title_fullStr ENSO-related moisture and temperature anomalies over South America derived from GPS radio occultation profiles
title_full_unstemmed ENSO-related moisture and temperature anomalies over South America derived from GPS radio occultation profiles
title_sort enso-related moisture and temperature anomalies over south america derived from gps radio occultation profiles
url http://hdl.handle.net/20.500.12110/paper_08998418_v37_n1_p268_Llamedo
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