A comparative and numerical study of effects of gravity waves in small miss-distance and miss-time GPS radio occultation temperature profiles
The Global Positioning System (GPS) Radio Occultation (RO) technique has global coverage and is capable of generating high vertical resolution temperature profiles of the upper troposphere and lower stratosphere with sub-Kelvin accuracy and long-term stability, regardless of weather conditions. In t...
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paper:paper_02731177_v45_n10_p1231_Alexander2023-06-08T15:25:38Z A comparative and numerical study of effects of gravity waves in small miss-distance and miss-time GPS radio occultation temperature profiles Alexander, Pedro M. De La Torre, Alejandro Eduardo Llamedo Soria, Pablo Martín Gravity waves Numerical simulation Radio occultation Stratosphere Close-in Constellation observing system for meteorology Eastern side Global coverage High density High vertical resolution Inhomogeneous structure Ionosphere and climates Long term stability Lower stratosphere Mesoscale model Miss-distance Numerical simulation Numerical studies Radio occultation Radio occultations Temperature profiles Time and space Upper troposphere Wave activity Weather conditions Atmospherics Computer simulation Cosmology Global positioning system Gravitational effects Gravity waves Hydrodynamics Ionosphere Meteorology Radio Sulfur compounds Temperature control Waves Mathematical models The Global Positioning System (GPS) Radio Occultation (RO) technique has global coverage and is capable of generating high vertical resolution temperature profiles of the upper troposphere and lower stratosphere with sub-Kelvin accuracy and long-term stability, regardless of weather conditions. In this work, we take advantage of the anomalously high density of occultation events at the eastern side of the highest Andes Mountains during the initial mission months of COSMIC (Constellation Observing System for Meteorology, Ionosphere and Climate). This region is well-known for its high wave activity. We choose to study two pairs of GPS RO, both containing two occultations that occurred close in time and space. One pair shows significant differences between both temperature profiles. Numerical simulations with a mesoscale model were performed, in order to understand this discrepancy. It is attributed to the presence of a horizontal inhomogeneous structure caused by gravity waves. © 2010 COSPAR. Fil:Alexander, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:de la Torre, A. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Llamedo, P. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. 2010 https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02731177_v45_n10_p1231_Alexander http://hdl.handle.net/20.500.12110/paper_02731177_v45_n10_p1231_Alexander |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Gravity waves Numerical simulation Radio occultation Stratosphere Close-in Constellation observing system for meteorology Eastern side Global coverage High density High vertical resolution Inhomogeneous structure Ionosphere and climates Long term stability Lower stratosphere Mesoscale model Miss-distance Numerical simulation Numerical studies Radio occultation Radio occultations Temperature profiles Time and space Upper troposphere Wave activity Weather conditions Atmospherics Computer simulation Cosmology Global positioning system Gravitational effects Gravity waves Hydrodynamics Ionosphere Meteorology Radio Sulfur compounds Temperature control Waves Mathematical models |
spellingShingle |
Gravity waves Numerical simulation Radio occultation Stratosphere Close-in Constellation observing system for meteorology Eastern side Global coverage High density High vertical resolution Inhomogeneous structure Ionosphere and climates Long term stability Lower stratosphere Mesoscale model Miss-distance Numerical simulation Numerical studies Radio occultation Radio occultations Temperature profiles Time and space Upper troposphere Wave activity Weather conditions Atmospherics Computer simulation Cosmology Global positioning system Gravitational effects Gravity waves Hydrodynamics Ionosphere Meteorology Radio Sulfur compounds Temperature control Waves Mathematical models Alexander, Pedro M. De La Torre, Alejandro Eduardo Llamedo Soria, Pablo Martín A comparative and numerical study of effects of gravity waves in small miss-distance and miss-time GPS radio occultation temperature profiles |
topic_facet |
Gravity waves Numerical simulation Radio occultation Stratosphere Close-in Constellation observing system for meteorology Eastern side Global coverage High density High vertical resolution Inhomogeneous structure Ionosphere and climates Long term stability Lower stratosphere Mesoscale model Miss-distance Numerical simulation Numerical studies Radio occultation Radio occultations Temperature profiles Time and space Upper troposphere Wave activity Weather conditions Atmospherics Computer simulation Cosmology Global positioning system Gravitational effects Gravity waves Hydrodynamics Ionosphere Meteorology Radio Sulfur compounds Temperature control Waves Mathematical models |
description |
The Global Positioning System (GPS) Radio Occultation (RO) technique has global coverage and is capable of generating high vertical resolution temperature profiles of the upper troposphere and lower stratosphere with sub-Kelvin accuracy and long-term stability, regardless of weather conditions. In this work, we take advantage of the anomalously high density of occultation events at the eastern side of the highest Andes Mountains during the initial mission months of COSMIC (Constellation Observing System for Meteorology, Ionosphere and Climate). This region is well-known for its high wave activity. We choose to study two pairs of GPS RO, both containing two occultations that occurred close in time and space. One pair shows significant differences between both temperature profiles. Numerical simulations with a mesoscale model were performed, in order to understand this discrepancy. It is attributed to the presence of a horizontal inhomogeneous structure caused by gravity waves. © 2010 COSPAR. |
author |
Alexander, Pedro M. De La Torre, Alejandro Eduardo Llamedo Soria, Pablo Martín |
author_facet |
Alexander, Pedro M. De La Torre, Alejandro Eduardo Llamedo Soria, Pablo Martín |
author_sort |
Alexander, Pedro M. |
title |
A comparative and numerical study of effects of gravity waves in small miss-distance and miss-time GPS radio occultation temperature profiles |
title_short |
A comparative and numerical study of effects of gravity waves in small miss-distance and miss-time GPS radio occultation temperature profiles |
title_full |
A comparative and numerical study of effects of gravity waves in small miss-distance and miss-time GPS radio occultation temperature profiles |
title_fullStr |
A comparative and numerical study of effects of gravity waves in small miss-distance and miss-time GPS radio occultation temperature profiles |
title_full_unstemmed |
A comparative and numerical study of effects of gravity waves in small miss-distance and miss-time GPS radio occultation temperature profiles |
title_sort |
comparative and numerical study of effects of gravity waves in small miss-distance and miss-time gps radio occultation temperature profiles |
publishDate |
2010 |
url |
https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_02731177_v45_n10_p1231_Alexander http://hdl.handle.net/20.500.12110/paper_02731177_v45_n10_p1231_Alexander |
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