Verification of the geographical origin of modeled air-mass trajectories by means of the isotope composition of rainwater during the SALLJEX experiment
The SALLJEX experiment was held during the summer 2002-2003. It consisted of three-dimensional observation of the atmosphere to study the structure of the low level jet along the eastern slopes of the Andes. Daily precipitation water samples were collected at two stations (Resistencia and Salta) in...
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todo:paper_15677419_v9_n4_p409_Gonzalez2023-10-03T16:26:42Z Verification of the geographical origin of modeled air-mass trajectories by means of the isotope composition of rainwater during the SALLJEX experiment González, M. Dapeña, C. Cerne, B. Sánchez-Ccoyllo, O. Freitas, S. Silva Dias, P.L. Panarello, H. Air mass trajectories Isotope content Low level jet Rainfall 3-D kinematics Air mass Air mass trajectories Air parcels Argentina Continental origin Geographical origins Isotope compositions Isotope data Low level jet Oxygen-18 Rainfall Sao Paulo , Brazil Three-dimensional observations Water samples Deuterium Experiments Jets Kinematics Oxygen Trajectories Water content Three dimensional air mass atmospheric modeling deuterium experimental study isotopic composition jet flow orographic effect oxygen isotope precipitation quality rainfall rainwater three-dimensional modeling topographic effect Andes Argentina Chaco [Argentina] Resistencia Salta [Argentina] Salta [Salta (PRV)] South America The SALLJEX experiment was held during the summer 2002-2003. It consisted of three-dimensional observation of the atmosphere to study the structure of the low level jet along the eastern slopes of the Andes. Daily precipitation water samples were collected at two stations (Resistencia and Salta) in northern Argentina and isotope content was analyzed. The isotope data were used in conjunction with air parcel trajectories obtained from a 3-D kinematic model (3D-MTC) developed by the University of Sao Paulo, Brazil. Values of deuterium excess were related with air masses of continental origin, whilst low values were associated with air masses with longer oceanic trajectories. Furthermore, although data are scarce, results show that oxygen-18 and deuterium excess in rainwater are related with the occurrence of the low level jet. © Springer Science+Business Media B.V. 2009. Fil:González, M. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Dapeña, C. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Cerne, B. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales; Argentina. Fil:Panarello, H. 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_15677419_v9_n4_p409_Gonzalez |
institution |
Universidad de Buenos Aires |
institution_str |
I-28 |
repository_str |
R-134 |
collection |
Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) |
topic |
Air mass trajectories Isotope content Low level jet Rainfall 3-D kinematics Air mass Air mass trajectories Air parcels Argentina Continental origin Geographical origins Isotope compositions Isotope data Low level jet Oxygen-18 Rainfall Sao Paulo , Brazil Three-dimensional observations Water samples Deuterium Experiments Jets Kinematics Oxygen Trajectories Water content Three dimensional air mass atmospheric modeling deuterium experimental study isotopic composition jet flow orographic effect oxygen isotope precipitation quality rainfall rainwater three-dimensional modeling topographic effect Andes Argentina Chaco [Argentina] Resistencia Salta [Argentina] Salta [Salta (PRV)] South America |
spellingShingle |
Air mass trajectories Isotope content Low level jet Rainfall 3-D kinematics Air mass Air mass trajectories Air parcels Argentina Continental origin Geographical origins Isotope compositions Isotope data Low level jet Oxygen-18 Rainfall Sao Paulo , Brazil Three-dimensional observations Water samples Deuterium Experiments Jets Kinematics Oxygen Trajectories Water content Three dimensional air mass atmospheric modeling deuterium experimental study isotopic composition jet flow orographic effect oxygen isotope precipitation quality rainfall rainwater three-dimensional modeling topographic effect Andes Argentina Chaco [Argentina] Resistencia Salta [Argentina] Salta [Salta (PRV)] South America González, M. Dapeña, C. Cerne, B. Sánchez-Ccoyllo, O. Freitas, S. Silva Dias, P.L. Panarello, H. Verification of the geographical origin of modeled air-mass trajectories by means of the isotope composition of rainwater during the SALLJEX experiment |
topic_facet |
Air mass trajectories Isotope content Low level jet Rainfall 3-D kinematics Air mass Air mass trajectories Air parcels Argentina Continental origin Geographical origins Isotope compositions Isotope data Low level jet Oxygen-18 Rainfall Sao Paulo , Brazil Three-dimensional observations Water samples Deuterium Experiments Jets Kinematics Oxygen Trajectories Water content Three dimensional air mass atmospheric modeling deuterium experimental study isotopic composition jet flow orographic effect oxygen isotope precipitation quality rainfall rainwater three-dimensional modeling topographic effect Andes Argentina Chaco [Argentina] Resistencia Salta [Argentina] Salta [Salta (PRV)] South America |
description |
The SALLJEX experiment was held during the summer 2002-2003. It consisted of three-dimensional observation of the atmosphere to study the structure of the low level jet along the eastern slopes of the Andes. Daily precipitation water samples were collected at two stations (Resistencia and Salta) in northern Argentina and isotope content was analyzed. The isotope data were used in conjunction with air parcel trajectories obtained from a 3-D kinematic model (3D-MTC) developed by the University of Sao Paulo, Brazil. Values of deuterium excess were related with air masses of continental origin, whilst low values were associated with air masses with longer oceanic trajectories. Furthermore, although data are scarce, results show that oxygen-18 and deuterium excess in rainwater are related with the occurrence of the low level jet. © Springer Science+Business Media B.V. 2009. |
format |
JOUR |
author |
González, M. Dapeña, C. Cerne, B. Sánchez-Ccoyllo, O. Freitas, S. Silva Dias, P.L. Panarello, H. |
author_facet |
González, M. Dapeña, C. Cerne, B. Sánchez-Ccoyllo, O. Freitas, S. Silva Dias, P.L. Panarello, H. |
author_sort |
González, M. |
title |
Verification of the geographical origin of modeled air-mass trajectories by means of the isotope composition of rainwater during the SALLJEX experiment |
title_short |
Verification of the geographical origin of modeled air-mass trajectories by means of the isotope composition of rainwater during the SALLJEX experiment |
title_full |
Verification of the geographical origin of modeled air-mass trajectories by means of the isotope composition of rainwater during the SALLJEX experiment |
title_fullStr |
Verification of the geographical origin of modeled air-mass trajectories by means of the isotope composition of rainwater during the SALLJEX experiment |
title_full_unstemmed |
Verification of the geographical origin of modeled air-mass trajectories by means of the isotope composition of rainwater during the SALLJEX experiment |
title_sort |
verification of the geographical origin of modeled air-mass trajectories by means of the isotope composition of rainwater during the salljex experiment |
url |
http://hdl.handle.net/20.500.12110/paper_15677419_v9_n4_p409_Gonzalez |
work_keys_str_mv |
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