Factores advectivos en el clima de la Puna Argentina

Autores
Prohaska, Federico J.
Año de publicación
1962
Idioma
español castellano
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Advective factors in tbe climate o f tbe argentine Altiplano. The dimate of the argentine Altiplano, predominantly autoctonous, is modified in its northeastern part by the advection of air-masses of tropical origin during the summer season, caused by the general atmospheric circulation. The mean wind direction is Northeast during the summer months (Nov.-March) and west and south in winter. In both seasons the gradient wind has approximately the same direction as the local thermal wind system, from the plains towards the mountains in summer and the other way round in winter. This advection introduces tropical characteristics in the typical subtropical climate of the frontier — zone between Bolivia and Argentina of the Altiplano as exemplified by the observations of the Geophysical Observatory of La Quiaca (22’06’S; 65"36’W ; 3.-Í60 m) : high atmospheric humidity, low clouds, precipitations, inestability of the air-masses and thunderstorms; all these meteorological elements are influencing the radiation balance of short and Iong wave lengths and thereby also the temperature and its variation (aperiodic, periodic, interdiurnal, etc.). This transpon of air-masses from the tropical zones to the Cordillera produces a great uniformity in the climatic conditions on the entire eastern slope of the Andes, from Perú to the extrem north of Argentine during the summertime.
Fil: Prohaska, Federico J.. Instituto Nacional de Tecnología Agropecuaria (Argentina)
Fuente
Boletín de Estudios Geográficos, No. 35
http://bdigital.uncu.edu.ar/11392
Materia
Clima
Puna de Atacama (Argentina)
Nivel de accesibilidad
acceso abierto
Condiciones de uso
http://creativecommons.org/licenses/by/2.5/ar/
Repositorio
Biblioteca Digital (UNCu)
Institución
Universidad Nacional de Cuyo
OAI Identificador
oai:bdigital.uncu.edu.ar:11393

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network_name_str Biblioteca Digital (UNCu)
spelling Factores advectivos en el clima de la Puna Argentina Prohaska, Federico J.ClimaPuna de Atacama (Argentina)Advective factors in tbe climate o f tbe argentine Altiplano. The dimate of the argentine Altiplano, predominantly autoctonous, is modified in its northeastern part by the advection of air-masses of tropical origin during the summer season, caused by the general atmospheric circulation. The mean wind direction is Northeast during the summer months (Nov.-March) and west and south in winter. In both seasons the gradient wind has approximately the same direction as the local thermal wind system, from the plains towards the mountains in summer and the other way round in winter. This advection introduces tropical characteristics in the typical subtropical climate of the frontier — zone between Bolivia and Argentina of the Altiplano as exemplified by the observations of the Geophysical Observatory of La Quiaca (22’06’S; 65"36’W ; 3.-Í60 m) : high atmospheric humidity, low clouds, precipitations, inestability of the air-masses and thunderstorms; all these meteorological elements are influencing the radiation balance of short and Iong wave lengths and thereby also the temperature and its variation (aperiodic, periodic, interdiurnal, etc.). This transpon of air-masses from the tropical zones to the Cordillera produces a great uniformity in the climatic conditions on the entire eastern slope of the Andes, from Perú to the extrem north of Argentine during the summertime.Fil: Prohaska, Federico J.. Instituto Nacional de Tecnología Agropecuaria (Argentina) Universidad Nacional de Cuyo. Facultad de Filosofía y Letras. Instituto de Geografía1962-04-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttp://bdigital.uncu.edu.ar/11393Boletín de Estudios Geográficos, No. 35http://bdigital.uncu.edu.ar/11392reponame:Biblioteca Digital (UNCu)instname:Universidad Nacional de Cuyoinstacron:UNCUspainfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/2.5/ar/2025-09-04T09:44:29Zoai:bdigital.uncu.edu.ar:11393Institucionalhttp://bdigital.uncu.edu.ar/Universidad públicaNo correspondehttp://bdigital.uncu.edu.ar/OAI/hdegiorgi@uncu.edu.ar;horaciod@gmail.comArgentinaNo correspondeNo correspondeNo correspondeopendoar:15842025-09-04 09:44:30.481Biblioteca Digital (UNCu) - Universidad Nacional de Cuyofalse
dc.title.none.fl_str_mv Factores advectivos en el clima de la Puna Argentina
title Factores advectivos en el clima de la Puna Argentina
spellingShingle Factores advectivos en el clima de la Puna Argentina
Prohaska, Federico J.
Clima
Puna de Atacama (Argentina)
title_short Factores advectivos en el clima de la Puna Argentina
title_full Factores advectivos en el clima de la Puna Argentina
title_fullStr Factores advectivos en el clima de la Puna Argentina
title_full_unstemmed Factores advectivos en el clima de la Puna Argentina
title_sort Factores advectivos en el clima de la Puna Argentina
dc.creator.none.fl_str_mv Prohaska, Federico J.
author Prohaska, Federico J.
author_facet Prohaska, Federico J.
author_role author
dc.subject.none.fl_str_mv Clima
Puna de Atacama (Argentina)
topic Clima
Puna de Atacama (Argentina)
dc.description.none.fl_txt_mv Advective factors in tbe climate o f tbe argentine Altiplano. The dimate of the argentine Altiplano, predominantly autoctonous, is modified in its northeastern part by the advection of air-masses of tropical origin during the summer season, caused by the general atmospheric circulation. The mean wind direction is Northeast during the summer months (Nov.-March) and west and south in winter. In both seasons the gradient wind has approximately the same direction as the local thermal wind system, from the plains towards the mountains in summer and the other way round in winter. This advection introduces tropical characteristics in the typical subtropical climate of the frontier — zone between Bolivia and Argentina of the Altiplano as exemplified by the observations of the Geophysical Observatory of La Quiaca (22’06’S; 65"36’W ; 3.-Í60 m) : high atmospheric humidity, low clouds, precipitations, inestability of the air-masses and thunderstorms; all these meteorological elements are influencing the radiation balance of short and Iong wave lengths and thereby also the temperature and its variation (aperiodic, periodic, interdiurnal, etc.). This transpon of air-masses from the tropical zones to the Cordillera produces a great uniformity in the climatic conditions on the entire eastern slope of the Andes, from Perú to the extrem north of Argentine during the summertime.
Fil: Prohaska, Federico J.. Instituto Nacional de Tecnología Agropecuaria (Argentina)
description Advective factors in tbe climate o f tbe argentine Altiplano. The dimate of the argentine Altiplano, predominantly autoctonous, is modified in its northeastern part by the advection of air-masses of tropical origin during the summer season, caused by the general atmospheric circulation. The mean wind direction is Northeast during the summer months (Nov.-March) and west and south in winter. In both seasons the gradient wind has approximately the same direction as the local thermal wind system, from the plains towards the mountains in summer and the other way round in winter. This advection introduces tropical characteristics in the typical subtropical climate of the frontier — zone between Bolivia and Argentina of the Altiplano as exemplified by the observations of the Geophysical Observatory of La Quiaca (22’06’S; 65"36’W ; 3.-Í60 m) : high atmospheric humidity, low clouds, precipitations, inestability of the air-masses and thunderstorms; all these meteorological elements are influencing the radiation balance of short and Iong wave lengths and thereby also the temperature and its variation (aperiodic, periodic, interdiurnal, etc.). This transpon of air-masses from the tropical zones to the Cordillera produces a great uniformity in the climatic conditions on the entire eastern slope of the Andes, from Perú to the extrem north of Argentine during the summertime.
publishDate 1962
dc.date.none.fl_str_mv 1962-04-10
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://bdigital.uncu.edu.ar/11393
url http://bdigital.uncu.edu.ar/11393
dc.language.none.fl_str_mv spa
language spa
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv http://creativecommons.org/licenses/by/2.5/ar/
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidad Nacional de Cuyo. Facultad de Filosofía y Letras. Instituto de Geografía
publisher.none.fl_str_mv Universidad Nacional de Cuyo. Facultad de Filosofía y Letras. Instituto de Geografía
dc.source.none.fl_str_mv Boletín de Estudios Geográficos, No. 35
http://bdigital.uncu.edu.ar/11392
reponame:Biblioteca Digital (UNCu)
instname:Universidad Nacional de Cuyo
instacron:UNCU
reponame_str Biblioteca Digital (UNCu)
collection Biblioteca Digital (UNCu)
instname_str Universidad Nacional de Cuyo
instacron_str UNCU
institution UNCU
repository.name.fl_str_mv Biblioteca Digital (UNCu) - Universidad Nacional de Cuyo
repository.mail.fl_str_mv hdegiorgi@uncu.edu.ar;horaciod@gmail.com
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score 12.623145