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
- Institución
- Universidad Nacional de Cuyo
- OAI Identificador
- oai:bdigital.uncu.edu.ar:11393
Ver los metadatos del registro completo
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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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1842340557444087808 |
score |
12.623145 |