Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena
The hydroclimatology of tropical South America is strongly coupled to low-frequency large-scale oceanic and atmospheric phenomena occurring over the Pacific and the Atlantic Oceans. In particular, El Nin˜o–Southern Oscillation (ENSO) affects climatic and hydrologic conditions on timescales ranging f...
- Autores:
-
Poveda Jaramillo, Germán
Mesa Sánchez, Óscar José
- Tipo de recurso:
- Article of journal
- Fecha de publicación:
- 1997
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- spa
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/70051
- Acceso en línea:
- https://repositorio.unal.edu.co/handle/unal/70051
http://bdigital.unal.edu.co/2198/
- Palabra clave:
- 55 Ciencias de la tierra / Earth sciences and geology
- Rights
- openAccess
- License
- Atribución-NoComercial 4.0 Internacional
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Atribución-NoComercial 4.0 InternacionalDerechos reservados - Universidad Nacional de Colombiahttp://creativecommons.org/licenses/by-nc/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Poveda Jaramillo, Germán84cea7b3-660a-4190-ac80-7a6a58f6d772300Mesa Sánchez, Óscar José9a42bf9e-dd9e-4948-a5c4-25b08ceef53e3002019-07-03T13:07:56Z2019-07-03T13:07:56Z1997ISSN: 0894-8755https://repositorio.unal.edu.co/handle/unal/70051http://bdigital.unal.edu.co/2198/The hydroclimatology of tropical South America is strongly coupled to low-frequency large-scale oceanic and atmospheric phenomena occurring over the Pacific and the Atlantic Oceans. In particular, El Nin˜o–Southern Oscillation (ENSO) affects climatic and hydrologic conditions on timescales ranging from seasons to decades. With some regional differences in timing and amplitude, tropical South America exhibits negative rainfall and streamflow anomalies in association with the low–warm phase of the Southern Oscillation (El Nin˜o), and positive anomalies with the high–cold phase. Such dependence is illustrated in the hydroclimatology of Colombia through several empirical analyses: correlation, empirical orthogonal functions, principal component, and spectral analysis, and discussion of the major physical mechanisms. Observations show that ENSO’s effect on river discharges occurs progressively later for rivers toward the east in Colombia and northern South America. Also, the impacts of La Nin˜a are more pronounced than those of El Nin˜o. Evidence is also presented to show that processes arising from land–atmosphere interactions in tropical South America affect sea surface temperatures in the Caribbean and the north tropical Atlantic. A hypothesis is formulated to explain these feedback mechanisms through perturbations in precipitation, soil moisture, and evapotranspiration over the continent. To begin with, the occurrence of both phases of ENSO affects all those fields. The proposed mechanisms would constitute the ‘‘land– atmosphere’’ bridge connecting Pacific and Atlantic SST anomalies.application/pdfspaAmerican Meteorological SocietyUniversidad Nacional de Colombia Sede Medellín Facultad de Minas Escuela de Geociencias y Medio AmbienteEscuela de Geociencias y Medio AmbientePoveda Jaramillo, Germán and Mesa Sánchez, Óscar José (1997) Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena. Journal of Climate, 10 (10). pp. 2690-2702. ISSN 0894-875555 Ciencias de la tierra / Earth sciences and geologyFeedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomenaArtículo de revistainfo:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1http://purl.org/coar/version/c_970fb48d4fbd8a85Texthttp://purl.org/redcol/resource_type/ARTORIGINALPoveda_&_Mesa_J_Climate.pdfapplication/pdf870837https://repositorio.unal.edu.co/bitstream/unal/70051/1/Poveda_%26_Mesa_J_Climate.pdf5d133a4286a33bc307448e0ecfc46cacMD51THUMBNAILPoveda_&_Mesa_J_Climate.pdf.jpgPoveda_&_Mesa_J_Climate.pdf.jpgGenerated Thumbnailimage/jpeg8675https://repositorio.unal.edu.co/bitstream/unal/70051/2/Poveda_%26_Mesa_J_Climate.pdf.jpge3d8f88319327a543e72540244b39389MD52unal/70051oai:repositorio.unal.edu.co:unal/700512024-06-04 23:08:58.629Repositorio Institucional Universidad Nacional de Colombiarepositorio_nal@unal.edu.co |
dc.title.spa.fl_str_mv |
Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena |
title |
Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena |
spellingShingle |
Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena 55 Ciencias de la tierra / Earth sciences and geology |
title_short |
Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena |
title_full |
Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena |
title_fullStr |
Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena |
title_full_unstemmed |
Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena |
title_sort |
Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena |
dc.creator.fl_str_mv |
Poveda Jaramillo, Germán Mesa Sánchez, Óscar José |
dc.contributor.author.spa.fl_str_mv |
Poveda Jaramillo, Germán Mesa Sánchez, Óscar José |
dc.subject.ddc.spa.fl_str_mv |
55 Ciencias de la tierra / Earth sciences and geology |
topic |
55 Ciencias de la tierra / Earth sciences and geology |
description |
The hydroclimatology of tropical South America is strongly coupled to low-frequency large-scale oceanic and atmospheric phenomena occurring over the Pacific and the Atlantic Oceans. In particular, El Nin˜o–Southern Oscillation (ENSO) affects climatic and hydrologic conditions on timescales ranging from seasons to decades. With some regional differences in timing and amplitude, tropical South America exhibits negative rainfall and streamflow anomalies in association with the low–warm phase of the Southern Oscillation (El Nin˜o), and positive anomalies with the high–cold phase. Such dependence is illustrated in the hydroclimatology of Colombia through several empirical analyses: correlation, empirical orthogonal functions, principal component, and spectral analysis, and discussion of the major physical mechanisms. Observations show that ENSO’s effect on river discharges occurs progressively later for rivers toward the east in Colombia and northern South America. Also, the impacts of La Nin˜a are more pronounced than those of El Nin˜o. Evidence is also presented to show that processes arising from land–atmosphere interactions in tropical South America affect sea surface temperatures in the Caribbean and the north tropical Atlantic. A hypothesis is formulated to explain these feedback mechanisms through perturbations in precipitation, soil moisture, and evapotranspiration over the continent. To begin with, the occurrence of both phases of ENSO affects all those fields. The proposed mechanisms would constitute the ‘‘land– atmosphere’’ bridge connecting Pacific and Atlantic SST anomalies. |
publishDate |
1997 |
dc.date.issued.spa.fl_str_mv |
1997 |
dc.date.accessioned.spa.fl_str_mv |
2019-07-03T13:07:56Z |
dc.date.available.spa.fl_str_mv |
2019-07-03T13:07:56Z |
dc.type.spa.fl_str_mv |
Artículo de revista |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_2df8fbb1 |
dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/article |
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info:eu-repo/semantics/publishedVersion |
dc.type.coar.spa.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 |
dc.type.coarversion.spa.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.content.spa.fl_str_mv |
Text |
dc.type.redcol.spa.fl_str_mv |
http://purl.org/redcol/resource_type/ART |
format |
http://purl.org/coar/resource_type/c_6501 |
status_str |
publishedVersion |
dc.identifier.issn.spa.fl_str_mv |
ISSN: 0894-8755 |
dc.identifier.uri.none.fl_str_mv |
https://repositorio.unal.edu.co/handle/unal/70051 |
dc.identifier.eprints.spa.fl_str_mv |
http://bdigital.unal.edu.co/2198/ |
identifier_str_mv |
ISSN: 0894-8755 |
url |
https://repositorio.unal.edu.co/handle/unal/70051 http://bdigital.unal.edu.co/2198/ |
dc.language.iso.spa.fl_str_mv |
spa |
language |
spa |
dc.relation.ispartof.spa.fl_str_mv |
Universidad Nacional de Colombia Sede Medellín Facultad de Minas Escuela de Geociencias y Medio Ambiente Escuela de Geociencias y Medio Ambiente |
dc.relation.references.spa.fl_str_mv |
Poveda Jaramillo, Germán and Mesa Sánchez, Óscar José (1997) Feedbacks between hydrological processes in tropical South America and large-scale ocean-atmospheric phenomena. Journal of Climate, 10 (10). pp. 2690-2702. ISSN 0894-8755 |
dc.rights.spa.fl_str_mv |
Derechos reservados - Universidad Nacional de Colombia |
dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
dc.rights.license.spa.fl_str_mv |
Atribución-NoComercial 4.0 Internacional |
dc.rights.uri.spa.fl_str_mv |
http://creativecommons.org/licenses/by-nc/4.0/ |
dc.rights.accessrights.spa.fl_str_mv |
info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
Atribución-NoComercial 4.0 Internacional Derechos reservados - Universidad Nacional de Colombia http://creativecommons.org/licenses/by-nc/4.0/ http://purl.org/coar/access_right/c_abf2 |
eu_rights_str_mv |
openAccess |
dc.format.mimetype.spa.fl_str_mv |
application/pdf |
dc.publisher.spa.fl_str_mv |
American Meteorological Society |
institution |
Universidad Nacional de Colombia |
bitstream.url.fl_str_mv |
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