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...

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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
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openAccess
License
Atribución-NoComercial 4.0 Internacional
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spelling 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
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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
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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/
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eu_rights_str_mv openAccess
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dc.publisher.spa.fl_str_mv American Meteorological Society
institution Universidad Nacional de Colombia
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