Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection

RESUMEN: We have observed that the dry-season length (DSL) has increased over southern Amazonia since 1979, primarily owing to a delay of its ending dates (dry-season end, DSE), and is accompanied by a prolonged fire season. A poleward shift of the subtropical jet over South America and an increase...

Full description

Autores:
Yin, Lei
Li, Wenhong
Arias Gómez, Paola Andrea
Dickinson, Robert E.
Huang, Lei
Chakraborty, Sudip
Fernandes, Katia
Liebmann, Brant
Fisher, Rosie
Myneni, Ranga B.
Tipo de recurso:
Article of investigation
Fecha de publicación:
2013
Institución:
Universidad de Antioquia
Repositorio:
Repositorio UdeA
Idioma:
eng
OAI Identifier:
oai:bibliotecadigital.udea.edu.co:10495/7642
Acceso en línea:
http://hdl.handle.net/10495/7642
Palabra clave:
Cimate variability
Climate model projection
Rainforests
Rights
openAccess
License
https://creativecommons.org/licenses/by-nc-nd/4.0/
id UDEA2_f21bc632aefaf6ff224a5b802882f085
oai_identifier_str oai:bibliotecadigital.udea.edu.co:10495/7642
network_acronym_str UDEA2
network_name_str Repositorio UdeA
repository_id_str
dc.title.spa.fl_str_mv Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection
title Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection
spellingShingle Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection
Cimate variability
Climate model projection
Rainforests
title_short Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection
title_full Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection
title_fullStr Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection
title_full_unstemmed Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection
title_sort Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection
dc.creator.fl_str_mv Yin, Lei
Li, Wenhong
Arias Gómez, Paola Andrea
Dickinson, Robert E.
Huang, Lei
Chakraborty, Sudip
Fernandes, Katia
Liebmann, Brant
Fisher, Rosie
Myneni, Ranga B.
dc.contributor.author.none.fl_str_mv Yin, Lei
Li, Wenhong
Arias Gómez, Paola Andrea
Dickinson, Robert E.
Huang, Lei
Chakraborty, Sudip
Fernandes, Katia
Liebmann, Brant
Fisher, Rosie
Myneni, Ranga B.
dc.contributor.researchgroup.spa.fl_str_mv Grupo de Ingeniería y Gestión Ambiental (GIGA)
dc.subject.none.fl_str_mv Cimate variability
Climate model projection
Rainforests
topic Cimate variability
Climate model projection
Rainforests
description RESUMEN: We have observed that the dry-season length (DSL) has increased over southern Amazonia since 1979, primarily owing to a delay of its ending dates (dry-season end, DSE), and is accompanied by a prolonged fire season. A poleward shift of the subtropical jet over South America and an increase of local convective inhibition energy in austral winter (June–August) seem to cause the delay of the DSE in austral spring (September–November). These changes cannot be simply linked to the variability of the tropical Pacific and Atlantic Oceans. Although they show some resemblance to the effects of anthropogenic forcings reported in the literature, we cannot attribute them to this cause because of inadequate representation of these processes in the global climate models that were presented in the Intergovernmental Panel on Climate Change’s Fifth Assessment Report. These models significantly underestimate the variability of the DSE and DSL and their controlling processes. Such biases imply that the future change of the DSE and DSL may be underestimated by the climate projections provided by the Intergovernmental Panel on Climate Change’s Fifth Assessment Report models. Although it is not clear whether the observed increase of the DSL will continue in the future, were it to continue at half the rate of that observed, the long DSL and fire season that contributed to the 2005 drought would become the new norm by the late 21st century. The large uncertainty shown in this study highlights the need for a focused effort to better understand and simulate these changes over southern Amazonia.
publishDate 2013
dc.date.issued.none.fl_str_mv 2013
dc.date.accessioned.none.fl_str_mv 2017-07-13T22:38:12Z
dc.date.available.none.fl_str_mv 2017-07-13T22:38:12Z
dc.type.spa.fl_str_mv Artículo de investigación
dc.type.coar.spa.fl_str_mv http://purl.org/coar/resource_type/c_2df8fbb1
dc.type.redcol.spa.fl_str_mv https://purl.org/redcol/resource_type/ART
dc.type.coarversion.spa.fl_str_mv http://purl.org/coar/version/c_970fb48d4fbd8a85
dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/article
dc.type.version.spa.fl_str_mv info:eu-repo/semantics/publishedVersion
format http://purl.org/coar/resource_type/c_2df8fbb1
status_str publishedVersion
dc.identifier.citation.spa.fl_str_mv R. Fu et al., "Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection" Proceedings Of The National Academy Of Sciences Of The United States Of America, vol.110 fasc.45 p.18110 - 18115, 2013. DOI: 10.1073/pnas.1302584110
dc.identifier.issn.none.fl_str_mv 0027-8424
dc.identifier.uri.none.fl_str_mv http://hdl.handle.net/10495/7642
dc.identifier.doi.none.fl_str_mv 10.1073/pnas.1302584110
identifier_str_mv R. Fu et al., "Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection" Proceedings Of The National Academy Of Sciences Of The United States Of America, vol.110 fasc.45 p.18110 - 18115, 2013. DOI: 10.1073/pnas.1302584110
0027-8424
10.1073/pnas.1302584110
url http://hdl.handle.net/10495/7642
dc.language.iso.spa.fl_str_mv eng
language eng
dc.relation.ispartofjournalabbrev.spa.fl_str_mv Proceedings Of The National Academy Of Sciences Of The United States Of America
dc.relation.citationendpage.spa.fl_str_mv 18115
dc.relation.citationissue.spa.fl_str_mv 45
dc.relation.citationstartpage.spa.fl_str_mv 18110
dc.relation.citationvolume.spa.fl_str_mv 110
dc.relation.ispartofjournal.spa.fl_str_mv Proceedings Of The National Academy Of Sciences Of The United States Of America
dc.rights.uri.spa.fl_str_mv https://creativecommons.org/licenses/by-nc-nd/4.0/
dc.rights.uri.*.fl_str_mv http://creativecommons.org/licenses/by-nc-nd/2.5/co/
dc.rights.accessrights.*.fl_str_mv Atribución-NoComercial-SinDerivadas 2.5 Colombia
dc.rights.accessrights.spa.fl_str_mv info:eu-repo/semantics/openAccess
dc.rights.coar.spa.fl_str_mv http://purl.org/coar/access_right/c_abf2
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/4.0/
http://creativecommons.org/licenses/by-nc-nd/2.5/co/
Atribución-NoComercial-SinDerivadas 2.5 Colombia
http://purl.org/coar/access_right/c_abf2
eu_rights_str_mv openAccess
dc.format.extent.spa.fl_str_mv 5
dc.format.mimetype.spa.fl_str_mv application/pdf
dc.publisher.spa.fl_str_mv PNAS
dc.publisher.place.spa.fl_str_mv Estados Unidos
institution Universidad de Antioquia
bitstream.url.fl_str_mv https://bibliotecadigital.udea.edu.co/bitstreams/76bc9fc6-8699-4976-b26d-684fca624f89/download
https://bibliotecadigital.udea.edu.co/bitstreams/e8af265e-30a7-4334-89a5-801838a7c8e7/download
https://bibliotecadigital.udea.edu.co/bitstreams/05435a9d-23d0-4b7f-bd5b-082c5191e75b/download
https://bibliotecadigital.udea.edu.co/bitstreams/46e66c2b-7370-4099-a90c-3e08b49ef6d5/download
https://bibliotecadigital.udea.edu.co/bitstreams/f93f672a-d9d5-4934-9093-abea8c5ab009/download
https://bibliotecadigital.udea.edu.co/bitstreams/738b42d7-69c3-4b2a-a90b-2c5489b9fc06/download
https://bibliotecadigital.udea.edu.co/bitstreams/69bf1034-0177-4aba-ac69-802f2ea74cf6/download
bitstream.checksum.fl_str_mv 9b5590f044d2b3aaa41348615aebf2b6
4afdbb8c545fd630ea7db775da747b2f
d41d8cd98f00b204e9800998ecf8427e
d41d8cd98f00b204e9800998ecf8427e
8a4605be74aa9ea9d79846c1fba20a33
f7dfa2bf6cdb19aeb0ee7131e2f64e1f
1b73c5a994a5528975d47cdbf7541dc5
bitstream.checksumAlgorithm.fl_str_mv MD5
MD5
MD5
MD5
MD5
MD5
MD5
repository.name.fl_str_mv Repositorio Institucional de la Universidad de Antioquia
repository.mail.fl_str_mv aplicacionbibliotecadigitalbiblioteca@udea.edu.co
_version_ 1851052608607748096
spelling Yin, LeiLi, WenhongArias Gómez, Paola AndreaDickinson, Robert E.Huang, LeiChakraborty, SudipFernandes, KatiaLiebmann, BrantFisher, RosieMyneni, Ranga B.Grupo de Ingeniería y Gestión Ambiental (GIGA)2017-07-13T22:38:12Z2017-07-13T22:38:12Z2013R. Fu et al., "Increased dry-season length over southern Amazonia in recent decades and its implication for future climate projection" Proceedings Of The National Academy Of Sciences Of The United States Of America, vol.110 fasc.45 p.18110 - 18115, 2013. DOI: 10.1073/pnas.13025841100027-8424http://hdl.handle.net/10495/764210.1073/pnas.1302584110RESUMEN: We have observed that the dry-season length (DSL) has increased over southern Amazonia since 1979, primarily owing to a delay of its ending dates (dry-season end, DSE), and is accompanied by a prolonged fire season. A poleward shift of the subtropical jet over South America and an increase of local convective inhibition energy in austral winter (June–August) seem to cause the delay of the DSE in austral spring (September–November). These changes cannot be simply linked to the variability of the tropical Pacific and Atlantic Oceans. Although they show some resemblance to the effects of anthropogenic forcings reported in the literature, we cannot attribute them to this cause because of inadequate representation of these processes in the global climate models that were presented in the Intergovernmental Panel on Climate Change’s Fifth Assessment Report. These models significantly underestimate the variability of the DSE and DSL and their controlling processes. Such biases imply that the future change of the DSE and DSL may be underestimated by the climate projections provided by the Intergovernmental Panel on Climate Change’s Fifth Assessment Report models. Although it is not clear whether the observed increase of the DSL will continue in the future, were it to continue at half the rate of that observed, the long DSL and fire season that contributed to the 2005 drought would become the new norm by the late 21st century. The large uncertainty shown in this study highlights the need for a focused effort to better understand and simulate these changes over southern Amazonia.5application/pdfengPNASEstados Unidoshttps://creativecommons.org/licenses/by-nc-nd/4.0/http://creativecommons.org/licenses/by-nc-nd/2.5/co/Atribución-NoComercial-SinDerivadas 2.5 Colombiainfo:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Cimate variabilityClimate model projectionRainforestsIncreased dry-season length over southern Amazonia in recent decades and its implication for future climate projectionArtículo de investigaciónhttp://purl.org/coar/resource_type/c_2df8fbb1https://purl.org/redcol/resource_type/ARThttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionProceedings Of The National Academy Of Sciences Of The United States Of America181154518110110Proceedings Of The National Academy Of Sciences Of The United States Of AmericaPublicationORIGINALAriasPaola_2013_IncreasedDry-seasonLength.pdfAriasPaola_2013_IncreasedDry-seasonLength.pdfArtículo de investigaciónapplication/pdf855807https://bibliotecadigital.udea.edu.co/bitstreams/76bc9fc6-8699-4976-b26d-684fca624f89/download9b5590f044d2b3aaa41348615aebf2b6MD51trueAnonymousREADCC-LICENSElicense_urllicense_urltext/plain; charset=utf-849https://bibliotecadigital.udea.edu.co/bitstreams/e8af265e-30a7-4334-89a5-801838a7c8e7/download4afdbb8c545fd630ea7db775da747b2fMD52falseAnonymousREADlicense_textlicense_texttext/html; charset=utf-80https://bibliotecadigital.udea.edu.co/bitstreams/05435a9d-23d0-4b7f-bd5b-082c5191e75b/downloadd41d8cd98f00b204e9800998ecf8427eMD53falseAnonymousREADlicense_rdflicense_rdfapplication/rdf+xml; charset=utf-80https://bibliotecadigital.udea.edu.co/bitstreams/46e66c2b-7370-4099-a90c-3e08b49ef6d5/downloadd41d8cd98f00b204e9800998ecf8427eMD54falseAnonymousREADLICENSElicense.txtlicense.txttext/plain; charset=utf-81748https://bibliotecadigital.udea.edu.co/bitstreams/f93f672a-d9d5-4934-9093-abea8c5ab009/download8a4605be74aa9ea9d79846c1fba20a33MD55falseAnonymousREADTEXTAriasPaola_2013_IncreasedDry-seasonLength.pdf.txtAriasPaola_2013_IncreasedDry-seasonLength.pdf.txtExtracted texttext/plain53224https://bibliotecadigital.udea.edu.co/bitstreams/738b42d7-69c3-4b2a-a90b-2c5489b9fc06/downloadf7dfa2bf6cdb19aeb0ee7131e2f64e1fMD56falseAnonymousREADTHUMBNAILAriasPaola_2013_IncreasedDry-seasonLength.pdf.jpgAriasPaola_2013_IncreasedDry-seasonLength.pdf.jpgGenerated Thumbnailimage/jpeg20252https://bibliotecadigital.udea.edu.co/bitstreams/69bf1034-0177-4aba-ac69-802f2ea74cf6/download1b73c5a994a5528975d47cdbf7541dc5MD57falseAnonymousREAD10495/7642oai:bibliotecadigital.udea.edu.co:10495/76422025-03-27 00:59:59.323https://creativecommons.org/licenses/by-nc-nd/4.0/open.accesshttps://bibliotecadigital.udea.edu.coRepositorio Institucional de la Universidad de Antioquiaaplicacionbibliotecadigitalbiblioteca@udea.edu.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