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...
- 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/
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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. |
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2013 |
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2013 |
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2017-07-13T22:38:12Z |
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2017-07-13T22:38:12Z |
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Artículo de investigación |
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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 |
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0027-8424 |
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http://hdl.handle.net/10495/7642 |
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10.1073/pnas.1302584110 |
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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 |
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eng |
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eng |
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Proceedings Of The National Academy Of Sciences Of The United States Of America |
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18115 |
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45 |
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18110 |
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110 |
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Proceedings Of The National Academy Of Sciences Of The United States Of America |
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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. 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