Artigo

Teleconnection between tree growth in the Amazonian floodplains and the El Niño-Southern Oscillation effect

There is a limited knowledge about the El Niño-Southern Oscillation (ENSO) effects on the Amazon basin, the world's largest tropical rain forest and a major factor in the global carbon cycle. Seasonal precipitation in the Andean watershed annually causes a several month-long inundation of the floodp...

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Autor principal: Schöngart, Jochen
Outros Autores: Junk, Wolfgang Johannes, Piedade, Maria Teresa Fernandez, Ayres, José Marcio, Hüttermann, Alloys, Worbes, Martin
Grau: Artigo
Idioma: English
Publicado em: Global Change Biology 2020
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Acesso em linha: https://repositorio.inpa.gov.br/handle/1/18923
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spelling oai:repositorio:1-18923 Teleconnection between tree growth in the Amazonian floodplains and the El Niño-Southern Oscillation effect Schöngart, Jochen Junk, Wolfgang Johannes Piedade, Maria Teresa Fernandez Ayres, José Marcio Hüttermann, Alloys Worbes, Martin Carbon Cycle Dendrochronology El Nino-southern Oscillation Growth Response Paleoclimate Seasonal Variation Tropical Forest Amazonia South America Euphorbia Euphorbiaceae There is a limited knowledge about the El Niño-Southern Oscillation (ENSO) effects on the Amazon basin, the world's largest tropical rain forest and a major factor in the global carbon cycle. Seasonal precipitation in the Andean watershed annually causes a several month-long inundation of the floodplains along the Amazon River that induces the formation of annual rings in trees of the flooded forests. Radial growth of trees is mainly restricted to the nonflooded period and thus the ring width corresponds to its duration. This allows the construction of a tree-ring chronology of the long-living hardwood species Piranhea trifoliata Baill. (Euphorbiaceae). El Niño causes anomalously low precipitation in the catchment that results in a significantly lower water discharge of the Amazon River and consequently in an extension of the vegetation period. In those years tree rings are significantly wider. Thus the tree-ring record can be considered as a robust indicator reflecting the mean climate conditions of the whole Western Amazon basin. We present a more than 200-year long chronology, which is the first ENSO-sensitive dendroclimatic proxy of the Amazon basin and permits the dating of preinstrumental El Niño events. Time series analyses of our data indicate that during the last two centuries the severity of El Niño increased significantly. © 2004 Blackwell Publishing Ltd. 2020-06-15T22:03:57Z 2020-06-15T22:03:57Z 2004 Artigo https://repositorio.inpa.gov.br/handle/1/18923 10.1111/j.1529-8817.2003.00754.x en Volume 10, Número 5, Pags. 683-692 Restrito Global Change Biology
institution Instituto Nacional de Pesquisas da Amazônia - Repositório Institucional
collection INPA-RI
language English
topic Carbon Cycle
Dendrochronology
El Nino-southern Oscillation
Growth Response
Paleoclimate
Seasonal Variation
Tropical Forest
Amazonia
South America
Euphorbia
Euphorbiaceae
spellingShingle Carbon Cycle
Dendrochronology
El Nino-southern Oscillation
Growth Response
Paleoclimate
Seasonal Variation
Tropical Forest
Amazonia
South America
Euphorbia
Euphorbiaceae
Schöngart, Jochen
Teleconnection between tree growth in the Amazonian floodplains and the El Niño-Southern Oscillation effect
topic_facet Carbon Cycle
Dendrochronology
El Nino-southern Oscillation
Growth Response
Paleoclimate
Seasonal Variation
Tropical Forest
Amazonia
South America
Euphorbia
Euphorbiaceae
description There is a limited knowledge about the El Niño-Southern Oscillation (ENSO) effects on the Amazon basin, the world's largest tropical rain forest and a major factor in the global carbon cycle. Seasonal precipitation in the Andean watershed annually causes a several month-long inundation of the floodplains along the Amazon River that induces the formation of annual rings in trees of the flooded forests. Radial growth of trees is mainly restricted to the nonflooded period and thus the ring width corresponds to its duration. This allows the construction of a tree-ring chronology of the long-living hardwood species Piranhea trifoliata Baill. (Euphorbiaceae). El Niño causes anomalously low precipitation in the catchment that results in a significantly lower water discharge of the Amazon River and consequently in an extension of the vegetation period. In those years tree rings are significantly wider. Thus the tree-ring record can be considered as a robust indicator reflecting the mean climate conditions of the whole Western Amazon basin. We present a more than 200-year long chronology, which is the first ENSO-sensitive dendroclimatic proxy of the Amazon basin and permits the dating of preinstrumental El Niño events. Time series analyses of our data indicate that during the last two centuries the severity of El Niño increased significantly. © 2004 Blackwell Publishing Ltd.
format Artigo
author Schöngart, Jochen
author2 Junk, Wolfgang Johannes
Piedade, Maria Teresa Fernandez
Ayres, José Marcio
Hüttermann, Alloys
Worbes, Martin
author2Str Junk, Wolfgang Johannes
Piedade, Maria Teresa Fernandez
Ayres, José Marcio
Hüttermann, Alloys
Worbes, Martin
title Teleconnection between tree growth in the Amazonian floodplains and the El Niño-Southern Oscillation effect
title_short Teleconnection between tree growth in the Amazonian floodplains and the El Niño-Southern Oscillation effect
title_full Teleconnection between tree growth in the Amazonian floodplains and the El Niño-Southern Oscillation effect
title_fullStr Teleconnection between tree growth in the Amazonian floodplains and the El Niño-Southern Oscillation effect
title_full_unstemmed Teleconnection between tree growth in the Amazonian floodplains and the El Niño-Southern Oscillation effect
title_sort teleconnection between tree growth in the amazonian floodplains and the el niño-southern oscillation effect
publisher Global Change Biology
publishDate 2020
url https://repositorio.inpa.gov.br/handle/1/18923
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score 11.674684