ENSO Drives interannual variation of forest woody growth across the tropics

dc.contributor.authorSami W. Rifai
dc.contributor.authorCécile Girardin
dc.contributor.authorÉrika Berenguer
dc.contributor.authorJhon del Águila Pasquel
dc.contributor.authorCecilia A. L. Dahlsjö
dc.contributor.authorChristopher E. Doughty
dc.contributor.authorKathryn J. Jeffery
dc.contributor.authorSam Moore
dc.contributor.authorImma Oliveras Menor
dc.contributor.authorTerhi Riutta
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T14:04:01Z
dc.date.available2026-03-22T14:04:01Z
dc.date.issued2018
dc.descriptionCitaciones: 74
dc.description.abstractMeteorological extreme events such as El Niño events are expected to affect tropical forest net primary production (NPP) and woody growth, but there has been no large-scale empirical validation of this expectation. We collected a large high-temporal resolution dataset (for 1-13 years depending upon location) of more than 172 000 stem growth measurements using dendrometer bands from across 14 regions spanning Amazonia, Africa and Borneo in order to test how much month-to-month variation in stand-level woody growth of adult tree stems (NPP<sub>stem</sub>) can be explained by seasonal variation and interannual meteorological anomalies. A key finding is that woody growth responds differently to meteorological variation between tropical forests with a dry season (where monthly rainfall is less than 100 mm), and aseasonal wet forests lacking a consistent dry season. In seasonal tropical forests, a high degree of variation in woody growth can be predicted from seasonal variation in temperature, vapour pressure deficit, in addition to anomalies of soil water deficit and shortwave radiation. The variation of aseasonal wet forest woody growth is best predicted by the anomalies of vapour pressure deficit, water deficit and shortwave radiation. In total, we predict the total live woody production of the global tropical forest biome to be 2.16 Pg C yr<sup>-1</sup>, with an interannual range 1.96-2.26 Pg C yr<sup>-1</sup> between 1996-2016, and with the sharpest declines during the strong El Niño events of 1997/8 and 2015/6. There is high geographical variation in hotspots of El Niño-associated impacts, with weak impacts in Africa, and strongly negative impacts in parts of Southeast Asia and extensive regions across central and eastern Amazonia. Overall, there is high correlation (<i>r</i> = -0.75) between the annual anomaly of tropical forest woody growth and the annual mean of the El Niño 3.4 index, driven mainly by strong correlations with anomalies of soil water deficit, vapour pressure deficit and shortwave radiation.This article is part of the discussion meeting issue 'The impact of the 2015/2016 El Niño on the terrestrial tropical carbon cycle: patterns, mechanisms and implications'.
dc.identifier.doi10.1098/rstb.2017.0410
dc.identifier.urihttps://doi.org/10.1098/rstb.2017.0410
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/44343
dc.language.isoen
dc.publisherRoyal Society
dc.relation.ispartofPhilosophical Transactions of the Royal Society B Biological Sciences
dc.sourceUniversity of Oxford
dc.subjectVapour Pressure Deficit
dc.subjectEnvironmental science
dc.subjectTropics
dc.subjectBiome
dc.subjectSubtropics
dc.subjectPrimary production
dc.subjectTropical and subtropical dry broadleaf forests
dc.subjectSeasonality
dc.subjectAtmospheric sciences
dc.subjectDry season
dc.titleENSO Drives interannual variation of forest woody growth across the tropics
dc.typearticle

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