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Vegetation dynamics and rainfall sensitivity of the Amazon

Vegetation dynamics and rainfall sensitivity of the Amazon
Vegetation dynamics and rainfall sensitivity of the Amazon
We show that the vegetation canopy of the Amazon rainforest is highly sensitive to changes in precipitation patterns and that reduction in rainfall since 2000 has diminished vegetation greenness across large parts of Amazonia. Large-scale directional declines in vegetation greenness may indicate decreases in carbon uptake and substantial changes in the energy balance of the Amazon. We use improved estimates of surface reflectance from satellite data to show a close link between reductions in annual precipitation, El Niño southern oscillation events, and photosynthetic activity across tropical and subtropical Amazonia. We report that, since the year 2000, precipitation has declined across 69% of the tropical evergreen forest (5.4 million km2) and across 80% of the subtropical grasslands (3.3 million km2). These reductions, which coincided with a decline in terrestrial water storage, account for about 55% of a satellite-observed widespread decline in the normalized difference vegetation index (NDVI). During El Niño events, NDVI was reduced about 16.6% across an area of up to 1.6 million km2 compared with average conditions. Several global circulation models suggest that a rise in equatorial sea surface temperature and related displacement of the intertropical convergence zone could lead to considerable drying of tropical forests in the 21st century. Our results provide evidence that persistent drying could degrade Amazonian forest canopies, which would have cascading effects on global carbon and climate dynamics.
amazon, climate change, precipitation, NDVI, MODIS, MAIAC
0027-8424
16041-16046
Hilker, T.
c7fb75b8-320d-49df-84ba-96c9ee523d40
Lyapustin, A. I.
f24c1dee-b9df-4fc8-9998-60b2952d170c
Tucker, C. J.
0b1e58a1-4474-4b41-b8ba-8fc07d8a70a9
Hall, F. G.
795160e6-8ce3-4250-9040-036a3b0f8ad9
Myneni, R. B.
e6f37c8d-39ef-4d3a-996d-c423a34d5971
Wang, Y.
23c775f0-3cac-44d5-9e16-2098959c493b
Bi, J.
5cad4178-6c9d-4897-ad4a-9d6b07a12acf
Mendes de Moura, Y.
2f7ec997-7172-41a7-b64c-e219d905ca4a
Sellers, P. J.
95aaa8ff-c365-4e3e-b51c-76428658bfe3
Hilker, T.
c7fb75b8-320d-49df-84ba-96c9ee523d40
Lyapustin, A. I.
f24c1dee-b9df-4fc8-9998-60b2952d170c
Tucker, C. J.
0b1e58a1-4474-4b41-b8ba-8fc07d8a70a9
Hall, F. G.
795160e6-8ce3-4250-9040-036a3b0f8ad9
Myneni, R. B.
e6f37c8d-39ef-4d3a-996d-c423a34d5971
Wang, Y.
23c775f0-3cac-44d5-9e16-2098959c493b
Bi, J.
5cad4178-6c9d-4897-ad4a-9d6b07a12acf
Mendes de Moura, Y.
2f7ec997-7172-41a7-b64c-e219d905ca4a
Sellers, P. J.
95aaa8ff-c365-4e3e-b51c-76428658bfe3

Hilker, T., Lyapustin, A. I., Tucker, C. J., Hall, F. G., Myneni, R. B., Wang, Y., Bi, J., Mendes de Moura, Y. and Sellers, P. J. (2014) Vegetation dynamics and rainfall sensitivity of the Amazon. Proceedings of the National Academy of Sciences, 111 (45), 16041-16046. (doi:10.1073/pnas.1404870111). (PMID:25349419)

Record type: Article

Abstract

We show that the vegetation canopy of the Amazon rainforest is highly sensitive to changes in precipitation patterns and that reduction in rainfall since 2000 has diminished vegetation greenness across large parts of Amazonia. Large-scale directional declines in vegetation greenness may indicate decreases in carbon uptake and substantial changes in the energy balance of the Amazon. We use improved estimates of surface reflectance from satellite data to show a close link between reductions in annual precipitation, El Niño southern oscillation events, and photosynthetic activity across tropical and subtropical Amazonia. We report that, since the year 2000, precipitation has declined across 69% of the tropical evergreen forest (5.4 million km2) and across 80% of the subtropical grasslands (3.3 million km2). These reductions, which coincided with a decline in terrestrial water storage, account for about 55% of a satellite-observed widespread decline in the normalized difference vegetation index (NDVI). During El Niño events, NDVI was reduced about 16.6% across an area of up to 1.6 million km2 compared with average conditions. Several global circulation models suggest that a rise in equatorial sea surface temperature and related displacement of the intertropical convergence zone could lead to considerable drying of tropical forests in the 21st century. Our results provide evidence that persistent drying could degrade Amazonian forest canopies, which would have cascading effects on global carbon and climate dynamics.

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More information

e-pub ahead of print date: 27 October 2014
Published date: 11 November 2014
Keywords: amazon, climate change, precipitation, NDVI, MODIS, MAIAC
Organisations: Geography & Environment

Identifiers

Local EPrints ID: 384681
URI: http://eprints.soton.ac.uk/id/eprint/384681
ISSN: 0027-8424
PURE UUID: 915995f0-0675-4402-99ca-20f31d23ef4e

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Date deposited: 13 Jan 2016 08:56
Last modified: 14 Mar 2024 22:02

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Contributors

Author: T. Hilker
Author: A. I. Lyapustin
Author: C. J. Tucker
Author: F. G. Hall
Author: R. B. Myneni
Author: Y. Wang
Author: J. Bi
Author: Y. Mendes de Moura
Author: P. J. Sellers

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