A global analysis of the impact of drought on net primary productivity

We investigated the impact of drought on interannual variability of net primary productivity (NPP) from 1997 to 2009, using the standardized precipitation evapotranspiration index (SPEI) drought index and satellite-derived vegetation greenness converted to NPP. SPEI is positive for wet conditions an...

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Main Authors: T. Chen, G. R. Werf, R. A. M. Jeu, G. Wang, A. J. Dolman
Format: Article
Language:English
Published: Copernicus Publications 2013-10-01
Series:Hydrology and Earth System Sciences
Online Access:http://www.hydrol-earth-syst-sci.net/17/3885/2013/hess-17-3885-2013.pdf
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spelling doaj-dec25b87d79c445e92b0c5206c5399192020-11-25T02:47:38ZengCopernicus PublicationsHydrology and Earth System Sciences1027-56061607-79382013-10-0117103885389410.5194/hess-17-3885-2013A global analysis of the impact of drought on net primary productivityT. ChenG. R. WerfR. A. M. JeuG. WangA. J. DolmanWe investigated the impact of drought on interannual variability of net primary productivity (NPP) from 1997 to 2009, using the standardized precipitation evapotranspiration index (SPEI) drought index and satellite-derived vegetation greenness converted to NPP. SPEI is positive for wet conditions and negative for dry conditions. We found that SPEI and NPP were coupled and showed in-phase behaviour on a global scale. We then used the Köppen climate classification to study the SPEI–NPP relations regionally and found that while NPP and SPEI were positively related (high SPEI, high NPP) in arid and in seasonal dry regions, the opposite occurs in most boreal regions (high SPEI, low NPP). High intensity drought events, such as the 2003 drought in Europe were picked up by our analysis. Our findings suggest that the strong positive relation between global average moisture availability and NPP consists of a composite of the positive relation across dry regions and the coherent NPP decline during and after intensive drought events in humid regions. Importantly, we also found that there are many areas on the globe that show no strong correlation between drought and NPP.http://www.hydrol-earth-syst-sci.net/17/3885/2013/hess-17-3885-2013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author T. Chen
G. R. Werf
R. A. M. Jeu
G. Wang
A. J. Dolman
spellingShingle T. Chen
G. R. Werf
R. A. M. Jeu
G. Wang
A. J. Dolman
A global analysis of the impact of drought on net primary productivity
Hydrology and Earth System Sciences
author_facet T. Chen
G. R. Werf
R. A. M. Jeu
G. Wang
A. J. Dolman
author_sort T. Chen
title A global analysis of the impact of drought on net primary productivity
title_short A global analysis of the impact of drought on net primary productivity
title_full A global analysis of the impact of drought on net primary productivity
title_fullStr A global analysis of the impact of drought on net primary productivity
title_full_unstemmed A global analysis of the impact of drought on net primary productivity
title_sort global analysis of the impact of drought on net primary productivity
publisher Copernicus Publications
series Hydrology and Earth System Sciences
issn 1027-5606
1607-7938
publishDate 2013-10-01
description We investigated the impact of drought on interannual variability of net primary productivity (NPP) from 1997 to 2009, using the standardized precipitation evapotranspiration index (SPEI) drought index and satellite-derived vegetation greenness converted to NPP. SPEI is positive for wet conditions and negative for dry conditions. We found that SPEI and NPP were coupled and showed in-phase behaviour on a global scale. We then used the Köppen climate classification to study the SPEI–NPP relations regionally and found that while NPP and SPEI were positively related (high SPEI, high NPP) in arid and in seasonal dry regions, the opposite occurs in most boreal regions (high SPEI, low NPP). High intensity drought events, such as the 2003 drought in Europe were picked up by our analysis. Our findings suggest that the strong positive relation between global average moisture availability and NPP consists of a composite of the positive relation across dry regions and the coherent NPP decline during and after intensive drought events in humid regions. Importantly, we also found that there are many areas on the globe that show no strong correlation between drought and NPP.
url http://www.hydrol-earth-syst-sci.net/17/3885/2013/hess-17-3885-2013.pdf
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