4.8 Article

Seasonal responses of terrestrial ecosystem water-use efficiency to climate change

Journal

GLOBAL CHANGE BIOLOGY
Volume 22, Issue 6, Pages 2165-2177

Publisher

WILEY
DOI: 10.1111/gcb.13180

Keywords

climate change; CO2 enrichment; process-based model; seasonal variation; terrestrial ecosystem; water-use efficiency

Funding

  1. National Basic Research Program of China [2013CB956303]
  2. National Natural Science Foundation of China [41530528]
  3. 111 Project [B14001]
  4. National Youth Top-notch Talent Support Program in China
  5. US Department of Energy (DOE), Office of Science, Biological and Environmental Research
  6. DOE [DE-AC05-000R22725]
  7. US Department of Energy (DOE), Office of Science, Biological and Environmental Research, Oak Ridge National Laboratory [DE-AC05-000R22725]
  8. CFCAS
  9. NSERC
  10. BIOCAP
  11. Environment Canada
  12. NRCan
  13. CarboEuropeIP
  14. FAO-GTOS-TCO
  15. iLEAPS
  16. Max Planck Institute for Biogeochemistry
  17. National Science Foundation
  18. University of Tuscia
  19. Universite Laval
  20. US Department of Energy

Ask authors/readers for more resources

Ecosystem water-use efficiency (EWUE) is an indicator of carbon-water interactions and is defined as the ratio of carbon assimilation (GPP) to evapotranspiration (ET). Previous research suggests an increasing long-term trend in annual EWUE over many regions and is largely attributed to the physiological effects of rising CO2. The seasonal trends in EWUE, however, have not yet been analyzed. In this study, we investigate seasonal EWUE trends and responses to various drivers during 1982-2008. The seasonal cycle for two variants of EWUE, water-use efficiency (WUE, GPP/ET), and transpiration-based WUE (WUEt, the ratio of GPP and transpiration), is analyzed from 0.5 degrees gridded fields from four process-based models and satellite-based products, as well as a network of 63 local flux tower observations. WUE derived from flux tower observations shows moderate seasonal variation for most latitude bands, which is in agreement with satellite-based products. In contrast, the seasonal EWUE trends are not well captured by the same satellite-based products. Trend analysis, based on process-model factorial simulations separating effects of climate, CO2, and nitrogen deposition (NDEP), further suggests that the seasonal EWUE trends are mainly associated with seasonal trends of climate, whereas CO2 and NDEP do not show obvious seasonal difference in EWUE trends. About 66% grid cells show positive annual WUE trends, mainly over mid-and high northern latitudes. In these regions, spring climate change has amplified the effect of CO2 in increasing WUE by more than 0.005 gC m(-2) mm(-1) yr(-1) for 41% pixels. Multiple regression analysis further shows that the increase in springtime WUE in the northern hemisphere is the result of GPP increasing faster than ET because of the higher temperature sensitivity of GPP relative to ET. The partitioning of annual EWUE to seasonal components provides new insight into the relative sensitivities of GPP and ET to climate, CO2, and NDEP.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.8
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available