U.S. Department of Energy Office of Biological and Environmental Research

PI-Submitted Research Highlights for
Terrestrial Ecosystem Science Program

A Direct Measure Of Basin-Wide Evaporation And Transpiration From The Amazon Rainforest

Charles Koven
Lawrence Berkeley National Laboratory

Highlight

23 June 2017

A water budget approach shows complex seasonal cycle and long-term changes in tropical forest function.

The Science   
The NGEE-Tropics research team combined satellite measurements of rainfall and gravity anomalies with Amazon river flow data to derive a seasonally-resolved estimate of evapotranspiration for the entire Amazon basin. Next the team analyzed the seasonal cycles and long-term variation of this measurement, and compare it to process-based land surface model predictions.

The Impact
The study's results show a more complex and different seasonal cycle than current land surface models predict. The study suggests a long-term decline in evapotranspiration from the forest, due to ecosystem functional change at the scale of the entire basin.

Summary
Evapotranspiration, which comprises the sum of all moisture fluxes from an ecosystem directly to the atmosphere, is a crucial quantity at the center of the terrestrial energy, water, and carbon cycles. Because measurements of evapotranspiration are typically made at local scales, and are sparse over remote locations such as the Amazon, the larger-scale fluxes are not well known.  This study combined observations of rainfall, river discharge, and time-varying gravity anomalies to construct a water budget for the Amazon basin, which allows the NGEE-Tropics researchers to solve for evapotranspiration as the missing term in the budget. This water budget-based measurement shows a complex seasonal cycle, with a deeper minimum during the wet season than is estimated by other upscaling estimates or by process-based models, and also shows that models tend to increase their seasonal evapotranspiration fluxes later in the dry season than is observed. Furthermore, a long-term analysis of evapotranspiration suggests a decline in the rate over the period of observation, which could be evidence of a large-scale change in ecosystem function.

Contacts (BER PM)
Daniel Stover, Dorothy Koch, Renu Joseph
SC-23.1
Daniel.Stover@science.doe.gov (301-903-0289)
dorothy.koch@science.doe.gov (301-903-0105)
Renu.Joseph@science.doe.gov  (301-903-9237)

(PI Contact)
Charles Koven
Lawrence Berkeley National Lab
cdkoven@lbl.gov, 510.486.6724

Funding
ALSS was supported by National Science Foundation grants AGS-1321745 and AGS-1553715. CDK received support from the Regional and Global Climate Modeling program through the BGC-Feedbacks SFA and the Terrestrial Ecosystem Sciences and Earth System Modeling programs through the Next Generation Ecosystem Experiments-Tropics (NGEE-Tropics) project of the Biological and Environmental Research (BER) Program in the U. S. Dept. of Energy Office of Science.

Publications
Swann, A. L. S., and Koven , C. D. A direct estimate of the seasonal cycle of evapotranspiration over the Amazon. Journal of Hydrometeorology (2017) doi:10.1175/JHM-D-17-0004.1 (Reference link)

C. Koven, LBNL, under funding from NGEE-Tropics and BGC-Feedbacks SFA. 

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