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PI-Submitted Research Highlights for
Subsurface Biogeochemical Research Program

Reconciling Observations and Global Models of Terrestrial Water Fluxes

Reed Maxwell


July 22, 2016

Water table depth and groundwater flow are key to understanding the amount of water that plants transmit to the atmosphere.

The Science
Plants are one of the largest water users on land and, through transpiration, they move more water into the atmosphere than streams or rivers move across the landscape. Unlike stream flow, which can be easily observed, measuring and simulating the amount of water plants transmit to the atmosphere are significant challenges.  A new modeling study using high performance computers (HPC) shows that lateral groundwater flow, not included in previous approaches, may be the missing link to predicting how important plant water use is to the total system.

The Impact
The relative importance of plant transpiration remains one of the largest uncertainties in balancing water at continental scales. Improving the large-scale simulation of plant transpiration will enable scientists to better predict hydrologic response and manage water resources, as well as predict and understand how much freshwater is available globally.

Using integrated hydrologic simulations that couple vegetation and land-energy processes with surface and subsurface hydrology, the researchers studied the relative importance of transpiration as a fraction of all the water moving from the land surface to the atmosphere (commonly referred to as transpiration partitioning) at the continental scale. They found that both the total flux of water and transpiration partitioning are connected to water table depth. Because of this connection, including groundwater flow in the model increases transpiration partitioning from 47% (±13%) to 62% (±12%). This finding suggests that groundwater flow, which is generally simplified or excluded from other continental-scale simulations, may provide a missing link to reconciling observations and global models of terrestrial water fluxes.

BER Program Managers
David Lesmes, SC-23.1, 301-903-2977
Paul Bayer, SC-23.1, 301-903-5324

Principal Investigators
Reed Maxwell
Colorado School of Mines

Laura Condon
Syracuse University

This work was supported by the Office of Biological and Environmental Research (BER), within the U.S. Department of Energy (DOE) Office of Science, and the Interoperable Design of Extreme-scale Application Software (IDEAS) project of the Office of Advanced Scientific Computing Research (ASCR), within the DOE Office of Science. Simulations were made possible through support from Yellowstone at the National Center for Atmospheric Research Computational and Information Systems Laboratory.

Maxwell, R. M., and L. E. Condon. “Connections between groundwater flow and transpiration partitioning.” Science 353(6297), 377–80 (2016). [DOI: 10.1126/science.aaf7891]

Related Links
Reference link


R. M. Maxwell, L. E. Condon, "Connections Between Groundwater Flow and Transpiration Partitioning." Science (2016). DOI: 10.1126/science.aaf7891

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