Closing the scale gap between land surface parameterizations and GCMs with a new scheme, SiB3Bins: SOIL MOISTURE SCALE GAP
The interaction of land with the atmosphere is sensitive to soil moisture (W). Evapotranspiration (ET) reacts to soil moisture in a nonlinear way, f(W), as soils dry from saturation to wilt point. This nonlinear behavior and the fact that soil moisture varies on scales as small as 1–10 m in nature, while numerical general circulation models (GCMs) have grid cell sizes on the order of 1 to 100s of kilometers, makes the calculation of grid cellaverage ET problematic. It is impractical to simulate the land in GCMs on the small scales seen in nature, so techniques have been developed to represent subgrid scale heterogeneity, including: (1) statisticaldynamical representations of grid subelements of varying wetness, (2) relaxation of f(W), (3) moderating f(W) with approximations of catchment hydrology, (4) “tiling” the landscape into vegetation types, and (5) hyperresolution. Here we present an alternative method for representing subgrid variability in W, one proven in a conceptual framework where landscapescale W is represented as a series of “Bins” of increasing wetness from dry to saturated. The grid celllevel f(W) is defined by the integral of the fractional area of the wetness bins and the value of f(W) associated with each. This approach accounts formore »
 Authors:

^{[1]}
;
^{[2]}
;
^{[1]};
^{[1]}
;
^{[1]};
^{[1]}
;
^{[3]}
 Colorado State Univ., Fort Collins, CO (United States)
 NASA Goddard Space Flight Center (GSFC), Greenbelt, MD (United States)
 Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
 Publication Date:
 Grant/Contract Number:
 AC0205CH11231
 Type:
 Accepted Manuscript
 Journal Name:
 Journal of Advances in Modeling Earth Systems
 Additional Journal Information:
 Journal Volume: 9; Journal Issue: 1; Journal ID: ISSN 19422466
 Publisher:
 American Geophysical Union (AGU)
 Research Org:
 Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
 Sponsoring Org:
 USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC23)
 Country of Publication:
 United States
 Language:
 English
 Subject:
 54 ENVIRONMENTAL SCIENCES
 OSTI Identifier:
 1408418
Baker, I. T., Sellers, P. J., Denning, A. S., Medina, I., Kraus, P., Haynes, K. D., and Biraud, S. C.. Closing the scale gap between land surface parameterizations and GCMs with a new scheme, SiB3Bins: SOIL MOISTURE SCALE GAP. United States: N. p.,
Web. doi:10.1002/2016MS000764.
Baker, I. T., Sellers, P. J., Denning, A. S., Medina, I., Kraus, P., Haynes, K. D., & Biraud, S. C.. Closing the scale gap between land surface parameterizations and GCMs with a new scheme, SiB3Bins: SOIL MOISTURE SCALE GAP. United States. doi:10.1002/2016MS000764.
Baker, I. T., Sellers, P. J., Denning, A. S., Medina, I., Kraus, P., Haynes, K. D., and Biraud, S. C.. 2017.
"Closing the scale gap between land surface parameterizations and GCMs with a new scheme, SiB3Bins: SOIL MOISTURE SCALE GAP". United States.
doi:10.1002/2016MS000764. https://www.osti.gov/servlets/purl/1408418.
@article{osti_1408418,
title = {Closing the scale gap between land surface parameterizations and GCMs with a new scheme, SiB3Bins: SOIL MOISTURE SCALE GAP},
author = {Baker, I. T. and Sellers, P. J. and Denning, A. S. and Medina, I. and Kraus, P. and Haynes, K. D. and Biraud, S. C.},
abstractNote = {The interaction of land with the atmosphere is sensitive to soil moisture (W). Evapotranspiration (ET) reacts to soil moisture in a nonlinear way, f(W), as soils dry from saturation to wilt point. This nonlinear behavior and the fact that soil moisture varies on scales as small as 1–10 m in nature, while numerical general circulation models (GCMs) have grid cell sizes on the order of 1 to 100s of kilometers, makes the calculation of grid cellaverage ET problematic. It is impractical to simulate the land in GCMs on the small scales seen in nature, so techniques have been developed to represent subgrid scale heterogeneity, including: (1) statisticaldynamical representations of grid subelements of varying wetness, (2) relaxation of f(W), (3) moderating f(W) with approximations of catchment hydrology, (4) “tiling” the landscape into vegetation types, and (5) hyperresolution. Here we present an alternative method for representing subgrid variability in W, one proven in a conceptual framework where landscapescale W is represented as a series of “Bins” of increasing wetness from dry to saturated. The grid celllevel f(W) is defined by the integral of the fractional area of the wetness bins and the value of f(W) associated with each. This approach accounts for the spatiotemporal dynamics of W. We implemented this approach in the SiB3 land surface parameterization and then evaluated its performance against a control, which assumes a horizontally uniform field of W. We demonstrate that the Bins method, with a physical basis, attenuates unrealistic jumps in model state and ET seen in the control runs.},
doi = {10.1002/2016MS000764},
journal = {Journal of Advances in Modeling Earth Systems},
number = 1,
volume = 9,
place = {United States},
year = {2017},
month = {3}
}