skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: How well do terrestrial biosphere models simulate coarse-scale runoff in the contiguous United States?

Abstract

Significant changes in the water cycle are expected under current global environmental change. Robust assessment of present-day water cycle dynamics at continental to global scales is confounded by shortcomings in the observed record. Modeled assessments also yield conflicting results which are linked to differences in model structure and simulation protocol. Here we compare simulated gridded (1 spatial resolution) runoff from six terrestrial biosphere models (TBMs), seven reanalysis products, and one gridded surface station product in the contiguous United States (CONUS) from 2001 to 2005. We evaluate the consistency of these 14 estimates with stream gauge data, both as depleted flow and corrected for net withdrawals (2005 only), at the CONUS and water resource region scale, as well as examining similarity across TBMs and reanalysis products at the grid cell scale. Mean runoff across all simulated products and regions varies widely (range: 71 to 356 mm yr(-1)) relative to observed continental-scale runoff (209 or 280 mm yr(-1) when corrected for net withdrawals). Across all 14 products 8 exhibit Nash-Sutcliffe efficiency values in excess of 0.8 and three are within 10% of the observed value. Region-level mismatch exhibits a weak pattern of overestimation in western and underestimation in eastern regions although twomore » products are systematically biased across all regions and largely scales with water use. Although gridded composite TBM and reanalysis runoff show some regional similarities, individual product values are highly variable. At the coarse scales used here we find that progress in better constraining simulated runoff requires standardized forcing data and the explicit incorporation of human effects (e.g., water withdrawals by source, fire, and land use change). (C) 2015 Elsevier B.V. All rights reserved.« less

Authors:
 [1];  [1];  [2];  [2];  [3];  [4];  [5];  [6];  [6];  [7];  [8]
  1. Northern Arizona Univ., Flagstaff, AZ (United States)
  2. Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
  3. Univ. of Colorado, Boulder, CO (United States)
  4. United States Department of Agriculture (USDA) Forest Service, Portland, OR (United States). Pacific Northwest Research Station
  5. Montana State Univ., Bozeman, MT (United States)
  6. United States Department of Agriculture (USDA) Forest Service, Knoxville, TN (United States). Southern Research Station
  7. Auburn Univ., AL (United States)
  8. Univ. of Maryland, College Park, MD (United States)
Publication Date:
Research Org.:
Oak Ridge National Lab. (ORNL), Oak Ridge, TN (United States)
Sponsoring Org.:
USDOE Office of Science (SC), Biological and Environmental Research (BER) (SC-23)
OSTI Identifier:
1335319
Alternate Identifier(s):
OSTI ID: 1249857
Grant/Contract Number:
AC05-00OR22725; FG02-06ER64317; MTU050516Z14
Resource Type:
Journal Article: Accepted Manuscript
Journal Name:
Ecological Modelling
Additional Journal Information:
Journal Volume: 303; Journal ID: ISSN 0304-3800
Publisher:
Elsevier
Country of Publication:
United States
Language:
English
Subject:
54 ENVIRONMENTAL SCIENCES; Terrestrial biosphere models; Runoff; Intercomparison; North American Carbon Program; Regional; AMERICAN REGIONAL REANALYSIS; GLOBAL VEGETATION MODEL; FRESH-WATER DISCHARGE; INTERANNUAL VARIABILITY; CIRCULATION MODEL; BALANCE; PRECIPITATION; CLIMATE; OCEAN

Citation Formats

Schwalm, C., Huntzinger, Deborah N., Cook, Robert B., Wei, Yaxing, Baker, I. T., Neilson, R. P., Poulter, B., Caldwell, Peter, Sun, G., Tian, H. Q., and Zeng, N.. How well do terrestrial biosphere models simulate coarse-scale runoff in the contiguous United States?. United States: N. p., 2015. Web. doi:10.1016/j.ecolmodel.2015.02.006.
Schwalm, C., Huntzinger, Deborah N., Cook, Robert B., Wei, Yaxing, Baker, I. T., Neilson, R. P., Poulter, B., Caldwell, Peter, Sun, G., Tian, H. Q., & Zeng, N.. How well do terrestrial biosphere models simulate coarse-scale runoff in the contiguous United States?. United States. doi:10.1016/j.ecolmodel.2015.02.006.
Schwalm, C., Huntzinger, Deborah N., Cook, Robert B., Wei, Yaxing, Baker, I. T., Neilson, R. P., Poulter, B., Caldwell, Peter, Sun, G., Tian, H. Q., and Zeng, N.. Wed . "How well do terrestrial biosphere models simulate coarse-scale runoff in the contiguous United States?". United States. doi:10.1016/j.ecolmodel.2015.02.006. https://www.osti.gov/servlets/purl/1335319.
@article{osti_1335319,
title = {How well do terrestrial biosphere models simulate coarse-scale runoff in the contiguous United States?},
author = {Schwalm, C. and Huntzinger, Deborah N. and Cook, Robert B. and Wei, Yaxing and Baker, I. T. and Neilson, R. P. and Poulter, B. and Caldwell, Peter and Sun, G. and Tian, H. Q. and Zeng, N.},
abstractNote = {Significant changes in the water cycle are expected under current global environmental change. Robust assessment of present-day water cycle dynamics at continental to global scales is confounded by shortcomings in the observed record. Modeled assessments also yield conflicting results which are linked to differences in model structure and simulation protocol. Here we compare simulated gridded (1 spatial resolution) runoff from six terrestrial biosphere models (TBMs), seven reanalysis products, and one gridded surface station product in the contiguous United States (CONUS) from 2001 to 2005. We evaluate the consistency of these 14 estimates with stream gauge data, both as depleted flow and corrected for net withdrawals (2005 only), at the CONUS and water resource region scale, as well as examining similarity across TBMs and reanalysis products at the grid cell scale. Mean runoff across all simulated products and regions varies widely (range: 71 to 356 mm yr(-1)) relative to observed continental-scale runoff (209 or 280 mm yr(-1) when corrected for net withdrawals). Across all 14 products 8 exhibit Nash-Sutcliffe efficiency values in excess of 0.8 and three are within 10% of the observed value. Region-level mismatch exhibits a weak pattern of overestimation in western and underestimation in eastern regions although two products are systematically biased across all regions and largely scales with water use. Although gridded composite TBM and reanalysis runoff show some regional similarities, individual product values are highly variable. At the coarse scales used here we find that progress in better constraining simulated runoff requires standardized forcing data and the explicit incorporation of human effects (e.g., water withdrawals by source, fire, and land use change). (C) 2015 Elsevier B.V. All rights reserved.},
doi = {10.1016/j.ecolmodel.2015.02.006},
journal = {Ecological Modelling},
number = ,
volume = 303,
place = {United States},
year = {Wed Mar 11 00:00:00 EDT 2015},
month = {Wed Mar 11 00:00:00 EDT 2015}
}

Journal Article:
Free Publicly Available Full Text
Publisher's Version of Record

Citation Metrics:
Cited by: 1 work
Citation information provided by
Web of Science

Save / Share: