Hillslope Hydrology in Global Change Research and Earth System Modeling

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  • Y. Fan
    Department of Earth and Planetary Sciences State University of New Jersey Rutgers New Brunswick NJ USA
  • M. Clark
    National Center for Atmospheric Research Boulder CO USA
  • D. M. Lawrence
    National Center for Atmospheric Research Boulder CO USA
  • S. Swenson
    National Center for Atmospheric Research Boulder CO USA
  • L. E. Band
    Department of Environmental Sciences University of Virginia Charlottesville VA USA
  • S. L. Brantley
    Earth and Environmental Systems Institute, Department of Geosciences Pennsylvania State University University Park PA USA
  • P. D. Brooks
    Department of Geology and Geophysics University of Utah Salt Lake City UT USA
  • W. E. Dietrich
    Department of Earth and Planetary Science University of California Berkeley CA USA
  • A. Flores
    Department of Geosciences Boise State University Boise ID USA
  • G. Grant
    College of Earth Ocean and Atmospheric Sciences Oregon State University Corvallis OR USA
  • J. W. Kirchner
    Department of Environmental Systems Science ETH Zürich Zürich Switzerland
  • D. S. Mackay
    Department of Geography The State University of New York at Buffalo Buffalo NY USA
  • J. J. McDonnell
    School of Environment and Sustainability University of Saskatchewan Saskatoon Saskatchewan Canada
  • P. C. D. Milly
    U.S. Geological Survey Princeton NJ USA
  • P. L. Sullivan
    Department of Geography and Atmospheric Science University of Kansas Lawrence KS USA
  • C. Tague
    Bren School of Environmental Science & Management University of California Santa Barbara CA USA
  • H. Ajami
    Department of Environmental Sciences University of California Riverside CA USA
  • N. Chaney
    Department of Civil and Environmental Engineering Duke University Durham NC USA
  • A. Hartmann
    Department Earth and Environmental Sciences Universities of Freiburg Freiburg Germany
  • P. Hazenberg
    Department of Geosciences University of Arizona Tucson AZ USA
  • J. McNamara
    Department of Geosciences Boise State University Boise ID USA
  • J. Pelletier
    Laboratory of Hydrology and Water Management Ghent University Ghent Belgium
  • J. Perket
    National Center for Atmospheric Research Boulder CO USA
  • E. Rouholahnejad‐Freund
    Department of Civil Engineering University of Bristol Bristol UK
  • T. Wagener
    Department of Hydrology & Atmospheric Sciences University of Arizona Tucson AZ USA
  • X. Zeng
    Department of Hydrology & Atmospheric Sciences University of Arizona Tucson AZ USA
  • E. Beighley
    Department of Civil and Environmental Engineering Northeastern University Boston MA USA
  • J. Buzan
    Department of Earth, Atmospheric, and Planetary Sciences Purdue University West Lafayette IN USA
  • M. Huang
    Atmospheric Sciences and Global Change Division Pacific Northwest National Laboratory Richland WA USA
  • B. Livneh
    Department of Civil, Environmental and Architectural Engineering University of Colorado Boulder Boulder CO USA
  • B. P. Mohanty
    Department of Biological and Agricultural Engineering Texas A&M University College Station TX USA
  • B. Nijssen
    Department of Civil and Environmental Engineering University of Washington Seattle WA USA
  • M. Safeeq
    School of Engineering University of California, Merced Fresno CA USA
  • C. Shen
    Department of Civil and Environmental Engineering Pennsylvania State University University Park PA USA
  • W. van Verseveld
    Department of Catchment and Urban Hydrology Deltares Delft The Netherlands
  • J. Volk
    Department of Geological Sciences and Engineering University of Nevada, Reno Reno NV USA
  • D. Yamazaki
    Institute of Industrial Science The University of Tokyo Tokyo Japan

書誌事項

公開日
2019-02
資源種別
journal article
権利情報
  • http://onlinelibrary.wiley.com/termsAndConditions#vor
DOI
  • 10.1029/2018wr023903
公開者
American Geophysical Union (AGU)

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説明

<jats:title>Abstract</jats:title><jats:p>Earth System Models (ESMs) are essential tools for understanding and predicting global change, but they cannot explicitly resolve hillslope‐scale terrain structures that fundamentally organize water, energy, and biogeochemical stores and fluxes at subgrid scales. Here we bring together hydrologists, Critical Zone scientists, and ESM developers, to explore how hillslope structures may modulate ESM grid‐level water, energy, and biogeochemical fluxes. In contrast to the one‐dimensional (1‐D), 2‐ to 3‐m deep, and free‐draining soil hydrology in most ESM land models, we hypothesize that 3‐D, lateral ridge‐to‐valley flow through shallow and deep paths and insolation contrasts between sunny and shady slopes are the top two globally quantifiable organizers of water and energy (and vegetation) within an ESM grid cell. We hypothesize that these two processes are likely to impact ESM predictions where (and when) water and/or energy are limiting. We further hypothesize that, if implemented in ESM land models, these processes will increase simulated continental water storage and residence time, buffering terrestrial ecosystems against seasonal and interannual droughts. We explore efficient ways to capture these mechanisms in ESMs and identify critical knowledge gaps preventing us from scaling up hillslope to global processes. One such gap is our extremely limited knowledge of the subsurface, where water is stored (supporting vegetation) and released to stream baseflow (supporting aquatic ecosystems). We conclude with a set of organizing hypotheses and a call for global syntheses activities and model experiments to assess the impact of hillslope hydrology on global change predictions.</jats:p>

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