A glimpse beneath earth's surface: GLobal HYdrogeology MaPS (GLHYMPS) of permeability and porosity

The lack of robust, spatially distributed subsurface data is the key obstacle limiting the implementation of complex and realistic groundwater dynamics into global land surface, hydrologic, and climate models. We map and analyze permeability and porosity globally and at high resolution for the first time. The new permeability and porosity maps are based on a recently completed high-resolution global lithology map that differentiates fine and coarse-grained sediments and sedimentary rocks, which is important since these have different permeabilities. The average polygon size in the new map is ~100 km2, which is a more than hundredfold increase in resolution compared to the previous map which has an average polygon size of ~14,000 km2. We also significantly improve the representation in regions of weathered tropical soils and permafrost. The spatially distributed mean global permeability ~10−15 m2 with permafrost or ~10−14 m2 without permafrost. The spatially distributed mean porosity of the globe is 14%. The maps will enable further integration of groundwater dynamics into land surface, hydrologic, and climate models.

[1]  N. LeRoy Poff,et al.  The ecological limits of hydrologic alteration (ELOHA): a new framework for developing regional environmental flow standards , 2007 .

[2]  A. Hoekstra,et al.  The water footprint of humanity , 2011, Proceedings of the National Academy of Sciences.

[3]  P. Döll,et al.  Global-scale modeling of groundwater recharge , 2008 .

[4]  Helen Bonsor,et al.  Quantitative maps of groundwater resources in Africa , 2012 .

[5]  Jens Hartmann,et al.  The new global lithological map database GLiM: A representation of rock properties at the Earth surface , 2012 .

[6]  S. Kanae,et al.  Model estimates of sea-level change due to anthropogenic impacts on terrestrial water storage , 2012 .

[7]  S. Ingebritsen,et al.  Geological implications of a permeability-depth curve for the continental crust , 1999 .

[8]  D. A. Morris,et al.  Summary of hydrologic and physical properties of rock and soil materials, as analyzed by the hydrologic laboratory of the U.S. Geological Survey, 1948-60 , 1966 .

[9]  B. Scanlon,et al.  Impact of water withdrawals from groundwater and surface water on continental water storage variations , 2012 .

[10]  Stephan Gruber,et al.  Derivation and analysis of a high-resolution estimate of global permafrost zonation , 2011 .

[11]  J. Hartmann,et al.  Lithological composition of the North American continent and implications of lithological map resolution for dissolved silica flux modeling , 2010 .

[12]  R. Maxwell,et al.  Interdependence of groundwater dynamics and land-energy feedbacks under climate change , 2008 .

[13]  Naota Hanasaki,et al.  An estimation of global virtual water flow and sources of water withdrawal for major crops and livestock products using a global hydrological model , 2010 .

[14]  A. Hoekstra,et al.  Global Monthly Water Scarcity: Blue Water Footprints versus Blue Water Availability , 2012, PloS one.

[15]  L. V. Beek,et al.  Water balance of global aquifers revealed by groundwater footprint , 2012, Nature.

[16]  Jens Hartmann,et al.  Mapping permeability over the surface of the Earth , 2011 .

[17]  S. M. de Jong,et al.  Large-scale groundwater modeling using global datasets: a test case for the Rhine-Meuse basin , 2011 .

[18]  V. Smakhtin Low flow hydrology: a review , 2001 .

[19]  R. H. Brooks,et al.  Hydraulic properties of porous media , 1963 .

[20]  H. Velthuizen,et al.  Harmonized World Soil Database (version 1.2) , 2008 .

[21]  H. Douville,et al.  A Simple Groundwater Scheme for Hydrological and Climate Applications: Description and Offline Evaluation over France , 2012 .

[22]  L. Konikow Contribution of global groundwater depletion since 1900 to sea‐level rise , 2011 .

[23]  Michel Meybeck,et al.  Lithologic composition of the Earth's continental surfaces derived from a new digital map emphasizing riverine material transfer , 2005 .

[24]  Haibin Li,et al.  Groundwater flow across spatial scales: importance for climate modeling , 2014 .

[25]  W. Lucht,et al.  Agricultural green and blue water consumption and its influence on the global water system , 2008 .

[26]  S. M. de Jong,et al.  Large-scale groundwater modeling using global datasets: a test case for the Rhine-Meuse basin , 2011 .

[27]  M. Bierkens,et al.  Nonsustainable groundwater sustaining irrigation: A global assessment , 2012 .

[28]  A. Hoekstra Human appropriation of natural capital: A comparison of ecological footprint and water footprint analysis , 2009 .

[29]  B. Scanlon,et al.  Ground water and climate change , 2013 .

[30]  J. Rockström,et al.  Greening the global water system , 2010 .

[31]  J. Proudman International Union of Geodesy and Geophysics , 1948, Nature.

[32]  Y. Fan,et al.  Global Patterns of Groundwater Table Depth , 2013, Science.

[33]  Petra Döll,et al.  A Pilot Global Assessment of Environmental Water Requirements and Scarcity , 2004 .

[34]  M. Bierkens,et al.  Global depletion of groundwater resources , 2010 .

[35]  T. Gleeson,et al.  Regional strategies for the accelerating global problem of groundwater depletion , 2012 .

[36]  Van Genuchten,et al.  A closed-form equation for predicting the hydraulic conductivity of unsaturated soils , 1980 .