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Soil structure is an important omission in Earth System Models
Most soil hydraulic information used in Earth System Models (ESMs) is derived from pedo-transfer functions that use easy-to-measure soil attributes to estimate hydraulic parameters. This parameterization relies heavily on soil texture, but overlooks the critical role of soil structure originated by...
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| Published in: | Nature communications 2020-01, Vol.11 (1), p.522-522, Article 522 |
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| creator | Fatichi, Simone Or, Dani Walko, Robert Vereecken, Harry Young, Michael H. Ghezzehei, Teamrat A. Hengl, Tomislav Kollet, Stefan Agam, Nurit Avissar, Roni |
| description | Most soil hydraulic information used in Earth System Models (ESMs) is derived from pedo-transfer functions that use easy-to-measure soil attributes to estimate hydraulic parameters. This parameterization relies heavily on soil texture, but overlooks the critical role of soil structure originated by soil biophysical activity. Soil structure omission is pervasive also in sampling and measurement methods used to train pedotransfer functions. Here we show how systematic inclusion of salient soil structural features of biophysical origin affect local and global hydrologic and climatic responses. Locally, including soil structure in models significantly alters infiltration-runoff partitioning and recharge in wet and vegetated regions. Globally, the coarse spatial resolution of ESMs and their inability to simulate intense and short rainfall events mask effects of soil structure on surface fluxes and climate. Results suggest that although soil structure affects local hydrologic response, its implications on global-scale climate remains elusive in current ESMs.
The effect of soil structure is not included in most Earth System Models. The authors here introduce and evaluate the consequences at local and global scale of modifying hydraulic properties of soils in response to biological activity—a process significantly changing soil structure. |
| doi_str_mv | 10.1038/s41467-020-14411-z |
| format | article |
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The effect of soil structure is not included in most Earth System Models. The authors here introduce and evaluate the consequences at local and global scale of modifying hydraulic properties of soils in response to biological activity—a process significantly changing soil structure.</description><identifier>ISSN: 2041-1723</identifier><identifier>EISSN: 2041-1723</identifier><identifier>DOI: 10.1038/s41467-020-14411-z</identifier><identifier>PMID: 31988306</identifier><language>eng</language><publisher>London: Nature Publishing Group UK</publisher><subject>704/106 ; 704/242 ; Biological activity ; Computer simulation ; Earth ; Fluxes ; Humanities and Social Sciences ; Hydraulic properties ; Hydraulics ; Hydrology ; Information systems ; Measurement methods ; multidisciplinary ; Parameter estimation ; Parameterization ; Rainfall ; Runoff ; Science ; Science (multidisciplinary) ; Soil properties ; Soil structure ; Soil texture ; Soils ; Spatial resolution ; Texture ; Transfer functions</subject><ispartof>Nature communications, 2020-01, Vol.11 (1), p.522-522, Article 522</ispartof><rights>The Author(s) 2020</rights><rights>This work is published under http://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c606t-24cccfc48f28e1a6000056fbb23742be7774587cb8b895265411d90bac2925e53</citedby><cites>FETCH-LOGICAL-c606t-24cccfc48f28e1a6000056fbb23742be7774587cb8b895265411d90bac2925e53</cites><orcidid>0000-0002-0287-6212 ; 0000-0001-8479-9910 ; 0000-0002-8921-6179 ; 0000-0003-1361-6659 ; 0000-0002-3236-2933 ; 0000-0002-9921-5129</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2346400032/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2346400032?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>230,314,727,780,784,885,25751,27922,27923,37010,37011,44588,53789,53791,74896</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/31988306$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Fatichi, Simone</creatorcontrib><creatorcontrib>Or, Dani</creatorcontrib><creatorcontrib>Walko, Robert</creatorcontrib><creatorcontrib>Vereecken, Harry</creatorcontrib><creatorcontrib>Young, Michael H.</creatorcontrib><creatorcontrib>Ghezzehei, Teamrat A.</creatorcontrib><creatorcontrib>Hengl, Tomislav</creatorcontrib><creatorcontrib>Kollet, Stefan</creatorcontrib><creatorcontrib>Agam, Nurit</creatorcontrib><creatorcontrib>Avissar, Roni</creatorcontrib><title>Soil structure is an important omission in Earth System Models</title><title>Nature communications</title><addtitle>Nat Commun</addtitle><addtitle>Nat Commun</addtitle><description>Most soil hydraulic information used in Earth System Models (ESMs) is derived from pedo-transfer functions that use easy-to-measure soil attributes to estimate hydraulic parameters. This parameterization relies heavily on soil texture, but overlooks the critical role of soil structure originated by soil biophysical activity. Soil structure omission is pervasive also in sampling and measurement methods used to train pedotransfer functions. Here we show how systematic inclusion of salient soil structural features of biophysical origin affect local and global hydrologic and climatic responses. Locally, including soil structure in models significantly alters infiltration-runoff partitioning and recharge in wet and vegetated regions. Globally, the coarse spatial resolution of ESMs and their inability to simulate intense and short rainfall events mask effects of soil structure on surface fluxes and climate. Results suggest that although soil structure affects local hydrologic response, its implications on global-scale climate remains elusive in current ESMs.
The effect of soil structure is not included in most Earth System Models. 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This parameterization relies heavily on soil texture, but overlooks the critical role of soil structure originated by soil biophysical activity. Soil structure omission is pervasive also in sampling and measurement methods used to train pedotransfer functions. Here we show how systematic inclusion of salient soil structural features of biophysical origin affect local and global hydrologic and climatic responses. Locally, including soil structure in models significantly alters infiltration-runoff partitioning and recharge in wet and vegetated regions. Globally, the coarse spatial resolution of ESMs and their inability to simulate intense and short rainfall events mask effects of soil structure on surface fluxes and climate. Results suggest that although soil structure affects local hydrologic response, its implications on global-scale climate remains elusive in current ESMs.
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| subjects | 704/106 704/242 Biological activity Computer simulation Earth Fluxes Humanities and Social Sciences Hydraulic properties Hydraulics Hydrology Information systems Measurement methods multidisciplinary Parameter estimation Parameterization Rainfall Runoff Science Science (multidisciplinary) Soil properties Soil structure Soil texture Soils Spatial resolution Texture Transfer functions |
| title | Soil structure is an important omission in Earth System Models |
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