{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,6,1]],"date-time":"2026-06-01T13:47:27Z","timestamp":1780321647124,"version":"3.54.1"},"reference-count":19,"publisher":"Wiley","issue":"20","license":[{"start":{"date-parts":[[2005,8,26]],"date-time":"2005-08-26T00:00:00Z","timestamp":1125014400000},"content-version":"vor","delay-in-days":0,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Hydrological Processes"],"published-print":{"date-parts":[[2005,12,30]]},"abstract":"<jats:title>Abstract<\/jats:title><jats:p>Hydraulic connectivity on hillslopes and the existence of preferred soil moisture states in a catchment have important controls on runoff generation. In this study we investigate the relationships between soil moisture patterns, lateral hillslope flow, and streamflow generation in a semi\u2010arid, snowmelt\u2010driven catchment. We identify five soil moisture conditions that occur during a year and present a conceptual model based on field studies and computer simulations of how streamflow is generated with respect to the soil moisture conditions. The five soil moisture conditions are (1) a summer dry period, (2) a transitional fall wetting period, (3) a winter wet, low\u2010flux period, (4) a spring wet, high\u2010flux period, and (5) a transitional late\u2010spring drying period. Transitions between the periods are driven by changes in the water balance between rain, snow, snowmelt and evapotranspiration. Low rates of water input to the soil during the winter allow dry soil regions to persist at the soil\u2013bedrock interface, which act as barriers to lateral flow. Once the dry\u2010soil flow barriers are wetted, whole\u2010slope hydraulic connectivity is established, lateral flow can occur, and upland soils are in direct connection with the near\u2010stream soil moisture. This whole\u2010slope connectivity can alter near\u2010stream hydraulics and modify the delivery of water, pressure, and solutes to the stream. Copyright \u00a9 2005 John Wiley &amp; Sons, Ltd.<\/jats:p>","DOI":"10.1002\/hyp.5869","type":"journal-article","created":{"date-parts":[[2005,8,26]],"date-time":"2005-08-26T17:16:49Z","timestamp":1125076609000},"page":"4023-4038","source":"Crossref","is-referenced-by-count":283,"title":["Soil moisture states, lateral flow, and streamflow generation in a semi\u2010arid, snowmelt\u2010driven catchment"],"prefix":"10.1002","volume":"19","author":[{"given":"James P.","family":"McNamara","sequence":"first","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"David","family":"Chandler","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Mark","family":"Seyfried","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Shiva","family":"Achet","sequence":"additional","affiliation":[],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"311","published-online":{"date-parts":[[2005,8,26]]},"reference":[{"key":"e_1_2_1_2_1","doi-asserted-by":"publisher","DOI":"10.1080\/02626667909491834"},{"key":"e_1_2_1_3_1","doi-asserted-by":"crossref","first-page":"61","DOI":"10.1061\/JRCEA4.0000425","article-title":"Properties of porous media affecting fluid flow","volume":"92","author":"Brooks RH","year":"1966","journal-title":"Journal of Irrigation and Drainage, Division of the American Society of Civil Engineers"},{"key":"e_1_2_1_4_1","doi-asserted-by":"publisher","DOI":"10.2136\/sssaj2002.1571"},{"key":"e_1_2_1_5_1","doi-asserted-by":"publisher","DOI":"10.2136\/sssaj2004.1501"},{"key":"e_1_2_1_6_1","volume-title":"Physical Hydrology","author":"Dingman SL","year":"1994"},{"key":"e_1_2_1_7_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0022-1694(00)00299-7"},{"key":"e_1_2_1_8_1","doi-asserted-by":"publisher","DOI":"10.1029\/96WR01240"},{"key":"e_1_2_1_9_1","doi-asserted-by":"publisher","DOI":"10.1029\/2001WR000872"},{"key":"e_1_2_1_10_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0022-1694(01)00483-8"},{"key":"e_1_2_1_11_1","doi-asserted-by":"publisher","DOI":"10.1029\/97WR02174"},{"key":"e_1_2_1_12_1","unstructured":"HarknessA.1997.Soil survey of Boise Front Project Idaho. 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Masters thesis Boise State University Boise ID."}],"container-title":["Hydrological Processes"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/api.wiley.com\/onlinelibrary\/tdm\/v1\/articles\/10.1002%2Fhyp.5869","content-type":"unspecified","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/onlinelibrary.wiley.com\/doi\/pdf\/10.1002\/hyp.5869","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2023,10,18]],"date-time":"2023-10-18T23:09:16Z","timestamp":1697670556000},"score":1,"resource":{"primary":{"URL":"https:\/\/onlinelibrary.wiley.com\/doi\/10.1002\/hyp.5869"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2005,8,26]]},"references-count":19,"journal-issue":{"issue":"20","published-print":{"date-parts":[[2005,12,30]]}},"alternative-id":["10.1002\/hyp.5869"],"URL":"https:\/\/doi.org\/10.1002\/hyp.5869","archive":["Portico"],"relation":{},"ISSN":["0885-6087","1099-1085"],"issn-type":[{"value":"0885-6087","type":"print"},{"value":"1099-1085","type":"electronic"}],"subject":[],"published":{"date-parts":[[2005,8,26]]}}}