FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2897620167> ?p ?o ?g. }

• W2897620167 abstract "Abstract Climate warming will have substantial impacts on hydrological fluxes in the California Sierra. A commonly used approach for assessing these impacts, particularly in mountain watersheds, is to substitute space for time. This conceptual model assumes that with warming, the hydrologic behaviour of higher elevation snow dominated watersheds (SDWs) will converge to the hydrologic behaviour of lower elevation transient snow watersheds (TSWs). To investigate the efficacy of this conceptual model, a process‐based model (RHESSys) was applied to a TSW and a SDW with a mean annual temperature 2 °C lower than the TSW in the Sierra National forest, California. This study investigated the effect of climate warming (2 and 4 °C) on the model estimates of snow water equivalent (SWE), streamflow, evapotranspiration (ET), and moisture deficit in the two watersheds. Modelling results show that SDW under 2 °C warming scenarios generates monthly SWE similar in magnitude and timing as TSW under historic conditions. However, SDW under 2 °C warming scenarios generates higher annual and summer streamflow due to shallower groundwater storage and experiences less water limitation due to lower ET, compared with TSW under historical climate conditions. In both watersheds, leaf area index and wetness index are primary factors controlling spatial patterns of seasonal ET under both historical climate conditions and warming scenarios. Climate warming increases the spatial variability in monthly ET, especially in the summer period. These modelling results suggest that vegetation structure and subsurface properties may be as important as climate in explaining hydrologic response to climate warming in small Sierra Nevada watersheds." @default.
• W2897620167 created "2018-10-26" @default.
• W2897620167 creator A5063640667 @default.
• W2897620167 creator A5067616792 @default.
• W2897620167 date "2018-11-13" @default.
• W2897620167 modified "2023-10-14" @default.
• W2897620167 title "Hydrologic responses to climate warming for a snow‐dominated watershed and a transient snow watershed in the California Sierra" @default.
• W2897620167 cites W1496634218 @default.
• W2897620167 cites W1498058617 @default.
• W2897620167 cites W1538296957 @default.
• W2897620167 cites W1565052374 @default.
• W2897620167 cites W1626579693 @default.
• W2897620167 cites W1680419106 @default.
• W2897620167 cites W1922160021 @default.
• W2897620167 cites W1962100519 @default.
• W2897620167 cites W1979778704 @default.
• W2897620167 cites W1980409935 @default.
• W2897620167 cites W1981646498 @default.
• W2897620167 cites W1991921673 @default.
• W2897620167 cites W2001211618 @default.
• W2897620167 cites W2002910992 @default.
• W2897620167 cites W2009489718 @default.
• W2897620167 cites W2024684186 @default.
• W2897620167 cites W2025401040 @default.
• W2897620167 cites W2033904036 @default.
• W2897620167 cites W2044022514 @default.
• W2897620167 cites W2051864512 @default.
• W2897620167 cites W2071333124 @default.
• W2897620167 cites W2080758103 @default.
• W2897620167 cites W2086953577 @default.
• W2897620167 cites W2087105362 @default.
• W2897620167 cites W2087513725 @default.
• W2897620167 cites W2094405218 @default.
• W2897620167 cites W2097837411 @default.
• W2897620167 cites W2099095111 @default.
• W2897620167 cites W2106632946 @default.
• W2897620167 cites W2117617809 @default.
• W2897620167 cites W2121464259 @default.
• W2897620167 cites W2122412480 @default.
• W2897620167 cites W2138229357 @default.
• W2897620167 cites W2148719805 @default.
• W2897620167 cites W2149173304 @default.
• W2897620167 cites W2153427373 @default.
• W2897620167 cites W2156351447 @default.
• W2897620167 cites W2157526647 @default.
• W2897620167 cites W2160258023 @default.
• W2897620167 cites W2171366295 @default.
• W2897620167 cites W2180426220 @default.
• W2897620167 doi "https://doi.org/10.1002/eco.2053" @default.
• W2897620167 hasPublicationYear "2018" @default.
• W2897620167 type Work @default.
• W2897620167 sameAs 2897620167 @default.
• W2897620167 citedByCount "11" @default.
• W2897620167 countsByYear W28976201672020 @default.
• W2897620167 countsByYear W28976201672021 @default.
• W2897620167 countsByYear W28976201672022 @default.
• W2897620167 countsByYear W28976201672023 @default.
• W2897620167 crossrefType "journal-article" @default.
• W2897620167 hasAuthorship W2897620167A5063640667 @default.
• W2897620167 hasAuthorship W2897620167A5067616792 @default.
• W2897620167 hasBestOaLocation W28976201671 @default.
• W2897620167 hasConcept C107054158 @default.
• W2897620167 hasConcept C115343472 @default.
• W2897620167 hasConcept C119857082 @default.
• W2897620167 hasConcept C126197015 @default.
• W2897620167 hasConcept C126645576 @default.
• W2897620167 hasConcept C127313418 @default.
• W2897620167 hasConcept C132651083 @default.
• W2897620167 hasConcept C150547873 @default.
• W2897620167 hasConcept C153294291 @default.
• W2897620167 hasConcept C176783924 @default.
• W2897620167 hasConcept C187320778 @default.
• W2897620167 hasConcept C18903297 @default.
• W2897620167 hasConcept C197046000 @default.
• W2897620167 hasConcept C205649164 @default.
• W2897620167 hasConcept C39432304 @default.
• W2897620167 hasConcept C41008148 @default.
• W2897620167 hasConcept C49204034 @default.
• W2897620167 hasConcept C53739315 @default.
• W2897620167 hasConcept C58640448 @default.
• W2897620167 hasConcept C76886044 @default.
• W2897620167 hasConcept C86803240 @default.
• W2897620167 hasConceptScore W2897620167C107054158 @default.
• W2897620167 hasConceptScore W2897620167C115343472 @default.
• W2897620167 hasConceptScore W2897620167C119857082 @default.
• W2897620167 hasConceptScore W2897620167C126197015 @default.
• W2897620167 hasConceptScore W2897620167C126645576 @default.
• W2897620167 hasConceptScore W2897620167C127313418 @default.
• W2897620167 hasConceptScore W2897620167C132651083 @default.
• W2897620167 hasConceptScore W2897620167C150547873 @default.
• W2897620167 hasConceptScore W2897620167C153294291 @default.
• W2897620167 hasConceptScore W2897620167C176783924 @default.
• W2897620167 hasConceptScore W2897620167C187320778 @default.
• W2897620167 hasConceptScore W2897620167C18903297 @default.
• W2897620167 hasConceptScore W2897620167C197046000 @default.
• W2897620167 hasConceptScore W2897620167C205649164 @default.
• W2897620167 hasConceptScore W2897620167C39432304 @default.
• W2897620167 hasConceptScore W2897620167C41008148 @default.
• W2897620167 hasConceptScore W2897620167C49204034 @default.
• W2897620167 hasConceptScore W2897620167C53739315 @default.

• next