FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2161738894> ?p ?o ?g. }

• W2161738894 endingPage "256" @default.
• W2161738894 startingPage "245" @default.
• W2161738894 abstract "Fire is a primary agent of landcover transformation in California semi-arid shrubland watersheds, however few studies have examined the impacts of fire and post-fire succession on streamflow dynamics in these basins. While it may seem intuitive that larger fires will have a greater impact on streamflow response than smaller fires in these watersheds, the nature of these relationships has not been determined. The effects of fire size on seasonal and annual streamflow responses were investigated for a medium-sized basin in central California using a modified version of the MIKE SHE model which had been previously calibrated and tested for this watershed using the Generalized Likelihood Uncertainty Estimation methodology. Model simulations were made for two contrasting periods, wet and dry, in order to assess whether fire size effects varied with weather regime. Results indicated that seasonal and annual streamflow response increased nearly linearly with fire size in a given year under both regimes. Annual flow response was generally higher in wetter years for both weather regimes, however a clear trend was confounded by the effect of stand age. These results expand our understanding of the effects of fire size on hydrologic response in chaparral watersheds, but it is important to note that the majority of model predictions were largely indistinguishable from the predictive uncertainty associated with the calibrated model—a key finding that highlights the importance of analyzing hydrologic predictions for altered landcover conditions in the context of model uncertainty. Future work is needed to examine how alternative decisions (e.g., different likelihood measures) may influence GLUE-based MIKE SHE streamflow predictions following different size fires, and how the effect of fire size on streamflow varies with other factors such as fire location." @default.
• W2161738894 created "2016-06-24" @default.
• W2161738894 creator A5045103641 @default.
• W2161738894 creator A5062920255 @default.
• W2161738894 date "2007-08-01" @default.
• W2161738894 modified "2023-10-14" @default.
• W2161738894 title "Predicting streamflow response to fire-induced landcover change: Implications of parameter uncertainty in the MIKE SHE model" @default.
• W2161738894 cites W1965568221 @default.
• W2161738894 cites W1971927512 @default.
• W2161738894 cites W1980937546 @default.
• W2161738894 cites W1983763074 @default.
• W2161738894 cites W1984868512 @default.
• W2161738894 cites W1987017697 @default.
• W2161738894 cites W1991921673 @default.
• W2161738894 cites W1994056660 @default.
• W2161738894 cites W1994619160 @default.
• W2161738894 cites W1996309381 @default.
• W2161738894 cites W2003696872 @default.
• W2161738894 cites W2007844036 @default.
• W2161738894 cites W2010934341 @default.
• W2161738894 cites W2018648266 @default.
• W2161738894 cites W2032608841 @default.
• W2161738894 cites W2036702728 @default.
• W2161738894 cites W2048330891 @default.
• W2161738894 cites W2054048804 @default.
• W2161738894 cites W2056995680 @default.
• W2161738894 cites W2073693966 @default.
• W2161738894 cites W2075108083 @default.
• W2161738894 cites W2075680927 @default.
• W2161738894 cites W2077249466 @default.
• W2161738894 cites W2086420480 @default.
• W2161738894 cites W2100422466 @default.
• W2161738894 cites W2120745888 @default.
• W2161738894 cites W2124738823 @default.
• W2161738894 cites W2156071316 @default.
• W2161738894 cites W2156248359 @default.
• W2161738894 cites W2165229670 @default.
• W2161738894 cites W2509752783 @default.
• W2161738894 cites W3095581964 @default.
• W2161738894 doi "https://doi.org/10.1016/j.jenvman.2006.06.003" @default.
• W2161738894 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/16901617" @default.
• W2161738894 hasPublicationYear "2007" @default.
• W2161738894 type Work @default.
• W2161738894 sameAs 2161738894 @default.
• W2161738894 citedByCount "36" @default.
• W2161738894 countsByYear W21617388942012 @default.
• W2161738894 countsByYear W21617388942013 @default.
• W2161738894 countsByYear W21617388942014 @default.
• W2161738894 countsByYear W21617388942015 @default.
• W2161738894 countsByYear W21617388942016 @default.
• W2161738894 countsByYear W21617388942017 @default.
• W2161738894 countsByYear W21617388942018 @default.
• W2161738894 countsByYear W21617388942019 @default.
• W2161738894 countsByYear W21617388942020 @default.
• W2161738894 countsByYear W21617388942021 @default.
• W2161738894 countsByYear W21617388942022 @default.
• W2161738894 countsByYear W21617388942023 @default.
• W2161738894 crossrefType "journal-article" @default.
• W2161738894 hasAuthorship W2161738894A5045103641 @default.
• W2161738894 hasAuthorship W2161738894A5062920255 @default.
• W2161738894 hasConcept C110872660 @default.
• W2161738894 hasConcept C119857082 @default.
• W2161738894 hasConcept C126645576 @default.
• W2161738894 hasConcept C127313418 @default.
• W2161738894 hasConcept C127413603 @default.
• W2161738894 hasConcept C132651083 @default.
• W2161738894 hasConcept C150547873 @default.
• W2161738894 hasConcept C166957645 @default.
• W2161738894 hasConcept C187320778 @default.
• W2161738894 hasConcept C18903297 @default.
• W2161738894 hasConcept C205649164 @default.
• W2161738894 hasConcept C2777707811 @default.
• W2161738894 hasConcept C2779343474 @default.
• W2161738894 hasConcept C39432304 @default.
• W2161738894 hasConcept C41008148 @default.
• W2161738894 hasConcept C49204034 @default.
• W2161738894 hasConcept C53739315 @default.
• W2161738894 hasConcept C58640448 @default.
• W2161738894 hasConcept C59898753 @default.
• W2161738894 hasConcept C76886044 @default.
• W2161738894 hasConcept C86803240 @default.
• W2161738894 hasConceptScore W2161738894C110872660 @default.
• W2161738894 hasConceptScore W2161738894C119857082 @default.
• W2161738894 hasConceptScore W2161738894C126645576 @default.
• W2161738894 hasConceptScore W2161738894C127313418 @default.
• W2161738894 hasConceptScore W2161738894C127413603 @default.
• W2161738894 hasConceptScore W2161738894C132651083 @default.
• W2161738894 hasConceptScore W2161738894C150547873 @default.
• W2161738894 hasConceptScore W2161738894C166957645 @default.
• W2161738894 hasConceptScore W2161738894C187320778 @default.
• W2161738894 hasConceptScore W2161738894C18903297 @default.
• W2161738894 hasConceptScore W2161738894C205649164 @default.
• W2161738894 hasConceptScore W2161738894C2777707811 @default.
• W2161738894 hasConceptScore W2161738894C2779343474 @default.
• W2161738894 hasConceptScore W2161738894C39432304 @default.
• W2161738894 hasConceptScore W2161738894C41008148 @default.
• W2161738894 hasConceptScore W2161738894C49204034 @default.
• W2161738894 hasConceptScore W2161738894C53739315 @default.

• next