FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4311091136> ?p ?o ?g. }

• W4311091136 endingPage "100144" @default.
• W4311091136 startingPage "100144" @default.
• W4311091136 abstract "As glaciers across the world continue to recede, there is a concern that their loss as a fresh water reservoir within mountainous basins will have a negative impact on stream temperatures and downstream water resources. Currently, there are relatively few glacio-hydrological models (GHMs) appropriate to study such phenomena and studies that have used GHMs generally acknowledge the high uncertainty associated with their simulations. Calibration techniques present a particular issue in GHMs as available glacier observations are limited and errors in the glacierized portion of a basin can be compensated by errors in the non-glacierized portion. Using as a study site the Cheakamus Basin in British Columbia, Canada, we 1) present a new, fully-coupled GHM, 2) analyze the effects different calibration techniques have on the model’s summer streamflow projections, and 3) compare the fully-coupled GHM results to projections using a one-way GHM. The calibration techniques studied vary in terms of glacier representation (dynamic/static), and glacier constraint (mass balance/thinning rates/thinning rates and area change). We find projected future climate forcings are sufficiently strong in the Cheakamus Basin so as to generally make the sign and significance of changes to the basin’s hydrology insensitive to the calibration and projection procedures studied. However, the variation among these procedures produces significant changes in the projected magnitude of future hydrological changes and therefore should be carefully considered in studies where precision beyond the sign and significance of change is required. Based on analysis of the variation within each procedure’s set of model outputs, we conclude 1) the two-way GHM has benefits over the one-way model, 2) calibration using dynamic glaciers and a thinning rate constraint is preferable for the new GHM, and 3) there is a need for additional studies on the uncertainties associated with the calibration of glacio-hydrological models." @default.
• W4311091136 created "2022-12-23" @default.
• W4311091136 creator A5012185198 @default.
• W4311091136 creator A5017651505 @default.
• W4311091136 date "2022-12-01" @default.
• W4311091136 modified "2023-10-14" @default.
• W4311091136 title "Assessing the influence of calibration methodology and model structure on glacio-hydrological simulations in the Cheakamus River Basin, British Columbia, Canada" @default.
• W4311091136 cites W1050971263 @default.
• W4311091136 cites W1480015928 @default.
• W4311091136 cites W1488838383 @default.
• W4311091136 cites W1680347109 @default.
• W4311091136 cites W1833846818 @default.
• W4311091136 cites W1907702319 @default.
• W4311091136 cites W1964337735 @default.
• W4311091136 cites W1981263865 @default.
• W4311091136 cites W1994293139 @default.
• W4311091136 cites W1995806727 @default.
• W4311091136 cites W2001833158 @default.
• W4311091136 cites W2004245996 @default.
• W4311091136 cites W2007134419 @default.
• W4311091136 cites W2010281465 @default.
• W4311091136 cites W2013061102 @default.
• W4311091136 cites W2024695456 @default.
• W4311091136 cites W2026018392 @default.
• W4311091136 cites W2055735626 @default.
• W4311091136 cites W2060917856 @default.
• W4311091136 cites W2063200147 @default.
• W4311091136 cites W2074658733 @default.
• W4311091136 cites W2082214402 @default.
• W4311091136 cites W2093840646 @default.
• W4311091136 cites W2095992564 @default.
• W4311091136 cites W2103497845 @default.
• W4311091136 cites W2112516630 @default.
• W4311091136 cites W2126105956 @default.
• W4311091136 cites W2133209872 @default.
• W4311091136 cites W2134284628 @default.
• W4311091136 cites W2142192031 @default.
• W4311091136 cites W2150680082 @default.
• W4311091136 cites W2156385369 @default.
• W4311091136 cites W2159225273 @default.
• W4311091136 cites W2169248607 @default.
• W4311091136 cites W2474205594 @default.
• W4311091136 cites W2555442175 @default.
• W4311091136 cites W2784513399 @default.
• W4311091136 cites W2797373644 @default.
• W4311091136 cites W2809873888 @default.
• W4311091136 cites W2911105719 @default.
• W4311091136 cites W3016516095 @default.
• W4311091136 cites W3103611345 @default.
• W4311091136 cites W3165070676 @default.
• W4311091136 cites W4251588266 @default.
• W4311091136 doi "https://doi.org/10.1016/j.hydroa.2022.100144" @default.
• W4311091136 hasPublicationYear "2022" @default.
• W4311091136 type Work @default.
• W4311091136 citedByCount "0" @default.
• W4311091136 crossrefType "journal-article" @default.
• W4311091136 hasAuthorship W4311091136A5012185198 @default.
• W4311091136 hasAuthorship W4311091136A5017651505 @default.
• W4311091136 hasBestOaLocation W43110911361 @default.
• W4311091136 hasConcept C100834320 @default.
• W4311091136 hasConcept C100970517 @default.
• W4311091136 hasConcept C105795698 @default.
• W4311091136 hasConcept C109007969 @default.
• W4311091136 hasConcept C111368507 @default.
• W4311091136 hasConcept C114793014 @default.
• W4311091136 hasConcept C121332964 @default.
• W4311091136 hasConcept C126645576 @default.
• W4311091136 hasConcept C126691448 @default.
• W4311091136 hasConcept C127313418 @default.
• W4311091136 hasConcept C1276947 @default.
• W4311091136 hasConcept C132651083 @default.
• W4311091136 hasConcept C165838908 @default.
• W4311091136 hasConcept C187320778 @default.
• W4311091136 hasConcept C205649164 @default.
• W4311091136 hasConcept C33923547 @default.
• W4311091136 hasConcept C39432304 @default.
• W4311091136 hasConcept C49204034 @default.
• W4311091136 hasConcept C53739315 @default.
• W4311091136 hasConcept C58640448 @default.
• W4311091136 hasConcept C76886044 @default.
• W4311091136 hasConceptScore W4311091136C100834320 @default.
• W4311091136 hasConceptScore W4311091136C100970517 @default.
• W4311091136 hasConceptScore W4311091136C105795698 @default.
• W4311091136 hasConceptScore W4311091136C109007969 @default.
• W4311091136 hasConceptScore W4311091136C111368507 @default.
• W4311091136 hasConceptScore W4311091136C114793014 @default.
• W4311091136 hasConceptScore W4311091136C121332964 @default.
• W4311091136 hasConceptScore W4311091136C126645576 @default.
• W4311091136 hasConceptScore W4311091136C126691448 @default.
• W4311091136 hasConceptScore W4311091136C127313418 @default.
• W4311091136 hasConceptScore W4311091136C1276947 @default.
• W4311091136 hasConceptScore W4311091136C132651083 @default.
• W4311091136 hasConceptScore W4311091136C165838908 @default.
• W4311091136 hasConceptScore W4311091136C187320778 @default.
• W4311091136 hasConceptScore W4311091136C205649164 @default.
• W4311091136 hasConceptScore W4311091136C33923547 @default.
• W4311091136 hasConceptScore W4311091136C39432304 @default.
• W4311091136 hasConceptScore W4311091136C49204034 @default.

• next