FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4322007216> ?p ?o ?g. }

• W4322007216 abstract "For more than a century, a major focus of Quaternary research has been the investigation of glacier advances and retreats during ice age cycles. The cradle for these studies are the European Alps. In recent years, glacier modelling permitted to produce long-term transient simulations of the European Alps glacier evolution. However, only sparse empirical data, e.g. geological reconstructions of glacier margins in the foreland of the Alps of the Last Glacial Maximum, are available to validate these simulations.Speleothems from the Alps are a widespread palaeoclimate archive. They provide stable carbon isotope records, which can potentially inform about soil and vegetation conditions above a cave site but also about the lack of soil during times of glacier coverage. In addition, speleothem growth in cold, high-elevation cave sites during glacials are a strong indicator of temperatures in the soil-karst-cave system above the freezing point, which is only likely to occur if the cave is covered by a temperate glacier. We here utilise existing speleothem data (growth histories and stable carbon isotopes) from Alpine caves to infer glacier coverage and thermo-dynamical state during the last glacial cycle and to assess the compatibility with modelled reconstructions. We compare data from the last glacial cycle from multiple cave sites located at different elevations (785 to 2319 m a.s.l.) in the Alps with simulations obtained with the Parallel Ice Sheet Model (PISM). We find a general agreement between speleothem-derived soil presence or absence and modelled glacier coverage. However, the speleothem data provide evidence of temperate glacier coverage which is not shown by all of the PISM simulations. Our work demonstrates the value of speleothem-based reconstructions from the Alps as proxies for assessing performance of palaeo-ice flow models." @default.
• W4322007216 created "2023-02-26" @default.
• W4322007216 creator A5015889339 @default.
• W4322007216 creator A5058543819 @default.
• W4322007216 creator A5068013521 @default.
• W4322007216 creator A5082084192 @default.
• W4322007216 date "2023-05-15" @default.
• W4322007216 modified "2023-09-29" @default.
• W4322007216 title "Speleothem growth and stable carbon isotopes as proxies of last glacial glacier coverage and thermo-dynamical states in the Alps" @default.
• W4322007216 doi "https://doi.org/10.5194/egusphere-egu23-8194" @default.
• W4322007216 hasPublicationYear "2023" @default.
• W4322007216 type Work @default.
• W4322007216 citedByCount "0" @default.
• W4322007216 crossrefType "posted-content" @default.
• W4322007216 hasAuthorship W4322007216A5015889339 @default.
• W4322007216 hasAuthorship W4322007216A5058543819 @default.
• W4322007216 hasAuthorship W4322007216A5068013521 @default.
• W4322007216 hasAuthorship W4322007216A5082084192 @default.
• W4322007216 hasConcept C100834320 @default.
• W4322007216 hasConcept C100970517 @default.
• W4322007216 hasConcept C114793014 @default.
• W4322007216 hasConcept C127313418 @default.
• W4322007216 hasConcept C151730666 @default.
• W4322007216 hasConcept C15739521 @default.
• W4322007216 hasConcept C166957645 @default.
• W4322007216 hasConcept C171878925 @default.
• W4322007216 hasConcept C182348080 @default.
• W4322007216 hasConcept C188291805 @default.
• W4322007216 hasConcept C205649164 @default.
• W4322007216 hasConcept C2778883040 @default.
• W4322007216 hasConcept C49204034 @default.
• W4322007216 hasConceptScore W4322007216C100834320 @default.
• W4322007216 hasConceptScore W4322007216C100970517 @default.
• W4322007216 hasConceptScore W4322007216C114793014 @default.
• W4322007216 hasConceptScore W4322007216C127313418 @default.
• W4322007216 hasConceptScore W4322007216C151730666 @default.
• W4322007216 hasConceptScore W4322007216C15739521 @default.
• W4322007216 hasConceptScore W4322007216C166957645 @default.
• W4322007216 hasConceptScore W4322007216C171878925 @default.
• W4322007216 hasConceptScore W4322007216C182348080 @default.
• W4322007216 hasConceptScore W4322007216C188291805 @default.
• W4322007216 hasConceptScore W4322007216C205649164 @default.
• W4322007216 hasConceptScore W4322007216C2778883040 @default.
• W4322007216 hasConceptScore W4322007216C49204034 @default.
• W4322007216 hasLocation W43220072161 @default.
• W4322007216 hasOpenAccess W4322007216 @default.
• W4322007216 hasPrimaryLocation W43220072161 @default.
• W4322007216 hasRelatedWork W2004162475 @default.
• W4322007216 hasRelatedWork W2183528172 @default.
• W4322007216 hasRelatedWork W2966111903 @default.
• W4322007216 hasRelatedWork W3007921656 @default.
• W4322007216 hasRelatedWork W3091316352 @default.
• W4322007216 hasRelatedWork W3215408053 @default.
• W4322007216 hasRelatedWork W357902498 @default.
• W4322007216 hasRelatedWork W4210276771 @default.
• W4322007216 hasRelatedWork W640366666 @default.
• W4322007216 hasRelatedWork W2188660403 @default.
• W4322007216 isParatext "false" @default.
• W4322007216 isRetracted "false" @default.
• W4322007216 workType "article" @default.