FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4322001073> ?p ?o ?g. }

• W4322001073 abstract "Ice shelves around the coastal portion of the Antarctic ice sheet are sensitive indicators of climate change. The thinning of ice shelves diminishes buttressing, promotes longitudinal spreading, and increases ice flux across the grounding line, leading to accelerated glacier discharge into the ocean. Thwaites Glacier in the Amundsen Sea Embayment is one of the fastest-changing outlet glaciers in Antarctica. Damaged areas with densely distributed crevasses and open fractures on Thwaites Glacier are key to future ice shelf stability, grounding line retreat and sea level contribution. The damage feedback processes should be taken into consideration when simulating the evolution of Thwaites Glacier using ice sheet models.Here, we add the continuum damage mechanics approach to the F.ETISh/Kori ice flow model, to simulate the present-day and near future behavior of the ice sheet and ice shelf system, including brittle ice physics. The damage field is described by equating it to the total crevasse depths used in Nick et al. (2010) and Sun et al. (2017). 100 years simulations under present-day climate conditions with and without damage in different scenarios have been conducted, and the change in ice velocity, ice thickness, the grounding line retreat and the sea level contribution of Thwaites Glacier have been analysed. Moreover, the change in ice velocity along four ice flow profiles in the first 20-year simulation has been analysed and the impact of damage on velocity has been assessed by comparing the simulated velocity fields with the observations (e.g., the MEaSUREs and ITS_LIVE ice velocity products).Results indicate that damage drastically increases the ice velocity over the ice shelves and weakens them as such that grounding line retreat ~18 km after 20 years, accelerates (~1.5 times) compared to the observed increase in flow speed and contributes around an order of magnitude to the sea level rise in 50 years. Change in ice velocity profiles of Thwaites Glacier also show that local damage may overestimate ice velocity, especially in the grounded ice near the grounding line, while it underestimates observed ice flow when local damage is omitted. Through a series of further sensitivity experiments, an analysis on the timing and magnitude of damage has been carried out to gauge the current and near future state of the Thwaites glacier basin.&#160;" @default.
• W4322001073 created "2023-02-26" @default.
• W4322001073 creator A5002495146 @default.
• W4322001073 creator A5026118407 @default.
• W4322001073 creator A5030773043 @default.
• W4322001073 creator A5087780695 @default.
• W4322001073 date "2023-05-15" @default.
• W4322001073 modified "2023-09-27" @default.
• W4322001073 title "Modelling the impacts of ice damage on the response of Thwaites Glacier, West Antarctica" @default.
• W4322001073 doi "https://doi.org/10.5194/egusphere-egu23-11798" @default.
• W4322001073 hasPublicationYear "2023" @default.
• W4322001073 type Work @default.
• W4322001073 citedByCount "0" @default.
• W4322001073 crossrefType "posted-content" @default.
• W4322001073 hasAuthorship W4322001073A5002495146 @default.
• W4322001073 hasAuthorship W4322001073A5026118407 @default.
• W4322001073 hasAuthorship W4322001073A5030773043 @default.
• W4322001073 hasAuthorship W4322001073A5087780695 @default.
• W4322001073 hasConcept C100834320 @default.
• W4322001073 hasConcept C104932425 @default.
• W4322001073 hasConcept C114793014 @default.
• W4322001073 hasConcept C123750103 @default.
• W4322001073 hasConcept C127313418 @default.
• W4322001073 hasConcept C136894858 @default.
• W4322001073 hasConcept C146233495 @default.
• W4322001073 hasConcept C16335420 @default.
• W4322001073 hasConcept C171289182 @default.
• W4322001073 hasConcept C174252726 @default.
• W4322001073 hasConcept C197435368 @default.
• W4322001073 hasConcept C24474704 @default.
• W4322001073 hasConcept C2777093003 @default.
• W4322001073 hasConcept C2778744917 @default.
• W4322001073 hasConcept C2780223605 @default.
• W4322001073 hasConcept C49204034 @default.
• W4322001073 hasConcept C81820708 @default.
• W4322001073 hasConcept C87547467 @default.
• W4322001073 hasConceptScore W4322001073C100834320 @default.
• W4322001073 hasConceptScore W4322001073C104932425 @default.
• W4322001073 hasConceptScore W4322001073C114793014 @default.
• W4322001073 hasConceptScore W4322001073C123750103 @default.
• W4322001073 hasConceptScore W4322001073C127313418 @default.
• W4322001073 hasConceptScore W4322001073C136894858 @default.
• W4322001073 hasConceptScore W4322001073C146233495 @default.
• W4322001073 hasConceptScore W4322001073C16335420 @default.
• W4322001073 hasConceptScore W4322001073C171289182 @default.
• W4322001073 hasConceptScore W4322001073C174252726 @default.
• W4322001073 hasConceptScore W4322001073C197435368 @default.
• W4322001073 hasConceptScore W4322001073C24474704 @default.
• W4322001073 hasConceptScore W4322001073C2777093003 @default.
• W4322001073 hasConceptScore W4322001073C2778744917 @default.
• W4322001073 hasConceptScore W4322001073C2780223605 @default.
• W4322001073 hasConceptScore W4322001073C49204034 @default.
• W4322001073 hasConceptScore W4322001073C81820708 @default.
• W4322001073 hasConceptScore W4322001073C87547467 @default.
• W4322001073 hasLocation W43220010731 @default.
• W4322001073 hasOpenAccess W4322001073 @default.
• W4322001073 hasPrimaryLocation W43220010731 @default.
• W4322001073 hasRelatedWork W1661227844 @default.
• W4322001073 hasRelatedWork W1975391852 @default.
• W4322001073 hasRelatedWork W2101029187 @default.
• W4322001073 hasRelatedWork W2159568546 @default.
• W4322001073 hasRelatedWork W4205669974 @default.
• W4322001073 hasRelatedWork W421834462 @default.
• W4322001073 hasRelatedWork W4220789436 @default.
• W4322001073 hasRelatedWork W4224023912 @default.
• W4322001073 hasRelatedWork W4248741606 @default.
• W4322001073 hasRelatedWork W4322001073 @default.
• W4322001073 isParatext "false" @default.
• W4322001073 isRetracted "false" @default.
• W4322001073 workType "article" @default.