Sea Ice Discrete Element Modeling: Melt and Fracture of Floes and Sheets ...

Over the last 40 years, the Arctic Ocean has experienced a significant reduction in surface area and thickness of sea ice for its minimum summer and year-round values. Sea ice, existing both as continuous ice sheets and distinct broken floes or blocks, is disappearing earlier and faster over time. T...

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Main Author: Moncada Lopez, Rigoberto
Format: Thesis
Language:English
Published: California Institute of Technology 2024
Subjects:
Online Access:https://dx.doi.org/10.7907/erqr-cr51
https://resolver.caltech.edu/CaltechTHESIS:07032023-235459528
id ftdatacite:10.7907/erqr-cr51
record_format openpolar
spelling ftdatacite:10.7907/erqr-cr51 2024-01-28T10:03:55+01:00 Sea Ice Discrete Element Modeling: Melt and Fracture of Floes and Sheets ... Moncada Lopez, Rigoberto 2024 PDF https://dx.doi.org/10.7907/erqr-cr51 https://resolver.caltech.edu/CaltechTHESIS:07032023-235459528 en eng California Institute of Technology No commercial reproduction, distribution, display or performance rights in this work are provided. Sea Ice melt FSD. Civil Engineering FOS Civil engineering breakage Discrete Element Method Landfast sea ice sheets Computational geomechanics Floes Text Dissertation Thesis thesis 2024 ftdatacite https://doi.org/10.7907/erqr-cr51 2024-01-04T12:48:56Z Over the last 40 years, the Arctic Ocean has experienced a significant reduction in surface area and thickness of sea ice for its minimum summer and year-round values. Sea ice, existing both as continuous ice sheets and distinct broken floes or blocks, is disappearing earlier and faster over time. These changes are largely occurring within marginal ice zones, where ice is most vulnerable to thermal forcings from the sun, oceans, and atmosphere and wind and ocean currents. Given that sea ice plays a vital role in regulating climate by delaying global energy exchanges, its loss is a vital factor in increasing global temperatures and the frequency of extreme weather events. Understanding and projecting seasonal variations in sea ice is imperative to improve climate predictions. However, many of the processes in sea ice are not fully described by most existing models, due to the limitations of continuum sea ice approaches. As a result the use of discontinuum techniques on sea ice is a very active field. In this ... Thesis Arctic Arctic Ocean Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic Arctic Ocean
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Sea Ice
melt
FSD.
Civil Engineering
FOS Civil engineering
breakage
Discrete Element Method
Landfast sea ice sheets
Computational geomechanics
Floes
spellingShingle Sea Ice
melt
FSD.
Civil Engineering
FOS Civil engineering
breakage
Discrete Element Method
Landfast sea ice sheets
Computational geomechanics
Floes
Moncada Lopez, Rigoberto
Sea Ice Discrete Element Modeling: Melt and Fracture of Floes and Sheets ...
topic_facet Sea Ice
melt
FSD.
Civil Engineering
FOS Civil engineering
breakage
Discrete Element Method
Landfast sea ice sheets
Computational geomechanics
Floes
description Over the last 40 years, the Arctic Ocean has experienced a significant reduction in surface area and thickness of sea ice for its minimum summer and year-round values. Sea ice, existing both as continuous ice sheets and distinct broken floes or blocks, is disappearing earlier and faster over time. These changes are largely occurring within marginal ice zones, where ice is most vulnerable to thermal forcings from the sun, oceans, and atmosphere and wind and ocean currents. Given that sea ice plays a vital role in regulating climate by delaying global energy exchanges, its loss is a vital factor in increasing global temperatures and the frequency of extreme weather events. Understanding and projecting seasonal variations in sea ice is imperative to improve climate predictions. However, many of the processes in sea ice are not fully described by most existing models, due to the limitations of continuum sea ice approaches. As a result the use of discontinuum techniques on sea ice is a very active field. In this ...
format Thesis
author Moncada Lopez, Rigoberto
author_facet Moncada Lopez, Rigoberto
author_sort Moncada Lopez, Rigoberto
title Sea Ice Discrete Element Modeling: Melt and Fracture of Floes and Sheets ...
title_short Sea Ice Discrete Element Modeling: Melt and Fracture of Floes and Sheets ...
title_full Sea Ice Discrete Element Modeling: Melt and Fracture of Floes and Sheets ...
title_fullStr Sea Ice Discrete Element Modeling: Melt and Fracture of Floes and Sheets ...
title_full_unstemmed Sea Ice Discrete Element Modeling: Melt and Fracture of Floes and Sheets ...
title_sort sea ice discrete element modeling: melt and fracture of floes and sheets ...
publisher California Institute of Technology
publishDate 2024
url https://dx.doi.org/10.7907/erqr-cr51
https://resolver.caltech.edu/CaltechTHESIS:07032023-235459528
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
genre_facet Arctic
Arctic Ocean
Sea ice
op_rights No commercial reproduction, distribution, display or performance rights in this work are provided.
op_doi https://doi.org/10.7907/erqr-cr51
_version_ 1789329491379617792