On the definition of marginal ice zone width
Sea ice features a dense inner pack ice zone surrounded by a marginal ice zone (MIZ) in which the sea ice properties are modified by interaction with the ice-free open ocean. The width of the MIZ is a fundamental length scale for polar physical and biological dynamics. Several different criteria for...
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ftcdlib:oai:escholarship.org/ark:/13030/qt80129095 2023-05-15T15:11:21+02:00 On the definition of marginal ice zone width Strong, C Foster, D Cherkaev, E Eisenman, I Golden, KM 1565 - 1584 2017-07-01 application/pdf https://escholarship.org/uc/item/80129095 unknown eScholarship, University of California qt80129095 https://escholarship.org/uc/item/80129095 public Journal of Atmospheric and Oceanic Technology, vol 34, iss 7 Meteorology & Atmospheric Sciences Atmospheric Sciences Oceanography Maritime Engineering article 2017 ftcdlib 2021-04-16T07:10:28Z Sea ice features a dense inner pack ice zone surrounded by a marginal ice zone (MIZ) in which the sea ice properties are modified by interaction with the ice-free open ocean. The width of the MIZ is a fundamental length scale for polar physical and biological dynamics. Several different criteria for establishing MIZ boundaries have emerged in the literature-wave penetration, floe size, sea ice concentration, etc.-and a variety of definitions for the width between the MIZ boundaries have been published. Here, three desirable mathematical properties for defining MIZ width are proposed: invariance with respect to translation and rotation on the sphere; uniqueness at every point in the MIZ; and generality, including nonconvex shapes. The previously published streamline definition is shown to satisfy all three properties, where width is defined as the arc length of a streamline through the solution to Laplaces's equation within the MIZ boundaries, while other published definitions each satisfy only one of the desired properties. When defining MIZ spatial average width from streamline results, the rationale for averaging with respect to distance along both MIZ boundaries was left implicit in prior studies. Here it is made rigorous by developing and applying the mathematics of an analytically tractable idealization of MIZ geometry-the eccentric annulus. Finally, satellite-retrieved Arctic sea ice concentrations are used to investigate how well streamline-based MIZ spatial average width is approximated by alternative definitions that lack desirable mathematical properties or local width values but offer computational efficiency. Article in Journal/Newspaper Arctic Sea ice University of California: eScholarship Arctic |
institution |
Open Polar |
collection |
University of California: eScholarship |
op_collection_id |
ftcdlib |
language |
unknown |
topic |
Meteorology & Atmospheric Sciences Atmospheric Sciences Oceanography Maritime Engineering |
spellingShingle |
Meteorology & Atmospheric Sciences Atmospheric Sciences Oceanography Maritime Engineering Strong, C Foster, D Cherkaev, E Eisenman, I Golden, KM On the definition of marginal ice zone width |
topic_facet |
Meteorology & Atmospheric Sciences Atmospheric Sciences Oceanography Maritime Engineering |
description |
Sea ice features a dense inner pack ice zone surrounded by a marginal ice zone (MIZ) in which the sea ice properties are modified by interaction with the ice-free open ocean. The width of the MIZ is a fundamental length scale for polar physical and biological dynamics. Several different criteria for establishing MIZ boundaries have emerged in the literature-wave penetration, floe size, sea ice concentration, etc.-and a variety of definitions for the width between the MIZ boundaries have been published. Here, three desirable mathematical properties for defining MIZ width are proposed: invariance with respect to translation and rotation on the sphere; uniqueness at every point in the MIZ; and generality, including nonconvex shapes. The previously published streamline definition is shown to satisfy all three properties, where width is defined as the arc length of a streamline through the solution to Laplaces's equation within the MIZ boundaries, while other published definitions each satisfy only one of the desired properties. When defining MIZ spatial average width from streamline results, the rationale for averaging with respect to distance along both MIZ boundaries was left implicit in prior studies. Here it is made rigorous by developing and applying the mathematics of an analytically tractable idealization of MIZ geometry-the eccentric annulus. Finally, satellite-retrieved Arctic sea ice concentrations are used to investigate how well streamline-based MIZ spatial average width is approximated by alternative definitions that lack desirable mathematical properties or local width values but offer computational efficiency. |
format |
Article in Journal/Newspaper |
author |
Strong, C Foster, D Cherkaev, E Eisenman, I Golden, KM |
author_facet |
Strong, C Foster, D Cherkaev, E Eisenman, I Golden, KM |
author_sort |
Strong, C |
title |
On the definition of marginal ice zone width |
title_short |
On the definition of marginal ice zone width |
title_full |
On the definition of marginal ice zone width |
title_fullStr |
On the definition of marginal ice zone width |
title_full_unstemmed |
On the definition of marginal ice zone width |
title_sort |
on the definition of marginal ice zone width |
publisher |
eScholarship, University of California |
publishDate |
2017 |
url |
https://escholarship.org/uc/item/80129095 |
op_coverage |
1565 - 1584 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_source |
Journal of Atmospheric and Oceanic Technology, vol 34, iss 7 |
op_relation |
qt80129095 https://escholarship.org/uc/item/80129095 |
op_rights |
public |
_version_ |
1766342224196403200 |