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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Main Authors: Strong, C, Foster, D, Cherkaev, E, Eisenman, I, Golden, KM
Format: Article in Journal/Newspaper
Language:unknown
Published: eScholarship, University of California 2017
Subjects:
Online Access:https://escholarship.org/uc/item/80129095
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record_format openpolar
spelling 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