High latitude coupled sea-ice-air thermodynamics

Presently ice extent forecast models such as the U.S. Navy Polar Ice Prediction System (PIPS) neglect or treat small-scale thermodynamic processes and entrainment unrealistically. Incorporating better algorithms that include more complete physics of the mixed layer dynamics will allow for improved p...

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Bibliographic Details
Main Author: Swick, William A.
Other Authors: Garwood, Roland W., Naval Postgraduate School (U.S.)., Oceanography, Guest, Arlene
Format: Thesis
Language:unknown
Published: Monterey, California. Naval Postgraduate School 2004
Subjects:
Ice
Online Access:https://hdl.handle.net/10945/1328
id ftnavalpschool:oai:calhoun.nps.edu:10945/1328
record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/1328 2024-06-09T07:43:53+00:00 High latitude coupled sea-ice-air thermodynamics Swick, William A. Garwood, Roland W. Naval Postgraduate School (U.S.). Oceanography Guest, Arlene 2004-09 xiv, 75 p. : col. ill., col. maps application/pdf https://hdl.handle.net/10945/1328 unknown Monterey, California. Naval Postgraduate School https://hdl.handle.net/10945/1328 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. Thermodynamics Ice Arctic regions Greenland Thesis 2004 ftnavalpschool 2024-05-15T00:46:59Z Presently ice extent forecast models such as the U.S. Navy Polar Ice Prediction System (PIPS) neglect or treat small-scale thermodynamic processes and entrainment unrealistically. Incorporating better algorithms that include more complete physics of the mixed layer dynamics will allow for improved prediction of ice thickness and distribution, open water boundaries, polynyas, and deep-water formation in the polar seas. A one-dimensional mixed layer turbulent kinetic energy (TKE) budget model based on Garwood's NPS mixed layer model for deep convection (Garwood, 1991) was written in MATLAB. The model consisted of a system of ten equations derived by vertically integrating the budgets for heat, momentum, salinity, and turbulent kinetic energy between the sea-ice-air interface and the base of the turbulent mixed layer. The NPS mixed layer model was tested using atmospheric forcing and ocean profiles collected at the Surface Heat Budget of the Arctic Ocean Experiment (SHEBA) site. Sensitivity studies using ocean profiles of the Greenland Sea were also conducted to address thermodynamics and ocean profiles that enhance thermohaline circulation. Findings and results as well as recommendations for further study are addressed to extend the relationships determined from small 1-D scales to the larger 3-D scales suitable for improvements to current ice models. Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/highlatitudecoup109451328 Thesis Arctic Arctic Ocean Greenland Greenland Sea Sea ice Surface Heat Budget of the Arctic Ocean Naval Postgraduate School: Calhoun Arctic Arctic Ocean Garwood ENVELOPE(164.283,164.283,-78.033,-78.033) Greenland
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language unknown
topic Thermodynamics
Ice
Arctic regions
Greenland
spellingShingle Thermodynamics
Ice
Arctic regions
Greenland
Swick, William A.
High latitude coupled sea-ice-air thermodynamics
topic_facet Thermodynamics
Ice
Arctic regions
Greenland
description Presently ice extent forecast models such as the U.S. Navy Polar Ice Prediction System (PIPS) neglect or treat small-scale thermodynamic processes and entrainment unrealistically. Incorporating better algorithms that include more complete physics of the mixed layer dynamics will allow for improved prediction of ice thickness and distribution, open water boundaries, polynyas, and deep-water formation in the polar seas. A one-dimensional mixed layer turbulent kinetic energy (TKE) budget model based on Garwood's NPS mixed layer model for deep convection (Garwood, 1991) was written in MATLAB. The model consisted of a system of ten equations derived by vertically integrating the budgets for heat, momentum, salinity, and turbulent kinetic energy between the sea-ice-air interface and the base of the turbulent mixed layer. The NPS mixed layer model was tested using atmospheric forcing and ocean profiles collected at the Surface Heat Budget of the Arctic Ocean Experiment (SHEBA) site. Sensitivity studies using ocean profiles of the Greenland Sea were also conducted to address thermodynamics and ocean profiles that enhance thermohaline circulation. Findings and results as well as recommendations for further study are addressed to extend the relationships determined from small 1-D scales to the larger 3-D scales suitable for improvements to current ice models. Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/highlatitudecoup109451328
author2 Garwood, Roland W.
Naval Postgraduate School (U.S.).
Oceanography
Guest, Arlene
format Thesis
author Swick, William A.
author_facet Swick, William A.
author_sort Swick, William A.
title High latitude coupled sea-ice-air thermodynamics
title_short High latitude coupled sea-ice-air thermodynamics
title_full High latitude coupled sea-ice-air thermodynamics
title_fullStr High latitude coupled sea-ice-air thermodynamics
title_full_unstemmed High latitude coupled sea-ice-air thermodynamics
title_sort high latitude coupled sea-ice-air thermodynamics
publisher Monterey, California. Naval Postgraduate School
publishDate 2004
url https://hdl.handle.net/10945/1328
long_lat ENVELOPE(164.283,164.283,-78.033,-78.033)
geographic Arctic
Arctic Ocean
Garwood
Greenland
geographic_facet Arctic
Arctic Ocean
Garwood
Greenland
genre Arctic
Arctic Ocean
Greenland
Greenland Sea
Sea ice
Surface Heat Budget of the Arctic Ocean
genre_facet Arctic
Arctic Ocean
Greenland
Greenland Sea
Sea ice
Surface Heat Budget of the Arctic Ocean
op_relation https://hdl.handle.net/10945/1328
op_rights This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
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