The temporal and spatial variability of the marine atmospheric boundary layer and its effect on electromagnetic propagation in and around the Greenland Sea marginal ice zone

Variability of the MABL and its effect on the electromagnetic (EM) refractive structure around the Greenland Sea marginal ice zone were examined. Rawinsonde profiles and surface observations collected from 3 ships during MIZEX-87(20 March-11 April) served as the data set. A program, developed to cal...

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Main Author: Groters, Douglas J.
Other Authors: Shaw, W.J., Naval Postgraduate School (U.S.), Meteorology, Davidson, Kenneth L.
Format: Thesis
Language:English
Published: Monterey, California. Naval Postgraduate School 1988
Subjects:
Online Access:https://hdl.handle.net/10945/23422
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record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/23422 2024-06-09T07:46:20+00:00 The temporal and spatial variability of the marine atmospheric boundary layer and its effect on electromagnetic propagation in and around the Greenland Sea marginal ice zone Groters, Douglas J. Shaw, W.J. Naval Postgraduate School (U.S.) Meteorology Davidson, Kenneth L. 1988-06 application/pdf https://hdl.handle.net/10945/23422 en_US eng Monterey, California. Naval Postgraduate School https://hdl.handle.net/10945/23422 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. Air water interactions Greenland Sea Atmospheric refraction Electromagnetic wave propagation Heat flux Sea ice Theses Meteorology Thesis 1988 ftnavalpschool 2024-05-15T00:53:53Z Variability of the MABL and its effect on the electromagnetic (EM) refractive structure around the Greenland Sea marginal ice zone were examined. Rawinsonde profiles and surface observations collected from 3 ships during MIZEX-87(20 March-11 April) served as the data set. A program, developed to calculate the refractivity at each vertical level of the rawinsonde profiles, also identified the levels at which trapping, superrefraction and subrefraction occurred. Temporal studies showed that a higher incidence of anomalous refractive layers occurred during periods when the region was under the influence of high pressure. More than 50% of the time, trapping and super-refractive layers were attributed to development of a capping inversion just above the MABL during these periods. Spatial studies showed that the refractive structure varied relative to distance from the ice edge as did the depth of the MABL. An upward slope in refractive layer heights was observed from the ice toward the open water. Significant spatial inhomogeneity was observed over horizontal ranges of less than 100 km. This was attributed to both the large-scale synoptic forcing affecting the region and to variations in the surface fluxes of heat and moisture over the ice and over the water. A range-dependent ray trace model developed at the Naval Ocean Systems Center was used to show how the ray paths of EM waves vary with a changing refractive structures. Keywords: Air water interactions, Greenland Sea, Atmospheric refraction, Electromagnetic wave propagation, Heat flux, Sea ice. Theses. (EDC) Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/thetemporalndspa1094523422 Thesis Greenland Greenland Sea Sea ice Naval Postgraduate School: Calhoun Greenland
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language English
topic Air water interactions
Greenland Sea
Atmospheric refraction
Electromagnetic wave propagation
Heat flux
Sea ice
Theses
Meteorology
spellingShingle Air water interactions
Greenland Sea
Atmospheric refraction
Electromagnetic wave propagation
Heat flux
Sea ice
Theses
Meteorology
Groters, Douglas J.
The temporal and spatial variability of the marine atmospheric boundary layer and its effect on electromagnetic propagation in and around the Greenland Sea marginal ice zone
topic_facet Air water interactions
Greenland Sea
Atmospheric refraction
Electromagnetic wave propagation
Heat flux
Sea ice
Theses
Meteorology
description Variability of the MABL and its effect on the electromagnetic (EM) refractive structure around the Greenland Sea marginal ice zone were examined. Rawinsonde profiles and surface observations collected from 3 ships during MIZEX-87(20 March-11 April) served as the data set. A program, developed to calculate the refractivity at each vertical level of the rawinsonde profiles, also identified the levels at which trapping, superrefraction and subrefraction occurred. Temporal studies showed that a higher incidence of anomalous refractive layers occurred during periods when the region was under the influence of high pressure. More than 50% of the time, trapping and super-refractive layers were attributed to development of a capping inversion just above the MABL during these periods. Spatial studies showed that the refractive structure varied relative to distance from the ice edge as did the depth of the MABL. An upward slope in refractive layer heights was observed from the ice toward the open water. Significant spatial inhomogeneity was observed over horizontal ranges of less than 100 km. This was attributed to both the large-scale synoptic forcing affecting the region and to variations in the surface fluxes of heat and moisture over the ice and over the water. A range-dependent ray trace model developed at the Naval Ocean Systems Center was used to show how the ray paths of EM waves vary with a changing refractive structures. Keywords: Air water interactions, Greenland Sea, Atmospheric refraction, Electromagnetic wave propagation, Heat flux, Sea ice. Theses. (EDC) Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/thetemporalndspa1094523422
author2 Shaw, W.J.
Naval Postgraduate School (U.S.)
Meteorology
Davidson, Kenneth L.
format Thesis
author Groters, Douglas J.
author_facet Groters, Douglas J.
author_sort Groters, Douglas J.
title The temporal and spatial variability of the marine atmospheric boundary layer and its effect on electromagnetic propagation in and around the Greenland Sea marginal ice zone
title_short The temporal and spatial variability of the marine atmospheric boundary layer and its effect on electromagnetic propagation in and around the Greenland Sea marginal ice zone
title_full The temporal and spatial variability of the marine atmospheric boundary layer and its effect on electromagnetic propagation in and around the Greenland Sea marginal ice zone
title_fullStr The temporal and spatial variability of the marine atmospheric boundary layer and its effect on electromagnetic propagation in and around the Greenland Sea marginal ice zone
title_full_unstemmed The temporal and spatial variability of the marine atmospheric boundary layer and its effect on electromagnetic propagation in and around the Greenland Sea marginal ice zone
title_sort temporal and spatial variability of the marine atmospheric boundary layer and its effect on electromagnetic propagation in and around the greenland sea marginal ice zone
publisher Monterey, California. Naval Postgraduate School
publishDate 1988
url https://hdl.handle.net/10945/23422
geographic Greenland
geographic_facet Greenland
genre Greenland
Greenland Sea
Sea ice
genre_facet Greenland
Greenland Sea
Sea ice
op_relation https://hdl.handle.net/10945/23422
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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