Development of regional extreme model atmospheres for aerothermodynamic calculations (II)

In an earlier paper (Model Atmospheres (I)), a procedure was developed for determining the most probable vertical temperature profile associated with the occurrence of 1% global temperature extreme at mandatory-pressure levels at stations in North American Arctic. The same technique, based upon a va...

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Main Author: Martin, Frank Lionel
Other Authors: Operations Research (OR), Naval Postgraduate School (U.S.), Graduate School of Operational and Information Sciences (GSOIS)
Format: Report
Language:English
Published: Monterey, California. Naval Postgraduate School 1973
Subjects:
NA
Online Access:https://hdl.handle.net/10945/29250
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spelling ftnavalpschool:oai:calhoun.nps.edu:10945/29250 2024-06-09T07:44:11+00:00 Development of regional extreme model atmospheres for aerothermodynamic calculations (II) Martin, Frank Lionel Operations Research (OR) Naval Postgraduate School (U.S.) Graduate School of Operational and Information Sciences (GSOIS) 1973-07-01 NA application/pdf https://hdl.handle.net/10945/29250 en_US eng Monterey, California. Naval Postgraduate School NPS-51MR73071A NA https://hdl.handle.net/10945/29250 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. NA BRYOZOA--CALIFORNIA--MONTEREY BAY Technical Report 1973 ftnavalpschool 2024-05-15T00:25:03Z In an earlier paper (Model Atmospheres (I)), a procedure was developed for determining the most probable vertical temperature profile associated with the occurrence of 1% global temperature extreme at mandatory-pressure levels at stations in North American Arctic. The same technique, based upon a variation of the stepwise multiple regression procedure was employed in the current study. Whereas the radiosondes investigated in Model Atmospheres (I) consisted entirely of "checked-data" quality, those stations desiagnated for study in this work required a much more refined data-screen, due to lack of initially checked radiosonde report quality. Nevertheless, after application of various acceptability criteria, the radiosondes at each station were arranged in the same format as employed in Model Atmospheres (I). There remained in each case a suitable sample population to provide significant results. The ensuing multiple regression analysis applied to the geographically and climatologically diverse set of stations of the current study led to realistic estimates of the temperature profiles which were conditionally dependent upon the existence of 1% extreme forcing-level temperature TJ at previously designated pressure levels PJ. (Author) NA http://archive.org/details/developmentofreg3071mart Report Arctic Naval Postgraduate School: Calhoun Arctic
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language English
topic NA
BRYOZOA--CALIFORNIA--MONTEREY BAY
spellingShingle NA
BRYOZOA--CALIFORNIA--MONTEREY BAY
Martin, Frank Lionel
Development of regional extreme model atmospheres for aerothermodynamic calculations (II)
topic_facet NA
BRYOZOA--CALIFORNIA--MONTEREY BAY
description In an earlier paper (Model Atmospheres (I)), a procedure was developed for determining the most probable vertical temperature profile associated with the occurrence of 1% global temperature extreme at mandatory-pressure levels at stations in North American Arctic. The same technique, based upon a variation of the stepwise multiple regression procedure was employed in the current study. Whereas the radiosondes investigated in Model Atmospheres (I) consisted entirely of "checked-data" quality, those stations desiagnated for study in this work required a much more refined data-screen, due to lack of initially checked radiosonde report quality. Nevertheless, after application of various acceptability criteria, the radiosondes at each station were arranged in the same format as employed in Model Atmospheres (I). There remained in each case a suitable sample population to provide significant results. The ensuing multiple regression analysis applied to the geographically and climatologically diverse set of stations of the current study led to realistic estimates of the temperature profiles which were conditionally dependent upon the existence of 1% extreme forcing-level temperature TJ at previously designated pressure levels PJ. (Author) NA http://archive.org/details/developmentofreg3071mart
author2 Operations Research (OR)
Naval Postgraduate School (U.S.)
Graduate School of Operational and Information Sciences (GSOIS)
format Report
author Martin, Frank Lionel
author_facet Martin, Frank Lionel
author_sort Martin, Frank Lionel
title Development of regional extreme model atmospheres for aerothermodynamic calculations (II)
title_short Development of regional extreme model atmospheres for aerothermodynamic calculations (II)
title_full Development of regional extreme model atmospheres for aerothermodynamic calculations (II)
title_fullStr Development of regional extreme model atmospheres for aerothermodynamic calculations (II)
title_full_unstemmed Development of regional extreme model atmospheres for aerothermodynamic calculations (II)
title_sort development of regional extreme model atmospheres for aerothermodynamic calculations (ii)
publisher Monterey, California. Naval Postgraduate School
publishDate 1973
url https://hdl.handle.net/10945/29250
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation NPS-51MR73071A
NA
https://hdl.handle.net/10945/29250
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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