Loading…

A Comparison of Several Meteorological Analysis Schemes over a Data-Rich Region

Among the many ways of comparing meteorological analyses, two are considered: their ability to fit the contours to observed data, and to portray accurately the amplitude and position of synoptic-scale waves. Four analysis methods are investigated in a data-rich area: the National Meteorological Cent...

Full description

Saved in:
Bibliographic Details
Published in:Monthly weather review 1977-09, Vol.105 (9), p.1083-1091
Main Authors: Otto-Bliesner, Bette, Baumhefner, David P., Schlatter, Thomas W., Bleck, Rainer
Format: Article
Language:English
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by
cites
container_end_page 1091
container_issue 9
container_start_page 1083
container_title Monthly weather review
container_volume 105
creator Otto-Bliesner, Bette
Baumhefner, David P.
Schlatter, Thomas W.
Bleck, Rainer
description Among the many ways of comparing meteorological analyses, two are considered: their ability to fit the contours to observed data, and to portray accurately the amplitude and position of synoptic-scale waves. Four analysis methods are investigated in a data-rich area: the National Meteorological Center (NMC) operational, successive-correction, objective analysis; a global statistical multivariate analysis; an isentropic analysis; and a hand-analyzed, subjective analysis. Analyses of wind and height for Dec. 11-14, 1967, are compared on mandatory pressure surfaces. The individual analyses show minor differences in the positions and intensities of synoptic-scale meteorological features, in gradients, and in the smoothing of the data. Most differences are explained in terms of the computational methods used by each analysis scheme. The NMC, isentropic, and multivariate schemes fit the station data more closely than the subjective analyses. On the basis of these comparisons, it is not possible to distinguish among the performances of the three objective analyses in a data-rich area.
doi_str_mv 10.1175/1520-0493(1977)105<1083:acosma>2.0.co;2
format article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_22791752</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>18444485</sourcerecordid><originalsourceid>FETCH-LOGICAL-c342t-8e0a1343ed0de404762262936adc3c0bda7868dd53a6b26cf01f6559c61e5f553</originalsourceid><addsrcrecordid>eNqFkE1Lw0AURQdRsFb_w6xEF2nffCZREULUKrQEWl0P08mkjSSZmkmF_nsTKm59m8u7HO7iIDQlMCEkFFMiKATAY3ZD4jC8JSAeCETsThvna_1IJzAx7p6eoNEfeYpGADQMQHJ-ji68_wQAKTkdoSzBqat3ui29a7Ar8Mp-21ZXeGE761pXuU1p-jdpdHXwpccrs7W19dj1GNb4SXc6WJZmi5d2U7rmEp0VuvL26jfH6OPl-T19DebZ7C1N5oFhnHZBZEETxpnNIbcceCgplTRmUueGGVjnOoxklOeCabmm0hRACilEbCSxohCCjdH1cXfXuq-99Z2qS29sVenGur1XlIZxb4v-C5KI9xcNi7MjaFrnfWsLtWvLWrcHRUAN5tXgUw0-1WC-r_uqN6-SNFstEkUVqDRTlP0AIFl59Q</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>18444485</pqid></control><display><type>article</type><title>A Comparison of Several Meteorological Analysis Schemes over a Data-Rich Region</title><source>EZB Free E-Journals</source><creator>Otto-Bliesner, Bette ; Baumhefner, David P. ; Schlatter, Thomas W. ; Bleck, Rainer</creator><creatorcontrib>Otto-Bliesner, Bette ; Baumhefner, David P. ; Schlatter, Thomas W. ; Bleck, Rainer</creatorcontrib><description>Among the many ways of comparing meteorological analyses, two are considered: their ability to fit the contours to observed data, and to portray accurately the amplitude and position of synoptic-scale waves. Four analysis methods are investigated in a data-rich area: the National Meteorological Center (NMC) operational, successive-correction, objective analysis; a global statistical multivariate analysis; an isentropic analysis; and a hand-analyzed, subjective analysis. Analyses of wind and height for Dec. 11-14, 1967, are compared on mandatory pressure surfaces. The individual analyses show minor differences in the positions and intensities of synoptic-scale meteorological features, in gradients, and in the smoothing of the data. Most differences are explained in terms of the computational methods used by each analysis scheme. The NMC, isentropic, and multivariate schemes fit the station data more closely than the subjective analyses. On the basis of these comparisons, it is not possible to distinguish among the performances of the three objective analyses in a data-rich area.</description><identifier>ISSN: 0027-0644</identifier><identifier>EISSN: 1520-0493</identifier><identifier>DOI: 10.1175/1520-0493(1977)105&lt;1083:acosma&gt;2.0.co;2</identifier><language>eng</language><ispartof>Monthly weather review, 1977-09, Vol.105 (9), p.1083-1091</ispartof><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>314,780,784,27924,27925</link.rule.ids></links><search><creatorcontrib>Otto-Bliesner, Bette</creatorcontrib><creatorcontrib>Baumhefner, David P.</creatorcontrib><creatorcontrib>Schlatter, Thomas W.</creatorcontrib><creatorcontrib>Bleck, Rainer</creatorcontrib><title>A Comparison of Several Meteorological Analysis Schemes over a Data-Rich Region</title><title>Monthly weather review</title><description>Among the many ways of comparing meteorological analyses, two are considered: their ability to fit the contours to observed data, and to portray accurately the amplitude and position of synoptic-scale waves. Four analysis methods are investigated in a data-rich area: the National Meteorological Center (NMC) operational, successive-correction, objective analysis; a global statistical multivariate analysis; an isentropic analysis; and a hand-analyzed, subjective analysis. Analyses of wind and height for Dec. 11-14, 1967, are compared on mandatory pressure surfaces. The individual analyses show minor differences in the positions and intensities of synoptic-scale meteorological features, in gradients, and in the smoothing of the data. Most differences are explained in terms of the computational methods used by each analysis scheme. The NMC, isentropic, and multivariate schemes fit the station data more closely than the subjective analyses. On the basis of these comparisons, it is not possible to distinguish among the performances of the three objective analyses in a data-rich area.</description><issn>0027-0644</issn><issn>1520-0493</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1977</creationdate><recordtype>article</recordtype><recordid>eNqFkE1Lw0AURQdRsFb_w6xEF2nffCZREULUKrQEWl0P08mkjSSZmkmF_nsTKm59m8u7HO7iIDQlMCEkFFMiKATAY3ZD4jC8JSAeCETsThvna_1IJzAx7p6eoNEfeYpGADQMQHJ-ji68_wQAKTkdoSzBqat3ui29a7Ar8Mp-21ZXeGE761pXuU1p-jdpdHXwpccrs7W19dj1GNb4SXc6WJZmi5d2U7rmEp0VuvL26jfH6OPl-T19DebZ7C1N5oFhnHZBZEETxpnNIbcceCgplTRmUueGGVjnOoxklOeCabmm0hRACilEbCSxohCCjdH1cXfXuq-99Z2qS29sVenGur1XlIZxb4v-C5KI9xcNi7MjaFrnfWsLtWvLWrcHRUAN5tXgUw0-1WC-r_uqN6-SNFstEkUVqDRTlP0AIFl59Q</recordid><startdate>19770901</startdate><enddate>19770901</enddate><creator>Otto-Bliesner, Bette</creator><creator>Baumhefner, David P.</creator><creator>Schlatter, Thomas W.</creator><creator>Bleck, Rainer</creator><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>8FD</scope><scope>H8D</scope><scope>L7M</scope></search><sort><creationdate>19770901</creationdate><title>A Comparison of Several Meteorological Analysis Schemes over a Data-Rich Region</title><author>Otto-Bliesner, Bette ; Baumhefner, David P. ; Schlatter, Thomas W. ; Bleck, Rainer</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c342t-8e0a1343ed0de404762262936adc3c0bda7868dd53a6b26cf01f6559c61e5f553</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1977</creationdate><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Otto-Bliesner, Bette</creatorcontrib><creatorcontrib>Baumhefner, David P.</creatorcontrib><creatorcontrib>Schlatter, Thomas W.</creatorcontrib><creatorcontrib>Bleck, Rainer</creatorcontrib><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Technology Research Database</collection><collection>Aerospace Database</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Monthly weather review</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Otto-Bliesner, Bette</au><au>Baumhefner, David P.</au><au>Schlatter, Thomas W.</au><au>Bleck, Rainer</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A Comparison of Several Meteorological Analysis Schemes over a Data-Rich Region</atitle><jtitle>Monthly weather review</jtitle><date>1977-09-01</date><risdate>1977</risdate><volume>105</volume><issue>9</issue><spage>1083</spage><epage>1091</epage><pages>1083-1091</pages><issn>0027-0644</issn><eissn>1520-0493</eissn><abstract>Among the many ways of comparing meteorological analyses, two are considered: their ability to fit the contours to observed data, and to portray accurately the amplitude and position of synoptic-scale waves. Four analysis methods are investigated in a data-rich area: the National Meteorological Center (NMC) operational, successive-correction, objective analysis; a global statistical multivariate analysis; an isentropic analysis; and a hand-analyzed, subjective analysis. Analyses of wind and height for Dec. 11-14, 1967, are compared on mandatory pressure surfaces. The individual analyses show minor differences in the positions and intensities of synoptic-scale meteorological features, in gradients, and in the smoothing of the data. Most differences are explained in terms of the computational methods used by each analysis scheme. The NMC, isentropic, and multivariate schemes fit the station data more closely than the subjective analyses. On the basis of these comparisons, it is not possible to distinguish among the performances of the three objective analyses in a data-rich area.</abstract><doi>10.1175/1520-0493(1977)105&lt;1083:acosma&gt;2.0.co;2</doi><tpages>9</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0027-0644
ispartof Monthly weather review, 1977-09, Vol.105 (9), p.1083-1091
issn 0027-0644
1520-0493
language eng
recordid cdi_proquest_miscellaneous_22791752
source EZB Free E-Journals
title A Comparison of Several Meteorological Analysis Schemes over a Data-Rich Region
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2024-12-29T15%3A19%3A15IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=A%20Comparison%20of%20Several%20Meteorological%20Analysis%20Schemes%20over%20a%20Data-Rich%20Region&rft.jtitle=Monthly%20weather%20review&rft.au=Otto-Bliesner,%20Bette&rft.date=1977-09-01&rft.volume=105&rft.issue=9&rft.spage=1083&rft.epage=1091&rft.pages=1083-1091&rft.issn=0027-0644&rft.eissn=1520-0493&rft_id=info:doi/10.1175/1520-0493(1977)105%3C1083:acosma%3E2.0.co;2&rft_dat=%3Cproquest_cross%3E18444485%3C/proquest_cross%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c342t-8e0a1343ed0de404762262936adc3c0bda7868dd53a6b26cf01f6559c61e5f553%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=18444485&rft_id=info:pmid/&rfr_iscdi=true