Loading…

Extremal climatic states simulated by a 2-dimensional model: Part II : Different climatic scenarios

Different climatic simulations have been obtained by using a 2-Dim horizontal energy balance model (EBM), which has been constrained to satisfy several extremal principles on dissipation and convection. Moreover, 2 different versions of the model with fixed and variable cloud-cover have been used. T...

Full description

Saved in:
Bibliographic Details
Published in:Tellus. Series A, Dynamic meteorology and oceanography Dynamic meteorology and oceanography, 2000-08, Vol.52 (4), p.440-454
Main Authors: PUJOL, T, LLEBOT, J. E
Format: Article
Language:English
Subjects:
Citations: Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
cited_by cdi_FETCH-LOGICAL-c372t-91a7a58f5a66c07270b648d76ba66c4e77ca7ffacea1de0449568597003fc9123
cites
container_end_page 454
container_issue 4
container_start_page 440
container_title Tellus. Series A, Dynamic meteorology and oceanography
container_volume 52
creator PUJOL, T
LLEBOT, J. E
description Different climatic simulations have been obtained by using a 2-Dim horizontal energy balance model (EBM), which has been constrained to satisfy several extremal principles on dissipation and convection. Moreover, 2 different versions of the model with fixed and variable cloud-cover have been used. The assumption of an extremal type of behaviour for the climatic system can acquire additional support depending on the similarities found with measured data for past conditions as well as with usual projections for possible future scenarios.
doi_str_mv 10.1034/j.1600-0870.2000.00193.x
format article
fullrecord <record><control><sourceid>proquest_csuc_</sourceid><recordid>TN_cdi_csuc_recercat_oai_recercat_cat_2072_209939</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>21508007</sourcerecordid><originalsourceid>FETCH-LOGICAL-c372t-91a7a58f5a66c07270b648d76ba66c4e77ca7ffacea1de0449568597003fc9123</originalsourceid><addsrcrecordid>eNqFUclOBCEUJEYTx-UfOBhv3T7oBfBmXCcx0YOeyRsaEia9KDDJ-PfSOlFvHnjwoKooKEIog5JBVV-sS9YCFCAFlBwASgCmqnK7RxY_B_tkAVxC0daqOSRHMa5hRrXVgpjbbQp2wJ6a3g-YvKExYbKRRj9s-rzq6OqDIuVF5wc7Rj-NGTxMne0v6TOGRJdLeklvvHM22DH90TF2xOCneEIOHPbRnu7mY_J6d_ty_VA8Pt0vr68eC1MJngrFUGAjXYNta0BwAau2lp1oV_NGbYUwKJxDY5F1Fur8mFY2SgBUzijGq2PCvnVN3BgdrLHBYNIT-t9mHjyL56JUpTLn_JvzFqb3jY1JDz4b73sc7bSJmrMGJID4F8gkU1wxloFy5yJMMQbr9FvIPxI-NAM9R6bXek5Gz8noOTL9FZneZurZ7g6MBnsXcDQ-_vLrbEVC9QnvF5Zu</addsrcrecordid><sourcetype>Open Access Repository</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>18192911</pqid></control><display><type>article</type><title>Extremal climatic states simulated by a 2-dimensional model: Part II : Different climatic scenarios</title><source>Taylor &amp; Francis Open Access</source><creator>PUJOL, T ; LLEBOT, J. E</creator><creatorcontrib>PUJOL, T ; LLEBOT, J. E</creatorcontrib><description>Different climatic simulations have been obtained by using a 2-Dim horizontal energy balance model (EBM), which has been constrained to satisfy several extremal principles on dissipation and convection. Moreover, 2 different versions of the model with fixed and variable cloud-cover have been used. The assumption of an extremal type of behaviour for the climatic system can acquire additional support depending on the similarities found with measured data for past conditions as well as with usual projections for possible future scenarios.</description><identifier>ISSN: 0280-6495</identifier><identifier>EISSN: 1600-0870</identifier><identifier>DOI: 10.1034/j.1600-0870.2000.00193.x</identifier><identifier>CODEN: TSAOD8</identifier><language>eng</language><publisher>Oxford: Blackwell</publisher><subject>Atmospheric radiation ; Earth, ocean, space ; Entropia ; Entropy ; Exact sciences and technology ; External geophysics ; Meteorology ; Other topics in atmospheric geophysics ; Radiació atmosfèrica ; Termodinàmica ; Thermodynamic</subject><ispartof>Tellus. Series A, Dynamic meteorology and oceanography, 2000-08, Vol.52 (4), p.440-454</ispartof><rights>2000 INIST-CNRS</rights><rights>Attribution-NonCommercial 3.0 Spain &lt;a href="http://creativecommons.org/licenses/by-nc/3.0/es/"&gt;http://creativecommons.org/licenses/by-nc/3.0/es/&lt;/a&gt;</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c372t-91a7a58f5a66c07270b648d76ba66c4e77ca7ffacea1de0449568597003fc9123</citedby></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,314,777,781,882,27906,27907</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&amp;idt=1408080$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>PUJOL, T</creatorcontrib><creatorcontrib>LLEBOT, J. E</creatorcontrib><title>Extremal climatic states simulated by a 2-dimensional model: Part II : Different climatic scenarios</title><title>Tellus. Series A, Dynamic meteorology and oceanography</title><description>Different climatic simulations have been obtained by using a 2-Dim horizontal energy balance model (EBM), which has been constrained to satisfy several extremal principles on dissipation and convection. Moreover, 2 different versions of the model with fixed and variable cloud-cover have been used. The assumption of an extremal type of behaviour for the climatic system can acquire additional support depending on the similarities found with measured data for past conditions as well as with usual projections for possible future scenarios.</description><subject>Atmospheric radiation</subject><subject>Earth, ocean, space</subject><subject>Entropia</subject><subject>Entropy</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Meteorology</subject><subject>Other topics in atmospheric geophysics</subject><subject>Radiació atmosfèrica</subject><subject>Termodinàmica</subject><subject>Thermodynamic</subject><issn>0280-6495</issn><issn>1600-0870</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2000</creationdate><recordtype>article</recordtype><recordid>eNqFUclOBCEUJEYTx-UfOBhv3T7oBfBmXCcx0YOeyRsaEia9KDDJ-PfSOlFvHnjwoKooKEIog5JBVV-sS9YCFCAFlBwASgCmqnK7RxY_B_tkAVxC0daqOSRHMa5hRrXVgpjbbQp2wJ6a3g-YvKExYbKRRj9s-rzq6OqDIuVF5wc7Rj-NGTxMne0v6TOGRJdLeklvvHM22DH90TF2xOCneEIOHPbRnu7mY_J6d_ty_VA8Pt0vr68eC1MJngrFUGAjXYNta0BwAau2lp1oV_NGbYUwKJxDY5F1Fur8mFY2SgBUzijGq2PCvnVN3BgdrLHBYNIT-t9mHjyL56JUpTLn_JvzFqb3jY1JDz4b73sc7bSJmrMGJID4F8gkU1wxloFy5yJMMQbr9FvIPxI-NAM9R6bXek5Gz8noOTL9FZneZurZ7g6MBnsXcDQ-_vLrbEVC9QnvF5Zu</recordid><startdate>20000801</startdate><enddate>20000801</enddate><creator>PUJOL, T</creator><creator>LLEBOT, J. E</creator><general>Blackwell</general><general>International Meteorological Institute in Stockholm</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>KL.</scope><scope>XX2</scope></search><sort><creationdate>20000801</creationdate><title>Extremal climatic states simulated by a 2-dimensional model: Part II : Different climatic scenarios</title><author>PUJOL, T ; LLEBOT, J. E</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c372t-91a7a58f5a66c07270b648d76ba66c4e77ca7ffacea1de0449568597003fc9123</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2000</creationdate><topic>Atmospheric radiation</topic><topic>Earth, ocean, space</topic><topic>Entropia</topic><topic>Entropy</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Meteorology</topic><topic>Other topics in atmospheric geophysics</topic><topic>Radiació atmosfèrica</topic><topic>Termodinàmica</topic><topic>Thermodynamic</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>PUJOL, T</creatorcontrib><creatorcontrib>LLEBOT, J. E</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Recercat</collection><jtitle>Tellus. Series A, Dynamic meteorology and oceanography</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>PUJOL, T</au><au>LLEBOT, J. E</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Extremal climatic states simulated by a 2-dimensional model: Part II : Different climatic scenarios</atitle><jtitle>Tellus. Series A, Dynamic meteorology and oceanography</jtitle><date>2000-08-01</date><risdate>2000</risdate><volume>52</volume><issue>4</issue><spage>440</spage><epage>454</epage><pages>440-454</pages><issn>0280-6495</issn><eissn>1600-0870</eissn><coden>TSAOD8</coden><abstract>Different climatic simulations have been obtained by using a 2-Dim horizontal energy balance model (EBM), which has been constrained to satisfy several extremal principles on dissipation and convection. Moreover, 2 different versions of the model with fixed and variable cloud-cover have been used. The assumption of an extremal type of behaviour for the climatic system can acquire additional support depending on the similarities found with measured data for past conditions as well as with usual projections for possible future scenarios.</abstract><cop>Oxford</cop><pub>Blackwell</pub><doi>10.1034/j.1600-0870.2000.00193.x</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record>
fulltext fulltext
identifier ISSN: 0280-6495
ispartof Tellus. Series A, Dynamic meteorology and oceanography, 2000-08, Vol.52 (4), p.440-454
issn 0280-6495
1600-0870
language eng
recordid cdi_csuc_recercat_oai_recercat_cat_2072_209939
source Taylor & Francis Open Access
subjects Atmospheric radiation
Earth, ocean, space
Entropia
Entropy
Exact sciences and technology
External geophysics
Meteorology
Other topics in atmospheric geophysics
Radiació atmosfèrica
Termodinàmica
Thermodynamic
title Extremal climatic states simulated by a 2-dimensional model: Part II : Different climatic scenarios
url http://sfxeu10.hosted.exlibrisgroup.com/loughborough?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-17T07%3A50%3A31IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_csuc_&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Extremal%20climatic%20states%20simulated%20by%20a%202-dimensional%20model:%20Part%20II%20:%20Different%20climatic%20scenarios&rft.jtitle=Tellus.%20Series%20A,%20Dynamic%20meteorology%20and%20oceanography&rft.au=PUJOL,%20T&rft.date=2000-08-01&rft.volume=52&rft.issue=4&rft.spage=440&rft.epage=454&rft.pages=440-454&rft.issn=0280-6495&rft.eissn=1600-0870&rft.coden=TSAOD8&rft_id=info:doi/10.1034/j.1600-0870.2000.00193.x&rft_dat=%3Cproquest_csuc_%3E21508007%3C/proquest_csuc_%3E%3Cgrp_id%3Ecdi_FETCH-LOGICAL-c372t-91a7a58f5a66c07270b648d76ba66c4e77ca7ffacea1de0449568597003fc9123%3C/grp_id%3E%3Coa%3E%3C/oa%3E%3Curl%3E%3C/url%3E&rft_id=info:oai/&rft_pqid=18192911&rft_id=info:pmid/&rfr_iscdi=true