南半球对流层中部大气环流的若干特点

P434.2; 分析了南半球对流层500hPa平均地转西风随纬度的分布特点,平均地转西风季节变化特点,计算分析了南半球位势高度对纬向平均的偏差,分析了超长波的分布特征.以上结果均与北半球同期计算结果作了对比比较,指出了南北半球大气环流的异同点....

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Re dai qi xiang xue bao 2000, Vol.16 (2), p.155-163
1. Verfasser: 曲维政 金华
Format: Artikel
Sprache:chi
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 163
container_issue 2
container_start_page 155
container_title Re dai qi xiang xue bao
container_volume 16
creator 曲维政 金华
description P434.2; 分析了南半球对流层500hPa平均地转西风随纬度的分布特点,平均地转西风季节变化特点,计算分析了南半球位势高度对纬向平均的偏差,分析了超长波的分布特征.以上结果均与北半球同期计算结果作了对比比较,指出了南北半球大气环流的异同点.
doi_str_mv 10.3969/j.issn.1004-4965.2000.02.008
format Article
fullrecord <record><control><sourceid>wanfang_jour_chong</sourceid><recordid>TN_cdi_wanfang_journals_rdqxxb200002008</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><cqvip_id>4155818</cqvip_id><wanfj_id>rdqxxb200002008</wanfj_id><sourcerecordid>rdqxxb200002008</sourcerecordid><originalsourceid>FETCH-LOGICAL-c588-1322c7f4eeede175f15354f00a8dc3dfe2427ffc1c8656581213b20de5139b883</originalsourceid><addsrcrecordid>eNo9j81Kw0AUhWehYKl9CEFwlfHOXzJZSvEPCm66D8lkpqaWlDaI3dq6UWlxIQiuFd1IVRDM-ziNvoUJFTf3wrkf55yL0CYBzHzX3-7iJMtSTAC4w31XYAoAGCgGkCuo9q-voUaWJVF5lC7l1KshZqd3dnpV3EzsPF98nNu38dfny8_k2T48LV5vi9m8FIv7i-_rR5u_F5d5Mc7X0aoJe5lu_O06au_ttpsHTuto_7C503KUkNIhjFLlGa61jjXxhCGCCW4AQhkrFhtdFTBGESVd4QpJKGERhVgLwvxISlZHW0vbszA1YdoJuv3TYVoGBsN4MBpF1Y9QjorcWJLquJ92BknJRqE6MUlPB5yI0luyX2PGZag</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype></control><display><type>article</type><title>南半球对流层中部大气环流的若干特点</title><source>Alma/SFX Local Collection</source><creator>曲维政 金华</creator><creatorcontrib>曲维政 金华</creatorcontrib><description>P434.2; 分析了南半球对流层500hPa平均地转西风随纬度的分布特点,平均地转西风季节变化特点,计算分析了南半球位势高度对纬向平均的偏差,分析了超长波的分布特征.以上结果均与北半球同期计算结果作了对比比较,指出了南北半球大气环流的异同点.</description><identifier>ISSN: 1004-4965</identifier><identifier>DOI: 10.3969/j.issn.1004-4965.2000.02.008</identifier><language>chi</language><publisher>青岛海洋大学,山东,青岛,266003</publisher><subject>南半球 ; 大气环流 ; 对流层 ; 西风廓线 ; 超长波</subject><ispartof>Re dai qi xiang xue bao, 2000, Vol.16 (2), p.155-163</ispartof><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/92292A/92292A.jpg</thumbnail><link.rule.ids>314,776,780,4010,27900,27901,27902</link.rule.ids></links><search><creatorcontrib>曲维政 金华</creatorcontrib><title>南半球对流层中部大气环流的若干特点</title><title>Re dai qi xiang xue bao</title><addtitle>Journal of Tropical Meteorology</addtitle><description>P434.2; 分析了南半球对流层500hPa平均地转西风随纬度的分布特点,平均地转西风季节变化特点,计算分析了南半球位势高度对纬向平均的偏差,分析了超长波的分布特征.以上结果均与北半球同期计算结果作了对比比较,指出了南北半球大气环流的异同点.</description><subject>南半球</subject><subject>大气环流</subject><subject>对流层</subject><subject>西风廓线</subject><subject>超长波</subject><issn>1004-4965</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2000</creationdate><recordtype>article</recordtype><recordid>eNo9j81Kw0AUhWehYKl9CEFwlfHOXzJZSvEPCm66D8lkpqaWlDaI3dq6UWlxIQiuFd1IVRDM-ziNvoUJFTf3wrkf55yL0CYBzHzX3-7iJMtSTAC4w31XYAoAGCgGkCuo9q-voUaWJVF5lC7l1KshZqd3dnpV3EzsPF98nNu38dfny8_k2T48LV5vi9m8FIv7i-_rR5u_F5d5Mc7X0aoJe5lu_O06au_ttpsHTuto_7C503KUkNIhjFLlGa61jjXxhCGCCW4AQhkrFhtdFTBGESVd4QpJKGERhVgLwvxISlZHW0vbszA1YdoJuv3TYVoGBsN4MBpF1Y9QjorcWJLquJ92BknJRqE6MUlPB5yI0luyX2PGZag</recordid><startdate>2000</startdate><enddate>2000</enddate><creator>曲维政 金华</creator><general>青岛海洋大学,山东,青岛,266003</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>2000</creationdate><title>南半球对流层中部大气环流的若干特点</title><author>曲维政 金华</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c588-1322c7f4eeede175f15354f00a8dc3dfe2427ffc1c8656581213b20de5139b883</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>chi</language><creationdate>2000</creationdate><topic>南半球</topic><topic>大气环流</topic><topic>对流层</topic><topic>西风廓线</topic><topic>超长波</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>曲维政 金华</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>Wanfang Data Journals - Hong Kong</collection><collection>WANFANG Data Centre</collection><collection>Wanfang Data Journals</collection><collection>万方数据期刊 - 香港版</collection><collection>China Online Journals (COJ)</collection><collection>China Online Journals (COJ)</collection><jtitle>Re dai qi xiang xue bao</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>曲维政 金华</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>南半球对流层中部大气环流的若干特点</atitle><jtitle>Re dai qi xiang xue bao</jtitle><addtitle>Journal of Tropical Meteorology</addtitle><date>2000</date><risdate>2000</risdate><volume>16</volume><issue>2</issue><spage>155</spage><epage>163</epage><pages>155-163</pages><issn>1004-4965</issn><abstract>P434.2; 分析了南半球对流层500hPa平均地转西风随纬度的分布特点,平均地转西风季节变化特点,计算分析了南半球位势高度对纬向平均的偏差,分析了超长波的分布特征.以上结果均与北半球同期计算结果作了对比比较,指出了南北半球大气环流的异同点.</abstract><pub>青岛海洋大学,山东,青岛,266003</pub><doi>10.3969/j.issn.1004-4965.2000.02.008</doi><tpages>9</tpages></addata></record>
fulltext fulltext
identifier ISSN: 1004-4965
ispartof Re dai qi xiang xue bao, 2000, Vol.16 (2), p.155-163
issn 1004-4965
language chi
recordid cdi_wanfang_journals_rdqxxb200002008
source Alma/SFX Local Collection
subjects 南半球
大气环流
对流层
西风廓线
超长波
title 南半球对流层中部大气环流的若干特点
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-02-02T01%3A12%3A15IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-wanfang_jour_chong&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=%E5%8D%97%E5%8D%8A%E7%90%83%E5%AF%B9%E6%B5%81%E5%B1%82%E4%B8%AD%E9%83%A8%E5%A4%A7%E6%B0%94%E7%8E%AF%E6%B5%81%E7%9A%84%E8%8B%A5%E5%B9%B2%E7%89%B9%E7%82%B9&rft.jtitle=Re%20dai%20qi%20xiang%20xue%20bao&rft.au=%E6%9B%B2%E7%BB%B4%E6%94%BF%20%E9%87%91%E5%8D%8E&rft.date=2000&rft.volume=16&rft.issue=2&rft.spage=155&rft.epage=163&rft.pages=155-163&rft.issn=1004-4965&rft_id=info:doi/10.3969/j.issn.1004-4965.2000.02.008&rft_dat=%3Cwanfang_jour_chong%3Erdqxxb200002008%3C/wanfang_jour_chong%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_id=info:pmid/&rft_cqvip_id=4155818&rft_wanfj_id=rdqxxb200002008&rfr_iscdi=true