首页 | 本学科首页   官方微博 | 高级检索  
     

全球小冰期的气候变化
引用本文:王立国,钟巍,李偲. 全球小冰期的气候变化[J]. 冰川冻土, 2002, 24(6): 750-758. DOI: 10.3969/j.issn.1000-0240.2002.06.010
作者姓名:王立国  钟巍  李偲
作者单位:1. 新疆大学, 资源与环境科学学院, 新疆, 乌鲁木齐, 830046;2. 华南师范大学地理系, 广东, 广州, 510631
基金项目:国家重点基础研究发展计划(973计划);G1999043508;
摘    要:根据全球小冰期气候信息的不同代用指标的结果分析,全球小冰期冷、暖气候变化趋势具有一致性.其中,太阳活动是影响全球小冰期气候变化的主要因素,强火山爆发及厄尔尼诺事件则是其强化因素,这些因素通过海-气作用这一复杂机制对全球气候产生深远影响.

关 键 词:全球气候变化  小冰期  
文章编号:1000-0240(2002)06-0750-09
收稿时间:2002-05-29
修稿时间:2002-05-29

Global Climate Changes During the Little Ice Age
WANG Li guo ,ZHONG Wei ,LI Cai. Global Climate Changes During the Little Ice Age[J]. Journal of Glaciology and Geocryology, 2002, 24(6): 750-758. DOI: 10.3969/j.issn.1000-0240.2002.06.010
Authors:WANG Li guo   ZHONG Wei   LI Cai
Affiliation:1. College of Resources and Environmental Sciences, Xinjiang University, Ürümqi Xinjiang 830046, China;2. Department of Geography, South China Normal University, Guangdong Guangzhou 510631, China
Abstract:The climate since 1500 A.D. has been highlighted in the field of global change. Recently, some studies, such as PAGES and WCRP, have opened up broad prospect for the detailed high-resolution climatic records, such as tree-rings, corals and ice-cores etc. More attention is focused on the global climate changes on the basis of paleoclimate information of annual-to-millennial time scales. Especially, the climate of the Little Ice Age(LIA), which may be regarded as a short-scale neoglacial episode or a series similar to the climate change from glacial period, is a very important time stream and have an important role in studying the variations of atmospheric circulation and environment and climate in regional or global extent, and in establishing scientifically contemporary climate matrix. Based on historical documents, dendroclimatic data and ice core records from Europe, Asia, North America, South America and Antarctica since the LIA, a synthetic analysis of the paleoclimatic information is made in this paper. The main results are given as follows: (1) The general tendency of global cold-warm change since the LIA exhibits a consistency in a certain degree, with a high spatial and temporal variation. There were strong cold periods in the 17th and 19th centuries and a strong warm period in the 1920’s-1940’s. (2) Because of apparent allocation difference between oceans and continents, there is a prominent distinction in the effect of atmospheric circulation patterns, radiation balance of underlying surface and abrupt events on regional and global climate. The strength of circulation systems between Atlantic, Arctic and Pacific, which have different power and duration, has different influence on the global climate change since the LIA from coast to continental interiors of Eurasia. Meanwhile, the uplift of the Tibetan Plateau further increases the regional difference and deeply influences global climate changes. (3) The large-scale effects of solar activity, violent volcanic eruptions and EL Nino events on ocean-atmospheric mechanism play a pivotal role in the global climate system. Especially, solar activity is the main factor affecting the global climate changes since the LIA. Those changes are further influenced by atmospheric circulation system enhanced by violent volcanic eruptions and EL Nino events.erentpowerand
Keywords:global climatic changes  Little Ice Age
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《冰川冻土》浏览原始摘要信息
点击此处可从《冰川冻土》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号