综合及预测

东亚季风边缘活动带研究综述

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  • 北京大学物理学院大气科学系,北京 100871
徐袁 (1979-), 男, 江苏泰州, 硕士研究生, 研究方向为气候学。E-mail: pkuxuyuan@etang.com

收稿日期: 2003-04-26

  修回日期: 2003-07-05

  网络出版日期: 2003-12-25

基金资助

国家基础发展规划项目 (No. G1999043405)

Research on East Asian Summer Monsoon: A Review

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  • Department of Atmospheric Sciences, Peking University, Beijing 100871, China

Received date: 2003-04-26

  Revised date: 2003-07-05

  Online published: 2003-12-25

Supported by

National Key Project for Nasic Sciences, No. G1999043405

摘要

由于其同时具有的生态脆弱性和气候敏感性,东亚季风边缘研究有利于加深认识季风以及生态系统在过渡带上的特性,而且它对于国家的西部大开发战略以及南水北调工程都有重要的气候学指导意义。从天气学原理角度出发,分析指出青藏高原等地形以及海陆热力差异是对东亚季风边缘影响的重要因子,ENSO和全球变暖等因子对季风边缘活动也有影响。阐述了季风的年际变化,季风边缘,季风边缘进退等概念。通过对代用资料如湖相沉积,湖面大小变化,陆相沉积以及农牧交错带演变研究的综述,对古季风的演变做了分析,指出近几千年来干旱化趋势的存在。利用现有气象观测资料所作的东亚季风边缘的年际和年代际变化很少,这是一个可以深入研究的方面,已有的气候平均态的研究可以对此做一定的指导。同时,北方干旱化和东亚冬季风边缘研究既有区别又有联系,两方面相互促进。

本文引用格式

徐袁,钱维宏 . 东亚季风边缘活动带研究综述[J]. 地理学报, 2003 , 58(7s) : 138 -146 . DOI: 10.11821/xb20037s017

Abstract

This paper summarizes the researches on the marginal active belt of East Asian summer monsoon. A range of sections are presented, dealing with the meaning of this research, the influencing factors in marginal monsoon activity, and studies on advance and retreat of monsoonal margins as well as interannual and interdecadal variations of northern boundary of East Asian summer monsoon.

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