3万年来亚洲降水与大气环流变化重建和模拟综述

被引：5

作者：

廖梦娜

于革

机构：

[1] 中国科学院南京地理与湖泊研究所湖泊与环境国家重点实验室

来源：

地理科学进展 | 2014年 / 33卷 / 06期

关键词：

亚洲; 湖泊水位; 晚第四纪; 古湖沼学; 古气候模型; 古气候重建;

D O I：

暂无

中图分类号：

P426.6 [降水]; P435 [数值试验];

学科分类号：

0706 ; 070601 ;

摘要：

区域性的湖泊水位能反映有效降水及气候变化,已成为重建第四纪降水和水量平衡最重要的指标。亚洲分布着几乎全球各种成因类型的湖泊,第四纪湖泊演化在全球第四纪研究中占有重要地位。多年来通过对地貌学、沉积学、生物地球化学和考古学的研究重建了各个区域的湖泊水位变化,并据此建立了湖泊演变数据库,作为研究第四纪亚洲区域气候变化的重要基础。本文介绍湖泊水位气候理论的发展历程,回顾晚第四纪亚洲湖泊水位研究的历史;分析晚第四纪亚洲从西到东不同区域湖泊水位变化历史和地域特征,并根据晚第四纪冰期和间冰期的两个特征期湖泊空间变化特征,从古气候模拟的角度探讨了气候驱动机制下湖泊水位变化的成因。

引用

页码：807 / 814

页数：8

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