小冰期

0.8～0m（2.1～0ka）降水继续减少，公元初冷期，中世纪暖期，小冰期在该区都有明确体现。

0.8 ~ 0m ( 2.1 ~ 0 ka ) precipitation continued to fall , the temperature experiences several fluctuations . The Medieval Warm period and the Little Ice Age in the area are obvious .

中国东部小冰期气候特征与环境变迁

The Climatic Features and Environmental Changes of Little Ice Age in Eastern China

重点介绍了气候变暖的新证据，3个特征时期即20世纪气候变暖、小冰期（LIA）、中世纪暖期（MWP）和近千年温度变化模拟的结果。

Discussion is concentrated upon the following issues : the new evidence of global warming , three special periods ( 20th century warming , LIA , and MWP ), and numerical simulations of temperature variations in the last millennium .

东亚地区小冰期气候的模拟

Climate simulation of little ice age over Eastern Asia

小冰期气候的研究

Studies on climate of the Little Ice Age

中世纪暖期与小冰期在中国地区普遍存在。

But the Medieval Warm Period and Little Ice Age are widespread in China .

中国西北地区的小冰期

The little ice age of Northwest China

小冰期气候变化主控因子的模拟试验

Modelling Experiments of the Effects of Climatic Main Factors on the Climate Change of Little Ice Age

另外，小冰期气候变化是各种因素的综合作用，不能忽略自然变化、温室气体浓度以及人类活动等诸多因素的影响。

In addition , natural changes , greenhouse gas concentrations and human activity , should not be ignored .

内蒙古岱海地区小冰期气候演化特征的地球化学记录

Geochemical record for the characteristics of climate change during the Little Ice Age in Daihai Lake , Nei Mongol

小冰期最盛期以来，冰川面积减少49.3%。

The area of glaciers has been reduced by 49.3 % since the Maximum of the Little Ice Age .

太阳活动和火山活动是小冰期气候变化的主要因素。

The solar activity and volcanic eruptions are the main factors of climatic changes during the Little Ice Age .

东亚小冰期气候形成中太阳辐射和火山灰作用的敏感性试验

Sensitivity Experiment of Climate Change in Eastern Asia during the Little Ice Age by Changing Solar Radiation and Volcanic Dust

但在寒冷的小冰期中也有过温暖时期；而且干冷，暖湿相联。

But during the cold Little Ice Age there were some warm periods , dry - cold , warm - damp .

另外，作者提出把从17世纪初开始的小冰期，气候干冷.沙尘暴频发作为现代沙漠化过程开始的观点。

The author thinks the contemporary desertification dates back to the 17th century when the climate was cold and dry , and dust storms were frequent .

另外，该段内气候总体以干冷为主，指示了中国东部小冰期气候的特点。

Actually the weather was dry and cold overall , which indicates the climatic characteristics of The Little Ice Age ( LIA ) in Eastern China .

讨论了大暖期千年尺度气候振荡，中世纪暖期、小冰期及现代气候变暖等问题。

Manifestation of millenniumial time scale oscillations , Megatermal , Mediaeval Warm Period , Little Ice Age , Modern Warming in the20th century in China were examined .

90年代以后，采用热释光和电子自旋共振技术测年，获得了我国第四纪冰川的一些数值年代，划分了5次冰期，其时代初步定为：小冰期Ⅲ（1871±20A.D.）

Based on the dating results , five Quaternary glaciation stages are determined primarily as follows : Little Ice Age , Stage ⅲ( 1871 ± 20A . D. )

考虑到该地区人口密度很低，人类活动不应成为造成该地区乔木植物绝灭的根本原因，笔者认为主要原因应归为长达300多年的“小冰期”寒冷和干旱气候的自然因素。

The authors suggest that cooling and drying in ( about ) 300 a the Little Ice Age is the main reason to the extinction of the arbor , not the people activity .

此降温幅度已与17～19世纪明清小冰期中的极端寒冷年份相近，在过去2000年中亦属于并不多见的极端寒冷年份。

The cold climate of these three years was like that of the extreme cold years from the 17th to 19th centuries . It is one of the rare extremely cold events in the past 2000 years .

再参照有关小冰期（1450或1490年开始至1850或1880年止，约400年）的文献资料，小冰期的气温比1880～1919年时期更低些，因此推论温度偏低期持续了约450年。

We understand the temperature of the Little Ice Age was lower than that of the period from 1880 to 1919 according to the references of the Little Ice Age ( from 1450 or 1490 to 1850 or 1880 , about 400 years ) .