末次冰盛期

结果表明，末次冰盛期的冰川范围是现代冰川的3.1倍；

The results indicate that glaciers in the LGM covered 3.1 times of the present glacier area in this region .

萨哈林岛在末次冰盛期的草原和泰加林主要山落叶松和松组成，和现在西伯利亚东北部的泰加林相似。

During the LGM , bog and taiga were mainly composed of Larix and Pinus in Sakhalin , which could be correlated to the present northeast Siberian taiga .

末次冰盛期低海平面时，河流下切，形成深达40～110m的钱塘江和太湖下切河谷。

In the last glaciation maximum ( 18-15 ka B P ) , the sea-level was lower and washout of river resulted in the formation of the Qiantang river and Taihu Lake incised valleys as deep as 40 to 110 m.

腾格里沙漠南缘末次冰盛期以来沙漠演化与气候变化

Desert Evolution and Climate Change of Southern Margin of Tengger Desert since Last Glacial Maximum

中国东部陆架沉积环境对末次冰盛期以来海面阶段性上升的响应

Sea-level rise and sedimentary environment response in the East China continental shelf since the last glacial maximum

末次冰盛期（18kaBP）是两万年来距人类环境最近、与现代反差最大的气候时期。

Climate conditions in the Last Glacial Maximum ( LGM , 18 kaBP ) were remarkably different from the present .

长江三角洲地区末次冰盛期前海退过程中气候变化的初步研究

Preliminary study on the Climate Changes in the Processes of Regression before the Last Glacial Maximum in the Yangtze Delta Area

杭州湾地区末次冰盛期第一硬质黏土层粒度特征及其环境意义

Grain-size characteristics of the first hard clay and their environmental implications during the last glacial maximum in the Hangzhou Bay region

在北海道末次冰盛期的草原和泰加林主要由落叶松、松以及云杉组成，气候更加干冷。

In Hokkaido , grassland and taiga were mainly consisted of Larix , Pinus and Picea . Climate was colder and drier than that around 30 ka .

中国古湖泊数据库收录的42个湖泊，提供的湖泊水量每千年变化的空间信息，可以用来系统分析中国区域末次冰盛期以来大气环流变化的状况。

The 42 lakes compiled in the Chinese Lake Status Data Base ( CLSDB ) , has provided the information of the spatial changes of lake status for each one-thousand year , which can be purposed for research on the atmospheric circulation changes of Chinese region since LGM .

末次冰期冰盛期和中全新世中国地区气候变化的数值研究FT中文网：气候转暖房价反弹房展终结冰期？

Simulations of Climate Changes over China in LGM and Mid-Holocene ; FT Chinese Network : climate warming house from the end of ice age citizens ?

影响西伯利亚南部猛犸象动物群消亡的主要变化可能开始于末次冰期冰盛期（LGM）之后。

The major change that influenced the demise of the mammoth fauna in southern Siberia was probably initiated after the Last Glaciation Maximum ( LGM ) .

近年来，中国科研工作者已就末次冰期冰盛期东亚区域气候开展了一些数值模拟工作。

Some numerical experiments for this period have been performed in China in recent several years .