1) Last Glacial Maxium
末此盛冰期
2) LGM
末次盛冰期
1.
MM5 SIMULATIONS OF THE CHINA REGIONAL CLIMATE OF THE LGM Ⅱ:INFLUENCES OF CHANGES OF LAND AREA,VEGETATION,AND LARGE-SCALE CIRCULATION BACKGROUND;
MM5对末次盛冰期中国气候的模拟研究Ⅱ:海陆分布、植被和大尺度环流背景变化的影响
2.
MM5 SIMULATIONS OF THE CHINA REGIONAL CLIMATE OF THE LGM Ⅰ:INFLUENCES OF CO_2 AND EARTH ORBIT CHANGES;
MM5对末次盛冰期中国气候的模拟研究Ⅰ:CO_2和地球轨道参数的影响
3.
Newly-Studies on Global Continental Climate and Terrestrial Yegetation during the LGM;
全球大陆末次盛冰期气候和植被研究进展
3) Last Glacial Maximum (LGM)
末次盛冰期
1.
There has been a big change of the sea level and seabed water temperature since the Last Glacial Maximum (LGM) in southern South China Sea.
末次盛冰期以来南海南部海平面及海洋底水温度均发生了很大的变化。
2.
In this article,Milkov and Sassen s model is selected to calculate the thickness of the gas hydrate stable zone (GHSZ) and the amount of gas hydrate in the Xisha Trough at present and at the last glacial maximum (LGM),respectively,and the effects of the changes in the bottom water temperature and the sea level on these were also discussed.
利用Milkov和Sassen的模型计算了目前及末次盛冰期时西沙海槽天然气水合物的稳定带(GHSZ)厚度及资源量,讨论了末次盛冰期以来海洋底水温度增加和海平面升高对西沙海槽天然气水合物储库变化的影响。
4) Last glacial maximum
末次盛冰期
1.
Paleoclimatic evolution deduced from organic carbon isotope of western Loess Plateau sediments since Last Glacial Maximum;
黄土高原西缘末次盛冰期以来古气候演化的有机碳同位素记录
2.
Environmental Changes Revealed by Lacustrine Sediment from Longgan Lake since Last Glacial Maximum;
龙感湖钻孔揭示的末次盛冰期以来的环境演化
3.
According to the protocol of the phase one of the Paleoclimate Modelling Intercomparion Project(PMIP),a global atmospheric general circulation model developed at the Institute of Atmospheric Physics under the Chinese Academy of Sciences(IAP-AGCM)was used to simulate East Asian climate at the Last Glacial Maximum(LGM),about 21,000 calendar years ago.
在国际古气候模拟比较计划设置的标准试验方案下,首先利用中国科学院大气物理研究所的全球大气环流模式(IAP-AGCM)模拟了末次盛冰期东亚气候状况,然后通过4组数值敏感性试验逐一模拟了大气CO2浓度、海洋表面温度(SST)和海冰、陆地冰盖和地形、东亚植被变化4项强迫因子的单独气候效应,进而对末次盛冰期东亚气候的成因进行了检测。
5) Last Glacial Maximum
末次冰盛期
1.
Vegetation on the emerged continental shelves of the South China Sea (SCS) during the Last Glacial Maximum (LGM) was deduced based on pollen of hemipelagic sediments from the continental slopes and the consideration of pollen transport dynamics and source areas.
在探讨孢粉的传播、来源地的基础上，根据南海南北陆坡柱状剖面（１７９４０ ，１７９６４） 的孢粉资料推断末次冰盛期（包括氧同位素３ 期的上部） 低海面时，南北出露的大陆架上生长的植被。
2.
This paper presents the estimated climatic scenarios in the Last Glacial Maximum(LGM) using glacier dynamics method, based on glacial vestiges well preserved in the head water of the Urumqi River and the relationship between glacier mass balance and climate in the contemporary climatic scenarios.
根据乌鲁木齐河源区末次冰盛期形成的保存完好的古冰川遗迹和现代气候条件下冰川物质平衡与气候的关系，用冰川动力学方法估算出冰川达到末次冰盛期规模时的气候条件。
3.
The past～25,000 years,which covers the Last Glacial Maximum,the last deglaciation andHolocene,witnessed the most dramatic climatic changes of global scale during recentgeologic history.
近25 ka以来跨越了末次冰盛期、末次冰消期及冰后期，是过去全球变化研究的一个重要时段。
6) the last glacial maximum
末次盛冰期
1.
Climate fluctuations during the Last Glacial Maximum have been a hot topic recently.
通过对长江三角洲东部地区鹤鸣孔第一硬黏土层的孢粉、藻类分析,研究了该地区末次盛冰期的气候波动。
2.
A high resolution terrestrial mollusk record from the Chinese Loess Plateau has been studied to study climate variability during the last glacial maximum (LGM).
本文通过对渭南黄土剖面末次盛冰期地层较高分辨率的蜗牛化石记录研究 ,发现这一时期特征蜗牛种类峰值的演替反映了古气候的演化过程和温、湿度的组合关系 ,气候变化显示出百年～千年尺度波动的特征 ,温度的变化明显地要早于湿度 (降水 )的变化 1 0 0 0～2 0 0 0a ,表现为变冷 -冷湿 -冷干 -温干 -温湿的气候过程 ,研究认为造成这一气候特点的原因是东亚冬、夏季风共同作用的结果。
补充资料：笃笃末末
1.盘盘旋旋。
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