盛冰期

末次盛冰期南京降水记录中ENSO的演化

The Evolution of ENSO During LGM from Precipitation Record in Nanjing

CO2浓度在末次盛冰期最低，其混合比为200×10-6，这使得气温降低。

During the LGM , CO2 concentration reached its lowest point of 200 × 10-6.This results in a temperature decrease over China .

赤道西太平洋海区末次盛冰期以来δ18O值显著降低，但有几次回返事件。

It has been demonstrated that the δ ~ ( 18 ) O in the west Pacific significantly decreased since the last glacial maximum together with , however , a few return events such as the cooling events during the Younger Dryas period of 13.7 ~ 12.2 cal .

末次盛冰期百年尺度气候变化的南京石笋记录

Century-scale climatic oscillations during the last glacial maximum recorded in a stalagmite from Nanjing

末次盛冰期以来中国北方干旱区演化及短尺度干旱事件

Evolution and drought events in arid region of northern China since the last glacial maximum

末次盛冰期黄土高原蜗牛化石记录的气候快速变化及其影响机制

Rapid climate variability recorded by mollusk species on the Loess Plateau during the 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

Paleoclimatic evolution deduced from organic carbon isotope of western Loess Plateau sediments since Last Glacial Maximum

末次盛冰期气候模拟及青藏高原冰盖的可能影响

Palaeoclimate modeling for the LGM and the possible influence of the continental ice sheet over the Qinghai-Xizang Plateau

南沙海区盛冰期的气候问题

The last glacial maximum climate problem in the sea area of the Nansha islands , south China Sea

赤道西太平洋末次盛冰期以来的浮游有孔虫氧碳稳定同位素记录

Oxygen and carbon stable isotopic records of planktonic foraminifers from the western equatorial Pacific since the last glacial maximum

末次盛冰期以来长江河口段河道演变研究综述

An Overview of the Research on Channel Evolution in the Yangtze River Mouth Region Since the Last Glacial Maximum

盛冰期南京石笋δ~（18）O与年纹层厚度的对比

Comparison Between Nanjing Stalagmite δ ~ ( 18 ) O and Annual Layer Thickness Records During the Last Glacial Maximum

晋西北地区末次盛冰期古风成砂的发现及环境演化

The discovery of palaeo eolian sand formed in the last glacial maximum and environmental evolution in the northwest of Shanxi

基于孢粉数据和植物功能型全球分类系统的全新世中期和末次盛冰期我国古植被格局定量重建

Pollen-based reconstruction of vegetation in China during the mid-Holocene and last glacial maximum using a global scheme of plant functional types

末次盛冰期的冰川范围十分有限，并且MIS3阶段的冰进规模远远超过了末次盛冰期。

However , the scale of glacial advance during MIS 3 / 4 even exceeded that of the Last Glacial Maximum .

末次盛冰期西太平洋海温差异对亚洲夏季风影响的数值模拟

Modeling the impact of the Western Pacific sea surface temperature difference on the Asian summer monsoon climate at the last glacial maxium

末次盛冰期北美风成环境变化及其在全球气候突变事件中的意义

Variations in the eolian environment of North America during the last glacial maximum and their significance in the global abrupt climatic events

末冰盛冰期向末次冰消期过渡期全球发生了一系列冷暖交替的气候事件，其中冷事件Heinrichl事件是最为关注的事件之一。

A series of alternating cold and warm events has happened all over the world in the transition from the last Glacial to the last deglaciation .

末次盛冰期以来全球湿润状况的地质证据&全球古湖泊数据库及其湖水位变化的大尺度时空分析

The geological evidence of the global moisture condition changes since the last glacial maximum : the construction of global Lake status data base & the synthesis in the large spatio-temporal scale

且在末次盛冰期低海平面时，陆源物质通量高而稳定，长江和东亚冬季风输运的粘土粒级碎屑物质增多。

The clay-size terrigenous detritus supplied by Yangtze River and East Asia winter monsoon also higher in the last glaciation maximum ( LGM ) while terrigenous flux is high and changes smoothly .

末次盛冰期冲绳海槽中部陆源物质来源于东海陆架，元素地球化学特征显示这些沉积物主要来源于古长江的入海物质。

The provenance of the sediment in middle Okinawa Trough during the Last Glacial Maximum is the shelf of the East China Sea . The characteristics of elemental geochemistry ascertain that the sediment was derived from the paleo-Changjiang River .

末次冰期盛冰期以来，由于气候的冷暖变化和海面的升降波动等影响，南京以下长江河道经历了多次摆动和变化调整。

With the effect of climatic change and sea level fluctuating , the channel has sway many times from south to north or from north to south since the last glaciation maximum , but its general deflection is to south .

该模拟结果的意义在于：（1）率先用具有物理机制的数值化模型再现了末次盛冰期中国的气候状况，结果与地质资料基本一致；

The simulation is able to sever : ( 1 ) It is first time to use a AGCM with physical processes and mechanism to simulate last maximum glacial climate in China and that is consistent with geological evidence basically .

末次盛冰期以来，由于海面发生大幅度的变化，长江河口段经历了深切古河谷形成古河谷充填三角洲发育的河床演变过程。

Since the Last Glacial Maximum , the riverbed of the Yangtze River mouth region has evolved from the shape of the deep incised-valley to the filling of the palaeo-valley and to the delta development because of the great change of the sea level .