1) ice melting
冰消融
2) last deglaciation
冰消期
1.
The elementary stratigraphy of the middle Okinawa Trough since the last deglaciation;
冲绳海槽中段末次冰消期以来的元素地层
3) deglaciation
冰消作用
4) last deglaciation
末次冰消期
1.
A typical borehole P5 was examined for lithology, dating, spore-pollen and microfossil to reveal the phases of climate and sea level fluctuation and the associated sedimentary facies recorded in the paleo-incised valley sediments in the southeastern Changjiang Delta Plain since the last deglaciation.
利用典型钻孔P5孔沉积物的岩性、测年、孢粉和有孔虫的分析结果,探讨了末次冰消期以来长江三角洲东南部古河谷区记录的气候波动和海平面阶段性上升过程及其控制下的古河谷沉积模式。
2.
The rapid climatic changes occurred at the northwest margin of East Asia monsoon region during the last deglaciation were divided into six climatic periods, namely Oldest Dryas, Exiling, Older Dryas, Allerd, IACP and Young Dryas periods.
通过对中卫剖面和米浪沟湾剖面的年代学与高分辨率气候地层记录的研究,认为末次冰消期东亚季风区西北缘发生气候快速变化事件,它可分辨出古仙女木、波令、老仙女木、阿勒鲁德、IACP 和新仙女木等6个气候阶段,并可与格陵兰冰心(GISP2)检出的6个气候阶段相对比。
3.
Being a warming stage in orbital scale changes, the last deglaciation period doesn’t keep a stable climate but characterized by some short cooling events.
末次冰消期本是气候变暖的时期,但期间也存在不同程度的短周期降温事件,新仙女木事件(Younger Dryas Event,简称YD)就是在持续升温的情况下突然发生的一次降温事件,也是地质历史上离现在最近表现最强烈的降温事件。
5) the last deglaciation
末次冰消期
1.
On the basis of biological, lacustrine and glacial sediment stratigraphy records, the paper analyzed the features of climate change during the last deglaciation in the Tibetan Plateau, and correlated to the climatic evolution sequences in Europe and Greenland.
根据生物、湖泊及冰川地层记录,分析了青藏高原末次冰消期的气候演化特点,并将其与格陵兰、欧洲气候演化序列进行了对比分析。
2.
This paper reports a recent research on climatic and environmental evolution at Changgouzhen(38°32′N,115°47′E)area,60km southwest of Beijing city during the Last Deglaciation.
对北京房山县长沟镇附近埋藏末次冰消期湖沼沉积物层序和岩性变化的观测资料，以及１４Ｃ测年、孢粉分析、磁化率、有机碳δ１３Ｃ值和有机质含量等测定资料的综合研究表明：１）约１３０００ａＢ。
3.
The mud area off Yangtze River estuary is one of the accumulative centers of Yangtze River sediment since the last deglaciation transgression, the core ECS-0702 (122°40.
长江口滨外泥质区是末次冰消期海侵以来的长江入海物质沉积中心和“物质汇”之一,论文对取自该泥质区的ECS-0702孔(122°40。
6) antarctic ice decrease
南极冰消退
参考词条
补充资料：冰川消融
冰川消融 由冰的融化和蒸发引起冰川消耗的现象，它是冰川物质消耗的主要方式。太阳直接辐射和近地层大气湍流交换是引起冰川消融的主要热源，冰面性质、冰川所在高度和坡向以及天气状况对消融也有影响。消融主要发生在夏季和白天，因而，具有日、季和年的变化。其数量取决于冰川所在纬度（温度）和冰面污染程度。冰川消融的方式有冰面消融、冰内消融和冰下消融，而以冰面消融为主。研究冰川消融是分析、预测冰川进退的重要途径，是山区公路与桥梁设计的依据，是了解河流补给状况，开发利用冰川资源的基础。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。