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The author concludes that the last deglaciation climate variation in the proxy records for the east Asian monsoon has an asymmetric shape; the warming events are abrupt and the cooling events are gradual.

指出东亚季风区末次消期气候的不对称性即从暖期向冷期的渐变以及从冷期向暖期的突变过程。

The project team has taken loess, lacustrine and peat sediments and tree ring as the research carrier, a systematic study has been carried on the warm phases of the different period (60-25 ka, last deglaciation, Holocene, the recent e few hundred years) and the last interglaciation on the basis of the extensive field investigation and laboratory analysis.

项目组以黄土、湖沼和树轮等沉积物为研究载体,经过大量的野外考察和实验室分析测试,对我国半干旱带末次间期和距今六万年以来不同时间段的温暖期(6万年到2.5万年、末次消期、全新世、最近几百年)进行了系统的研究,取得了一批重要的阶段性成果,确认了东亚季风气候和温暖期的不稳定性特征。

She came to the small river, the river deglaciation snowmelt followed, singing a sweet song into the distance, along with the mountains and the ding dong of a few shares to trickle, like a sweet river ditty reverberating.

她来到小河边,河水随之消雪融,欢唱着动听的歌流向远方,再加上山上叮咚而至的几股涓涓细流,宛如一首悦耳的小曲在河边回荡。

The present project of "deepsea processes and records" targets at the ignored aspects of the theory. Combining the geological records with climatic numerical modeling, we recognized the stepwise process of development of the "Western Pacific Warm Pool" and the East Asian monsoon system, and found that the sea surface warming in the Warm Pool was leading the melting process of the boreal icesheet during the deglaciation.

本项目以"西太平洋暖池"为重点,通过地质资料和气候数值模拟的结合,揭示了"西太平洋暖池"和东亚季风发育的阶段性,发现了暖池海区消期表层水升温超前于北半球盖的融化。

The climatic warming from last deglaciation to the early Holocene in the inner shelf of the ECS has been worldwidely recorded, which may be the integrated results of orbital insolation forcing, the solar activities and the northward migration of intertropical convergence zone.

东海内陆架区对末次消期至早全新世气候回暖的记录与该时期世界性的广泛记录相一致,应该是轨道时间尺度上太阳辐射增强与ITCZ北移以及太阳活动变化综合影响的结果。

The research results indicated that the climatic changes could be divided into four stages as follows: late deglaciation (11324-10290 a B. P.), early holocene (10290-8850 a B. P.), mid holocene (8850-4400 a B. P.) and late holocene

研究结果表明,柴达木盆地尕海湖地区环境演化大致经过4个阶段:消期晚期(3109~3454cm)、早全新世(2623~3109cm)、中全新世(1114~2623cm)和晚全新世(50~1114cm)。

This low carbonate event may have resulted from changes of rainfall. During deglaciation, the dry climate caused a decrease in terrigenous sediment input. However, during Early-Middle Holocene, the rainfall, especially the heavy rain with higher erosions increased rapidly, leading to the increase of terrigenous sedimental supplies from South China mainland and Hainan islands.

消期,出现干旱,陆源物质减少,而早中全新世的雨量,尤其是具较强冲刷能力的大雨量急剧增加,造成北部海南岛和华南陆地的冲刷增强,陆源物质供给增加,从而出现低钙事件。

They reveal the paleoceanographic and paleoclimatic evolutionary history during the Neogene in the high latitude of the North Atlantic, find the millennial timescale climatic variability during the early Pleistocene "41 ka world" and couple the oscillation between surface temperature and deep water during the glacial periods, indicating the climatic instability of deglaciation during the glacial and interglacial cycles.

它们揭示了北大西洋高纬度海区新近纪的古海洋学和古气候的演化历史,发现了早更新世"41ka世界"千年尺度的气候波动,以及期表层水温与深层水的耦合颤动,说明期旋回中消期气候的不稳定性。

In terms of productivity, an overall increasing trend was shown in PC-14 from the deglaciation (14.0—11.6ka) to the Holocene, reflecting a climate transition from an El Ni?

消期到全新世, PC14 生产力呈现阶段上升趋势,指示了由E1 Ni?o 气候向La Ni?

Furthermore, the east Asian monsoon climatic instability during the last deglaciation has been discussed. The significant variability within monsoon precipitation events during the last deglaciation event or even Younger Dryas id related to the interaction between cold air mass from the Siberian-Mongolian high pressure zone with warm, humid air masses from the ocean.

与西北欧和极地北大西洋相比较,东亚末次消期尤其是新仙女木季风降水的有意义的变率与西伯利亚—蒙古高压强弱的变化所导致的内陆冷气团与来自海洋的暖湿气团的相互作用有关。

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Lugalbanda was a god and shepherd king of Uruk where he was worshipped for over a thousand years.

Lugalbanda 是神和被崇拜了一千年多 Uruk古埃及喜克索王朝国王。

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