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dryas相关的网络例句

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与 dryas 相关的网络例句 [注:此内容来源于网络,仅供参考]

; 3 younger Dryas Only has reflection in the hundred-year-scales climatic curve, it is not evident in the curve of long period; 4 in the hundred-year-scales climatic curve, the last glacial maximum fluctuation as frequuently and 18-28KaBP was the stage in which the frequency fluctuation was the largest.

;(3)新仙女木事件仅反映在百年尺度的气候曲线上,在较长周期的饿曲线上不明显;(4)在百年尺度的气候曲线中,末次冰盛期气候波动频繁,其中18-28KaBP 是频率波动的最大阶段,但随着周期尺度的加大,气候的波动频率逐渐趋于均匀。

The fluctuations of the EC abundance correlate well with that of δ〓O in GRIP ice core, indicating the existence of some short-term climate change events, such as Younger Dryas, Heinrich events and Bond's cycles.

渭南黄土剖面的元素碳浓度曲线的总体波动形式与格陵兰GRIP冰芯氧同位素记录曲线有相似性,并对短尺度的气候事件如:新仙女木事件、哈因里奇事件(H1-H6)、Bond旋回等有较好的反映。

Scientists have found microscopic diamonds across North America in a black layer of carbon-rich material corresponding to the beginning of the Younger Dryas, a 1,300-year cold spell during which North American mammoths, saber-toothed cats, camels and giant sloths became extinct.

科学家们发现极小的钻石全北美黑色一层富含碳的材料相应的开头新仙女木,一个1300年的春寒中北美猛犸象,剑齿猫科动物,骆驼和巨大sloths灭绝。

10Be records in the Okinawa Trough sediment during the last glacial, the Younger Dryas cold period, and the Holocene show that the main part of the fluctuations in 10Be content in the sediment can be attributed to variations in the 1°Be production rate.

表层沉积物中的10Be,9Be和Pb三者表现出完全不同的分布特征。10Be的分布主要受黑潮及其支流黄海暖流所支配;10Be的分布受黄河陆源物质输入的影响,主要集中在南黄海泥质区;Pb则主要分布在长江口和琉球群岛附近,反映了人类活动的影响。

Since the Present Epoch, large scale glaciation has ceased. Especially the ending of the Younger dryas Event about 10Ka ago, led to global warming in a rapid way. Contemporary glacial geologic process since the Present Epoch began in the global.

全新世以来,大规模冰川作用已停止,特别是距今1.0万年前后的新仙女木事件的结束,全球性快速增温,以结束LGM未次冰期而进入全新世以来的现代冰川地质作用。

This cognition is coincident with the resu1ts of organic carbon, pollen and phyto1ith. The f1uctuations of the EC abundance correlate we1l with that of 5 ls0 in GRIP ice core, indicating the existence of some short--term climate change events, such as Younger Dryas, Heinrich events and Bond's cycles.

渭南黄土剖面的元素碳浓度曲线的总体波动形式与格陵兰GRIP冰芯氧同位素记录曲线有相似性,并对短尺度的气候事件如:新仙女本事件、哈团里奇事件(H1-H6)、Bond旋回等有较好的反映。

The stratigraphic sequences covering the Younger Dryas period has been further divided into Heiheze silt, Baxie paleosol and Taohe loess.

将对新仙女木期(L1LL0)地层作进一步划分,它由黑河则粉沙、巴谢古土壤和桃河黄土构成。

Six obvious short-term SST descending events have been recognized in the last glacial. The age of "Younger Dryas" event was estimated at 11.75~12.38kaBP, and the H1~H4 events were estimated at 15.51~16.76, 21.15~22.40, 26.79~27.42 and 34.31~34.94kaBP, respectively.

南海西南陆坡区在末次冰期出现6次明显的海水表层降温事件,其中&新仙女木&事件的年代约为11.75~12.38kaBP,H1~H4事件的年代分别约为15.51~16.76、21.15~22.40、26.79~27.42和34.31~34.94kaBP。

The analyses of environmental indexes of the sediment from a 5.3m core, CE-2 core, taken from Co Ngoin lake, reveals the process of climate change in the central Tibetan Plateau during 12~4kaBP, shown as cold and wet period (before 11.2kaBP)→Allerod period (11.2~10.9kaBP)→Younger Dryas (10.9~10.5kaBP)→warm and wet period (Holocene, after 10.5kaBP).

通过CE-2孔5.3m湖泊沉积物高分辨率多指标综合研究,获得了高原中部12kaBP以来详细的气候环境演化过程:11.2kaBP前的冷湿阶段-阿勒罗德期(11.2~10.9kaBP)-新仙女木期(10.9~10.5kaBP)-全新世暖湿期(10.5kaBP后)。

The analyses of environmental indexes of the sediment from a 5.3m core, CE-2 core, taken from Co Ngoin lake, reveals the process of climate change in the central Tibetan Plateau during 124kaBP, shown as cold and wet period (before 11.2kaBP)→Allerod period (11.2~10.9kaBP)→Younger Dryas (10.9~10.5kaBP)→warm and wet period (Holocene, after 10.5kaBP).

更多综合研究,获得了高原中部12kaBP以来详细的气候环境演化过程:11.2kaBP前的冷湿阶段-阿勒罗德期(11.2~10.9kaBP)-新仙女木期(10.9~10.5kaBP)-全新世暖湿期(10.5kaBP后)。

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