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monsoon相关的网络例句

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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,发现了暖池海区冰消期表层水升温超前于北半球冰盖的融化。

Three preliminary conclusions could be approached as follows:(1) SST changes were distinctively characteristic of stepwise fluctuations. A warming trend during the last deglaciation was punctuated by a slightly cooling event which corresponded to the Younger Dryas. The Holocene episode could be divided into three phases of warming, continuously high temperature and cooling.(2) Two remarkable cooling records were documented around 4 kaBP and 1.5 kaBP after the megathermal of the Holocene.(3) Comparison between time series of MD05-2904 diatom R SST index and stalagmite δ^18O results from Dongge Cave, Guizhou Province suggested that changes in the East Asian Monsoon climate is synchronous with variations in the SST in the northern SCS since the last deglaciation and they might have a close correlation with each other

结果表明:(1)南海北部15 kaBP以来表层海水温度呈现明显的阶段性波动特点,即末次冰消期气候转暖过程中,12.9~11.5 kaBP前后温度略有下降,与新仙女木事件对应,全新世南海北部气候依次经历了升温期、高温期和降温期3个变化阶段;(2)全新世大暖期鼎盛期结束后,南海北部海水温度阶段下降,两次明显降温分别发生于4 kaBP前后和1.5 kaBP前后;(3) MD05-2904孔硅藻R值时间序列曲线与董哥洞D4石笋δ^18O曲线对比表明,南海北部表层海水温度变化与末次冰消期以来东亚季风强度变化关系较为密切。

About 70% of the total rainfall as heavy downpour in the summer monsoon months and 30% in winter.

夏季季风季节的暴雨占总降雨量的70%,冬季占30%。

Heating over the Bay of Bengal can induce Indian Southwestlies monsoon to extend eastwardly, heating over the subtropical continent is the major mechanism for the subtropical high over the Northern Hemisphere.

孟加拉湾的热源可使印度西南季风向东延伸,而副热带大陆热源也是北半球副热带高压系统形成的主要机制。

We suggest that snow cover, temperature and rainfall interact and produce chaos which is possibility the reason why prediction of annual monsoon rainfall is not come through, and the reason why the relationship between snow cover and rainfall is elusory.

积雪、温度和降水相互作用可能会产生混沌行为,这可能就是为什么对季风降水的年预报不能成功的原因,也可能是为什么积雪与季风降水之间的关系变得难以捉摸的原因。

The record of the eolian sequence indicated that the East Asia monsoon is started at 8.35Ma.

红粘土开始堆积标志着东亚季风约在8.3Ma开始建立。

Under the influence of tropical monsoon climate, the foehn effect of the rain shadow field of the Changshan Mountains and the Wuzhishan Mountains and the cold ocean current in the Beibu Gulf, it is developed into the semi-ari d climate and the environment of dry grasslands with sparse trees.

在大气环流、雨影区和海流的共同影响下,岛西形成热带半干旱气候和热带稀树草原环境,孕育并存在自然沙漠化发展的动力、空间和物质基础。

East Asian winter monsoon ; late Pliocene ; isotope ; foraminifer ; South China Sea

东亚冬季风;上新世晚期;同位素;有孔虫;南海

Results show that the existence and geometric shape of land-sea distribution crucially affect the Asian summer monsoon.

试验结果显示:海陆分布的存在以及海陆分布的几何形状对亚洲夏季风的形成有非常重要的影响。

The past research about Holocene palaeoclimate in east part of China emphasizes on the impact of summer monsoon.

在我国东部全新世气候变化研究方面,过去的研究着重于夏季风及其对我国东部气候变化影响上。

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