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SST相关的网络例句
与 SST 相关的网络例句 [注:此内容来源于网络,仅供参考]

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。

The major results are as follow:① There is a great similarity between Intertropical Convergence Zone over the Pacific and SST in the seasonal trend, with ITCZ and high SST found in Southern Hemisphere in winter and in Northern Hemisphere in summer.

结果表明:(1)热带太平洋辐合带系统与海温具有相同的季节变化趋势,冬季赤道辐合带和高海温位于南半球,夏季位于北半球。

The observational equations have been derived using the three methods above which are based on high-low SST and low-low SST observational data respectively, at the same time, the shortages and merits of these three methods are analyzed. 3The problem of gravity field recovery can be attributed to the solution of over determined system of equations.

本文分别以高低卫卫跟踪和低低卫卫跟踪观测数据为基础,导出了基于上述三种方法的观测方程,并分析了它们的优缺点。3重力场恢复最终归结为超定线性方程组的求解问题。

The results show that the highest SST appears in August and the lowest SST in February every year.

结果表明:长江口区表层水温最高值出现在8月份,最低值出现在2月份。

It is justified that during the stronger winter monsoon, the westerlies are intensified over the equatorial western Pacific and the in situ SSTA is positive, while and the easterlies are intensified over the equatorial eastern Pacific and the SSTA is negative because of the air-sea interaction over the Northern Pacific.

证明由于北太平洋的上的海—气相互作用,强东亚冬季风期间,赤道西太平洋西风加强,SST为正异常;赤道东太平洋东风加强,SST为负异常。

In the northern part of the Okinawa Trough,at about 7.5-7.0kaBP of the early Holocene, this studied region was controlled by the continental shelf water, and at about 7.0aBP Kuroshio water combined with continental shelf water intensively, then the region was controlled by the intensified Kuroshio water with upwellings during 7.0-6.0kaBP; from 6.0-2.0ka BP the upwellings developed stably and the thermocline gradually declined: from 6.0-5.0 kaBP the impact of the upwellings mainly focused on the thermocline and much less on the sea surface, from 5.0-4.0kaBP the SST decreased because the sea surface was influenced by the cool water brought by the intensified upwellings; from 2.0-1.2kaBP, the upwelling declined and the SST increased consequently; since 1.2 kaBP the upwelling increased and the thermocline declined obviously.

冲绳海槽北部、九州西南海区,全新世7.5-7.0ka BP陆源物质影响明显, 7.0kaBP前后黑潮侵入并与陆架水强烈混合,7.0-6.0ka BP期间黑潮影响逐渐控制了该区,上升流开始发生,温跃层开始变浅;约在6.0-2.0ka BP之间上升流持续稳定发育,温跃层深度逐渐下降:6.0-5.0ka BP上升流影响作用于温跃层但对表层影响较小,5.0-4.0ka BP海水表层温度受上升流冷水影响降低;而约2.0-1.2ka BP,上升流减弱,海水表层温度回升;近1200年来上升流加强、温跃层深度减小的趋势更加显著。

With eastern Pacific SST as the criterion, SST is low prior to 1976, suggestive of a robust Walker circulation and v.v. for the subsequent years.

根据El Nino发生的海区位置ENSO可划分为两种类型:赤道东太平洋增暖型和中太平洋增暖型。

The SST pattern in the Indian Ocean is warm in the western part and cold in the eastern part when SST in the eastern equatorial Pacific is warm,and v.v.

对应于赤道东太平洋暖位相期,印度洋地区的海温分布为东冷西暖;与此相反,在赤道东太平洋冷位相期,印度洋地区的海温分布为东暖西冷。

Results The effects of killing PC-3 by different dosage (0.2,0.4 and 0.8μg/ml ) of octreotide in transf...

结果 胰腺癌细胞转染SST 2后,不同浓度奥曲肽(0 。2 ,0 。4,0 。8μg/ml)杀伤已转染SST 2的PC 3细胞的能力较杀伤未转染SST 2的PC 3细胞的能力均有明显增强(均P 。0 5 )。

By analyzing next-spring abnormal features of 500 hPa height and 850 hPa, 200 hPa meridional wind due to Nino3 SST rising, it is found that Nino3 SST rising abnormally in the second half year leads to 500 hPa height field rising in the tropic and Northwest Pacific subtropical region, namely the Northwest Pacific subtropical high is stronger and shifts westwards and northwards compared with the mean, and the trough over East Asia is weaker with its location shifts eastwards; the height field falls from the area around Balkhash to Baikal Lake, i.

通过分析下半年Nino3区(150o~90oW,5oS~5oN)海表温度升高引起的次年春季500 hPa高度、850 hPa及200 hPa经向风的异常特征,发现下半年Nino3区显著升温,可导致次年春季热带和西北太平洋副热带地区的500 hPa高度场升高,即西太平洋副热带高压偏强、偏西、偏北,东亚大槽偏弱、偏东;巴尔喀什湖至贝加尔湖的高度场降低,即该地区经常有低槽维持;亚洲至西太平洋地区盛行纬向环流。

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