海洋上层 meaning in Chinese
u er layer of the ocea
u er ocean
u erlayeroftheocea
u erocean
upper layer of the oceans
Examples
- Thus , as the ocean becomes more and more acidic , the upper , shell - friendly portion will become thinner
因此，随著海洋越来越酸，海洋上层利于有壳生物存活的部份会变薄。 - ( 2 ) ln winter of the northern hemisphere , because of the difference in the land - ocean distribution , the temperature nowadays is lower than that of 14mab . p . simulated in the upper layer but higher in the middle layer ( about 200 - 1500m ) . in deep ocean the discrepancy of temperature seems hardly to be obvious
( 2 )北半球冬季，由于海陆分布的差异使得海温在海洋上层古海温要暖于现代，在海洋中上层(约200 ? 1500米)现代的海温则要暖于14mab - But only for the closure of indonesia passage , warm pool can be formed under 150m with the center between 300m and 600m or so while in upper layer the modern sea temperature is still colder , so seen from the simulation , only the open of indonesia passage can not form the warm pool like the present
P )模拟的海温要暖，形成浅层暖池。但单是上述通道关闭，暖池只形成在150米以下，中心在300 ? 600米深海洋层，而海洋上层( 150米以上)仍为现代冷。依数值模拟来看，只有上述通道的开启，并不能形成如现代浅层海洋暖池。 - In this text , according to south china sea ( scs ) hydrology investigation data , including the nansen data , bt and ctd data , thermocline distribution of scs and its characteristics have been studied . at same time , with the data of sun " s thermal radiation , air temperature , and other weather data the ocean thermocline has been calculated . the research involves the following aspects : large - scale data processing method ; data quality control ; thermocline identification and statistics method ; thermocline map ; thermocline influence factors of scs ; thermocline results comparison using nansen data and bt data ; thermocline forecast
研究涉及到以下几个方面：大规模资料的处理方法、质量控制；温跃层的计算机识别、温跃层的统计分类方法；南海温跃层三项示性特征图的绘制；南海温度跃层的影响因素、南海温度跃层的分布状况；南森资料与bt资料计算南海温跃层的结果比较；海洋上层温度结构模式及计算等。