温跃层

基本解释 (translations)

thermocline

与温跃层相关的网络例句 [注：此内容来源于网络，仅供参考]

Based on the reanalysis of JEDAC datasets and the assimilation of SODA, the authors studied the variation of the heat status in the West Pacific Warm pool and discussed the ocean temperature variety in the heat content at different depths, the inherent relations between ocean temperatures at surface and subsurface, the eastward propagation of anomalous ocean temperature and the thermocline variation, and the influence of equatorial undercurrent on the eastward propagation.

中文摘要：应用 JEDAC 海温和SODA 再分析资料，分析研究了西太平洋暖池的热状况变化特征，探讨了WPWP 的热含量变化与不同深度海温变化，特别是与表层和次表层海温场之间的内在联系，分析研究了WPWP 异常海温东传过程中与温跃层变化之间的关系，最后讨论了赤道潜流在异常海温东传过程的作用。

The unsaturation of CO2 in the epilimnion is caused by the fixation of CO2 during the photosynthesis and the sharp increase of CO2 in the metalimnion may be due to the degradation of the photosynthesis production.

其中，温水层CO2欠饱和是光合作用吸收CO2引起的，温跃层中pCO2的急剧增加是光合产物降解产生CO2引起的。

We studied the constraints and impacts of inhomogeneous climatic mean state of Tropical Pacific Ocean on air-sea disturbances using the relationship between the epilimnion and variation of sea bottom orography in the Eastern and Western Pacific Ocean, and provided dynamical explanation.

利用东西太平洋地区海底地形的变化与温跃层之间的关系，研究了热带太平洋非均匀的气候基态对海气扰动形成和发展的影响和制约，并作出了动力学解释。3。

For one-dimensional ocean temperature model, we optimally determined the initial and boundary conditions and related model parameters through variational assimilation method along with inverse problem techniques using incomplete and complete observational data,so as to determine the variation of position of epilimnion which has influences on SST.

由于温跃层的变化对海表温度的影响，我们以简单的海温模式为例，采用变分同化技术及反问题的技巧，在局部和整体观测资料下，对初、边值条件和模式参数等进行最优估计，确定温跃层的位置及其变化规律。4。

The population exhibited a distributional shift in mid July from the upstream, more riverine portion of the reservoir to the cooler area near the dam when epilimnion temperatures upreservoir exceeded 30 _ C.

种群在7月中旬分布转变，水库的分支流域进入接近大坝较冷的区域当温跃层的温度超过30℃。

The relation between the eastward propagation of the ocean temperature anomalies and the thermocline variation along the equator tells that the temperature variation at thermocline lags behind the eastward propagation during which the EUC plays an important role.

由WPWP 异常海温沿赤道东传过程和温跃层变化之间的关系可知，温跃层变化滞后于WPWP 区域东传的异常海温，在WPWP 区域异常海温东传过程中，赤道潜流起了重要作用。

Using a one--dimensional differential thermocline model, we simulated the temperature and thermocline of Yellow and Bohai Sea.

本论文建立了黄渤海环流的三维斜压模式，进行了黄渤海三维环流的数值模拟研究，另外，用一个温跃层一维微分模式对黄渤海的温度及跃层现象进行了数值模拟，最后，建立了一个黄渤海温度及环流的数值模式。

The water at that depth is a constant 4°C, its temperature protected by a layer of water above it called a thermocline.

在这个深度上的湖水一直恒定在摄氏4摄氏度，在其之上的一层水被称为温跃层(较热的水面区与冷的深冷水区之间的水层)，可以保持其的温度。

The down core changes of Florisphaera profunda percentage content implied that the thermocline was shallower in glacial periods and deeper in interglacial periods, which might be the direct controlling factors of WPWP productivity changes. It is speculated that the glacial-interglacial fluctuation of the depth of thermocline was induced by the super-ENSO variation.

钙质超微化石下透光带属种Florisphaeva profunda百分含量指示的温跃层深度变化表明冰期温跃层浅、间冰期温跃层加深，这说明类ENSO式变化导致的冰期-间冰期温跃层深度波动可能是MIS7期以来暖池核心区古生产力在冰期高而在间冰期显著降低的直接控制因素。

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。

与温跃层相关的网络解释 [注：此内容来源于网络，仅供参考]

thermocouple ammeter：热电偶安培表

thermocline 温跃层 | thermocouple ammeter 热电偶安培表 | thermocouple comparator 热电偶比较器

thermocline：温跃层

声音传播的速度在温跃层(Thermocline)达到最大. 研究声波在水中传播的情况对于声纳的使用非常重要. 如果水温是均一的,声音传播速度随深度而增加,导致声波向表面折射或弯曲. 然而由于温跃层的存在,导致形成了一个声波消失带,

thermocline：跃温层

繁殖季主要在冬末春初,於深海底床产卵,卵为浮性卵漂浮至海面上,孵化后之仔稚鱼生活在跃温层(thermocline),幼鱼则随着成长渐降入深海底部(Marshall,1973),除少数种类之大型个体可供食用外,大部份均於捕获后充作下杂鱼来喂食养殖鱼类.

thermocline：温跃层; 斜温层

thermally unstable substance 热不稳定物质 | thermocline 温跃层; 斜温层 | thermodynamic model of climate 气候的热力学模式

permanent thermocline：永久性温跃层

涌浪|swell | 永久性温跃层|permanent thermocline | 优势种|dominant species

permanent thermocline：海洋主温跃层

permanent testing 长期试验 | permanent thermocline 海洋主温跃层 | permanent tissue 永久组织

seasonal thermocline：季节性温跃层

季节变化|seasonal variation | 季节性温跃层|seasonal thermocline | 寄生|parasitism

main thermocline：主[温]跃层

昼夜垂直移动|diel vertical migration, diurnal vertical migration | 主[温]跃层|main thermocline | 主动大陆边缘|active continental margin

traceback depth：的例句

温跃层:depth of thermocline | traceback depth的例句: | traceback depth的全文例句:

seamail：海运信件

seam-weldingmachine 缝焊机 | seamail 海运信件 | seamainthermocline 海洋主温跃层