Accurate typhoon sea surface wind is the key point to obtain true wave and storm tide.
准确的台风海面风场是获得比较真实的海浪、风暴潮等海洋现象的关键所在。
A history and current situation on numerical prediction of sea surface wind field in NMEFC is introduced briefly.
本文简要介绍了国家海洋环境预报中心海面风场数值预报的历史和现状。
The accurate sea surface wind forecasting is the important guarantee for ship's safe navigation and typhoon evasion.
准确的海面风速预报是舰艇航行安全和防台工作的重要保证。
By contrasting these simulative results, the experiments check up the forcing of heat flux and complex terrain to sea surface wind.
通过模拟试验对比，以检验地形，感热，潜热对海面风风速、风向的强迫作用。
In this paper, also the primary applications of EOF and SVD in analyzing satellite altimeter data of sea surface wind and wave is studied.
本文还就经验正交展开和奇异值分解方法在卫星高度计海面风、浪资料分析中的应用作了初步探时。
Then some applications of marine remote sensing to monitoring seaice, ocean color and sea surface wind speed field were mainly introduced;
以海冰冰清，海面风场，海洋水色等的监测为代表，重点介绍了海洋遥感的应用；
An advanced operational numerical prediction system has been developed to predict limited region sea surface wind field on the work station.
本文简要介绍了在工作站上运行有限区域海面风场数值预报业务化系统的情况。
The sea surface wind speed is an important parameter of Marine environment and satellite microwave radiometer is an important tool to monitor this parameter.
海面风速是海洋环境的重要参数，微波辐射计是卫星监测海面风速的重要手段。
The sea surface wind stress and net heat flux affect the seasonal variation of water mass character in the PN section by changing the mixed layer depth every season.
海面风场和净热通量场通过改变混合层的深度影响障碍层深度的季节变化，而海面降水对于季节平均的障碍层分布和变化都没有显著的影响。
The sea surface wind stress and net heat flux in the PN section affect the seasonal variation of the barrier layer depth by changing the mixed layer depth every season.
海面风场和净热通量场通过改变混合层的深度影响障碍层深度的季节变化，而海面降水对于季节平均的障碍层分布和变化都没有显著的影响。
The apps show sea surface height, sea surface wind, areas of overfishing, oceanic currents, and other non-Google Earth projects that graphically illustrate Marine pollution.
这些应用可以显示洋面高度、海风、过度捕鱼的区域、洋流，以及显示海洋污染的非google Earth内容。
If sounding data or predicted weather data are available, the model may be suitable to provide sea surface wind forecast in application of environmental problems for archipelagic waters.
提供的探空观测或天气尺度预报场，适合在群岛海域的海洋环境问题应用中使用。
Normal swells, known technically as gravity waves, are created by wind pushing the surface of the sea up and gravity then pulling it down, causing it to bounce.
一般的波浪，技术上被成为重力波，是由于风推动着海洋表面上升而后又在重力的作用下被拉向下方，这便会导致海水的回弹。
Besides being steady and strong, downslope winds can also be cold, and the frigid wind over the ocean surface has helped form fresh sea ice in areas where older ice was blown out to sea.
下行风除了强烈和稳定，还具有低温的特点，这股寒流风吹过海面之后，在那些已形成海冰被吹出海域的地方，新的海冰就形成了。
A typical ocean wave forms when wind produces a ripple across the surface of the sea.
风掠过海面时产生水波就形成了典型的海浪。
The curved surface rises along the shoreline, blocking the sea wind.
弯曲的表面沿着海岸线蔓延，将海风挡住。
Generally sea surface is fluctuant and influenced easily by wind or other acting force, which reduces received optical power seriously and raises the requirement of receiver performance.
通常海水界面不是平静的水平面，容易受到风力或其他外力的影响，产生随机起伏，降低接收光功率，由此提高了对接收机的要求。
The computer models combine information on ocean warming, sea surface temperatures, wind and rainfall levels.
计算机模型结合海洋升温信息，海平面温度信息，风和降雨量信息。
The emulational results based on this model shown that it is a go od model to explain the effect on IR passive imaging of sea surface by wind.
本文在研究海面的红外成像特性中，建立了基于刚体的双尺度成像模型，从被动成像方面讨论了海面辐射特性的变化规律。
Theoretical interpretation of sea surface emission signatures provides the potential possibility to facilitate ocean wind vector retrieval using purely passive means.
风成海面的极化辐射特性提供了利用被动微波遥感手段反演海洋风场的途径。
With the farther decline of the paleo monsoon and the rise of the sea surface, the east north wind from the shelf was the cold wet air stream.
随着古季风活动的进一步衰退和海面的不断升高，来自陆架区的东北风变为冷湿气流。
Results of calculation show that the differences of the sea surface effective radiation between cloudy and clear skys are very large, but their variations with the changes of wind speed are small.
结果表明，晴天与阴天的海面有效辐射值相差较大，可是它们随海面风速的变化均甚小。
The responses of sea surface temperature (SST) in the western equatorial Pacific warm pool to the westerly wind bursts (WWBs) play an important role in the relationship between WWB and ENSO.
赤道西大平洋暖池海表温度(SST)对西风爆发(WWB)的响应是WWB与ENSO相互作用的一个重要环节。
The main conclusions are as follow: 1. The wind stress of sea surface is one dynamical factor of thermocline, which has important effect on intensity and depth of the seasonal thermocline.
主要结果如下：海表风应力是影响温跃层的动力因子，对季节性温跃层的深度和强度均有重大影响，但对大洋温跃层的影响不大；
The main conclusions are as follow: 1. The wind stress of sea surface is one dynamical factor of thermocline, which has important effect on intensity and depth of the seasonal thermocline.
主要结果如下：海表风应力是影响温跃层的动力因子，对季节性温跃层的深度和强度均有重大影响，但对大洋温跃层的影响不大；
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