中尺度海气相互作用的天气现象如台风、入海气旋等在该区域活动频繁。
The mesoscale air-sea interaction weather phenomenon such as typhoon, passing cyclone happens frequently on this area.
这种向东传播的波动出现在波长较长的波段范围内，这个范围的大小受海气相互作用强度的制约。
The eastward propagating waves exist in the scope of comparatively long wavelengths and this scope is governed by the intensity of the air-sea interaction.
本文数值模拟结果表明，ENSO循环的主要动力学过程可由热带海气相互作用系统自身所确定。
The results from this model study indicate that the essential dynamics of the ENSO cycle can be determined by the tropical Pacific coupled ocean-atmosphere system itself.
大气环流与热盐环流(THC)变化之间的因果关系，是海气相互作用研究领域的一个悬而未决的问题。
The causality between atmospheric circulation and thermohaline circulation (THC) is an open question in the field of air-sea interaction.
从简单海气相互作用方程组出发，引进新的海洋对大气加热函数，得到简单海气相互作用方程组的解析解。
From a group of simple air-sea coupled equations, introducing a new heating function of oceans to the air, we get an analytical solution of the air-sea coupled equations.
使用谐波分析及奇异值分解(SVD)方法分析比较了北太平洋、热带太平洋区域的海气资料及海气相互作用。
Diagnostic analysis and contrast are performed in air-sea data and their interaction between the North Pacific and the Tropical Pacific by means of harmonic analysis and SVD.
本文对大气低频振荡的可能机制进行了评述，指出在热带地区应着重考虑积云对流加热和海气相互作用，各种机制间的联系应加强研究。
It is pointed out that in tropical belt cumulus heating and sea-air interaction should be mostly taken into account, and the relations among the mechanisms should be studied more.
例如，如果PD O源于海气相互作用的，需要10年海洋调整时间，然后方面的现象，将(在理论上)是可预测的准备时间长达10年。
For example, if PDO arises from air-sea interactions that require 10 year ocean adjustment times, then aspects of the phenomenon will (in theory) be predictable at lead times of up to 10 years.
海-气间湍流热通量是研究海气相互作用的重要课题，深刻理解海气间湍流热交换有助于进一步耦合大气海洋模式，也有助于进一步研究海洋热量和淡水收支等科学问题。
The sea surface turbulent heat fluxes, as the key subjects of air-sea interaction, are very important for understanding the coupled atmosphere-ocean models and oceanic heat and freshwater budget.
提出SPCZ是反映西太暖池同东太冷舌海气耦合系统以及暖池大气同相邻陆区大气间相互作用的重要特征。
It can be said that the SPCZ represents the air-sea system interaction of the Western Pacific Warm Pool (WPWP) and the eastern Pacific cold tongue, as well as the interaction of.
另外，风速在南海海气非线性相互作用中起着重要作用。
Thus, w is a very important physical factor in the nonlinear interaction of the South China Sea.
另外，风速在南海海气非线性相互作用中起着重要作用。
Thus, w is a very important physical factor in the nonlinear interaction of the South China Sea.
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