因为大气层负责海洋和空间的水汽交换他建议增建大气和年轻石质星球的地幔相互作用的模型。
Because atmospheres are responsible for releasing water from oceans into space, he suggests additional modeling of the interactions between the atmosphere and mantle of a young rocky planet.
对于理解地球大气、陆地和海洋在真实过程中相互作用的机制及其原因，模型和观测两者都是不可或缺的。
Both are necessary in understanding how and why Earth's atmosphere, land, and oceans function together as they do.
许多这样的相互作用把大气、海洋、冰和陆块彼此联系起来。
Many such interactions link the atmosphere, oceans, ice, and land masses.
它们大多以一千年为一循环周期。这表明太阳的多变性和海洋与大气之间的相互作用是影响这些气候变化的尤为重要的因素。
Many of them occur on thousand-year cycles, indicating that solar variability and interactions between the ocean and atmosphere are especially important factors influencing these climate changes.
海洋潮汐和大气、海洋、海冰之间存在复杂的相互作用，它对地球气候有复杂而深远的影响。
Ocean tides play a significant role in climate due to its complex interactions between ocean, atmosphere, and sea ice.
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.
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.
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.
应用推荐