海洋热流 meaning in Chinese
oceanic heat flow
Examples
- The variations of sea ice in the arctic ocean are simulated by using a improved high resolution hibler dynamic - thermodynamic sea ice model during 1979 - 1998 . the model is driven by surface atmospheric and oceanic forcing consists of geostrophic winds , surface air temperature , specific humidity , and longwave and shortwave radiative fluxes provided by international arctic buoy program ( iabp ) . the simulated results show that arctic sea ice have noticeable seasonal and annual variability
利用一个hibler海冰热动力模式，在改进了其热力部分和改变模拟范围以及提高分辨率的基础上，以北极国际浮标计划( iabp )提供的1979 - 1998年间逐日变化的日平均海平面气温场，湿度场，长短波辐射场，风场，洋流场，海洋热流量场为强迫场，模拟了上述20年间北极海冰的时空演变。