n. 冰雪融化成的水,冰河融化后的水
网络 冰雪融化成的水; 融水; 溶雪水
Glaciers are open systems, with snow as the system´s input and meltwater as the system´s main output.
冰川是开放系统,雪是系统的输入,融水是系统的主要输出。
With additional time, pressure, and refrozen meltwater from above, the small firn granules become larger, interlocked crystals of blue glacial ice.
随着时间的推移,压力的增加,再加上从上方重新冻结的融水,小冰原颗粒成为相互锁结的大晶体蓝色冰川冰。
Here water may be stored in ice form for hundreds or even hundreds of thousands of years before being released again into the liquid water system as meltwater.
在这里,水可能以冰的形式储存数百年甚至数十万年,然后再以融水的形式释放到液态水系统中。
The theory posited that this meltwater flooded into the North Atlantic, lowering the salinity and intensity of surface waters enough to prevent them from sinking.
该理论假设,这些融水涌入北大西洋,降低了地表水的盐度和强度,足以防止它们下沉。
Warmer temperatures mean more ponds of meltwater on the ice´s surface.
暖空气意味着冰面会形成更多水塘,从而改变冰面的折光系数。