沿海水域的亮度差异可能是由于其他因素所导致,包括淡水径流,强劲的水流,水的深度以及清澈度。
Differences in brightness in coastal area waters may be due to other factors, including freshwater runoff, strong currents, and water depth and clarity.
体积相对轻的淡水流入海洋后,还会改变格林兰岛和北美洲北部之间的洋流循环模式,这种情况最终可能导致更多的海水淹没北美大陆。
The input of relatively light freshwater also alters circulation patterns that cycle water between Greenland and northern North America, which could lead to more water on the North American end.
世界水循环中,每年平均只有9%的淡水流失。
The global average withdrawal of fresh water was 9% of the amount that flowed through the world’s hydrologic cycle.
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