The study of indirect evidence focuses on morphometry analysis and snowline reconstruction based on the palaeoclimate.
间接证据的研究方法很多,一般多赖查、性分 析和以古气候资讯为基础的雪线重建。
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That forms the snowline, which occurs at different heights around the planet depending on climate.
这使线得以形成。地球上线高度有所不同是依据气候所致。
They form above the snowline, or the lowest elevation where there’s ice and snow all year round.
它们形成在线之上,或者是全年都有最低海拔。
Secondly, the mountain lies near the tropics, so the snowline is high, and the glaciers relatively small, barely big enough to widdle it down.
其次,这座山位于热带附近,所以线较高,且川相对较小,不太可能大到把它冲下来。
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