气候学家们还以同样方法模拟了当今发生的极端降雨型(干旱后随之而来的是洪水，而不是均匀分布的降雨)以及北冰洋的融冰现象。
Similar analyses have been done for today's extreme rainfall patterns (drought followed by deluge, not precipitation spread out evenly) and the retreat of arctic sea ice.
前人的研究结果表明，这个封闭型大湖的水位及水量平衡的变化敏感地记录了发生在过去不同时间尺度上的气候变化幅度。
The former research results indicated that the lake level and water balance changing of this closed large water body sensitively record the paleoclimatic variations on different time scales.
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