Glaciers are sometimes classified by temperature as faster-flowing temperate glaciers or as slower-flowing polarglaciers.
冰川有时按温度分为流动较快的温和冰川或流动较慢的极地冰川。
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The melting of glaciers, ice caps and polar ice sheets on land, however, has the potential to account for much more.
然而,陆地上的冰川、冰盖和极地冰盾的融化有更大的潜在力量。
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The rest (approximately 1.7%) is stored in polar ice caps, glaciers, and permanent snow, and another 1.7% in groundwater, lakes, rivers, streams, and soil.