Science Magazine | AAAS: Science Advances 中文 关注 西风诱导的降水增加驱动青藏高原近地表冻土储量增加，尽管气温正在上升 | Science Advances 青藏高原降水增加导致气候变暖下近地表地下冰意外增加。 Westerly induced precipitation increase drives near-surface ground ice gain on the Tibetan Plateau despite warming | Science Advances science.org
