昨天，印度环境部长拉梅什对记者说，气候变化将导致喜马拉雅山冰川在2035年前彻底融化的断言没有事实根据。
Yesterdaythe Indian environment minister, Jairam Ramesh, told reporters theclaim that climate change would cause Himalayan glaciers to melt awayby 2035 was unfounded.
自工业化时代刚开始以来，不到1摄氏度的升温引起的环境变化是令人可怕、出人意料的，其中包括冰川消融和前所未有的珊瑚礁退化。
Less than one degree Celsius of warming since the pre-industrial age has unleashed frightening and unforeseen change, including glacier-melt and unprecedented coral-reef degradation.
无论怎样，在冰川下埋藏之后，苔藓复活说明随着环境的变化，有些生命能够复苏。但恢复消失的冰川本身却是更棘手的问题。
Nevertheless, this resurrection after ice entombment displays the resiliency of some life as conditions change. But restoring the disappearing ice itself, well, that's a far trickier matter.
结果表明，宁化地区晚第四纪古气候环境没有形成冰川的条件，但明显受到全球气温变化的控制。
The Late Quaternary paleoclimate environment in Ninghua was not suitable for the development of a glacier, and it was kept under the influence of the global temperature variation.
到目前为止，我们用这种方法监视大地，海洋，冰川和云层已经有10个年头了，我们像医生检查病人生命特征一般记录著地球的环境变化。
Now in its 10th year of monitoring the land, oceans, sea ice and clouds, Terra tracks environmental change like a doctor monitors a patient's vital signs.
到目前为止，我们用这种方法监视大地，海洋，冰川和云层已经有10个年头了，我们像医生检查病人生命特征一般记录着地球的环境变化。
Now in its 10th year of monitoring the land, oceans, sea ice and clouds, Terra tracks environmental change like a doctor monitors a patients vital signs.
结果表明，宁化地区晚第四纪古气候环境没有形成冰川的条件，但明显受到全球气温变化的控制。
P. the Late Quaternary paleoclimate environment in Ninghua was not suitable for the development of a glacier, and it was kept under the influence of the global temperature variation.
冰期中的全球性冰川事件不仅对全球性海平面变化，而且对低纬陆棚碳酸盐环境的沉积作用也有重要影响。
World-wide glacial event in an ice age not only contributes to eustatic sea level changes but also penetrates to the shelf carbonate environments and sedimentation coeval low latitude area.
冰期中的全球性冰川事件不仅对全球性海平面变化，而且对低纬陆棚碳酸盐环境的沉积作用也有重要影响。
World-wide glacial event in an ice age not only contributes to eustatic sea level changes but also penetrates to the shelf carbonate environments and sedimentation coeval low latitude area.
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