2014年年报

Jürgen Mienert
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引用次数: 0

摘要

CAGE研究北极环境下海底甲烷水合物和相关温室气体释放过程。大量的甲烷水合物,一种类似冰的物质,存在于高压低温的海底。海洋变暖使其可能容易融化。我们知道,以这种方式释放的甲烷是一种强大的温室气体,在过去的地质时代加速了气候变暖。我们的目标是研究它对我们的未来意味着什么。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Annual Report 2014
CAGE studies sub-seabed methane hydrates and related greenhouse gas release processes in Arctic environments. Enormous amounts of methane hydrate, an ice-like substance, exist in the ocean floor at high pressure and low temperature. Ocean warming makes it potentially vulnerable to melting. We know that methane released in this way acted as a powerful greenhouse gas accelerating climate warming in the geological past. We aim to examine what it could mean to our future.
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