Land warming as part of global warming
Land warming as part of global warming
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土地变暖是全球变暖的一部分
DOI：
10.1029/2006eo440003
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发表时间：
2006
期刊：
影响因子：
--
通讯作者：
Shaopeng Huang
中科院分区：
文献类型：
--
作者：
Shaopeng Huang
最近地球表面的变暖在气象记录中有很好的记载。根据世界气象组织的资料，地球表面平均气温在世纪上升了约0.6°C [Jones和Moberg，2003年]。
任何全球尺度的SAT变化都伴随着包括大陆陆块在内的所有主要气候系统组成部分的热状态的变化。根据世界范围内的气象和钻孔温度记录，这项研究表明，20世纪世纪的全球变暖已经向大陆陆块沉积了大量的热能，并导致地下岩石的加热加剧。对全球气候系统的反馈和持续的地表下变暖的长期环境后果仍有待确认。
The recent warming of Earth's surface is well documented in meteorological records. According to the World Meteorological Organization, the Earth's average surface air temperature (SAT) rose about 0.6°C in the twentieth century [Jones and Moberg,2003].
Any global scale variation in SAT is accompanied by variation of the thermal state of all major climate system components including the continental landmasses. Based on worldwide meteorological and borehole temperature records, this study suggests that the twentieth century global warming has deposited a large amount of thermal energy into the continental landmasses, and has resulted in an intensified heating of rocks underground. The feedback to the global climate system and the long-term environmental consequences of the on-going subsurface warming of the land remain to be recognized.