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DOI10.1126/science.aad8550
Response to Comment on "long-term climate forcing by atmospheric oxygen concentrations"
Poulsen C.J.; Tabor C.; White J.
发表日期2016
ISSN0036-8075
卷号353期号:6295
英文摘要Goldblatt argues that a decrease in pressure broadening of absorption lines in an atmosphere with low oxygen leads to an increase in outgoing longwave radiation and atmospheric cooling. We demonstrate that cloud and water vapor feedbacks in a global climate model compensate for these decreases and lead to atmospheric warming.
英文关键词oxygen; water vapor; absorption; atmospheric pressure; climate forcing; climate modeling; global climate; global warming; longwave radiation; oxygen; water vapor; air temperature; Article; boundary layer; climate; cloud; cooling; humidity; oxygen concentration; positive feedback; priority journal; radiation; warming; water vapor; atmosphere; theoretical model; Atmosphere; Climate; Models, Theoretical; Oxygen; Steam
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/245126
作者单位Department of Earth and Environmental Sciences, University of Michigan, Ann Arbor, MI 48109, United States; National Center for Atmospheric Research (NCAR), Boulder, CO 80305, United States; Department of Biology, Baylor University, Waco, TX 76798, United States
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Poulsen C.J.,Tabor C.,White J.. Response to Comment on "long-term climate forcing by atmospheric oxygen concentrations"[J],2016,353(6295).
APA Poulsen C.J.,Tabor C.,&White J..(2016).Response to Comment on "long-term climate forcing by atmospheric oxygen concentrations".Science,353(6295).
MLA Poulsen C.J.,et al."Response to Comment on "long-term climate forcing by atmospheric oxygen concentrations"".Science 353.6295(2016).
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