Skip to main content
dPanther Home
|
Sea Level Rise
mydPanther Home
Low simulated radiation limit for runaway greenhouse climates
Item menu
Print
Send
Add
Share
Description
Standard View
MARC View
Metadata
Usage Statistics
STANDARD VIEW
MARC VIEW
METADATA
USAGE STATISTICS
Permanent Link:
http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15060336/00001
Material Information
Title:
Low simulated radiation limit for runaway greenhouse climates
Series Title:
Nature Geoscience- Volume 6
Creator:
Colin Goldblatt
Tyler D. Robinson
Kevin J. Zahnle
David Crisp
Affiliation:
University of Victoria -- School of Earth and Ocean Sciences
University of Washington -- Astronomy Department
NASA Ames Research Center -- Space Science and Astrobiology Division
Jet Propulsion Laboratory
Publication Date:
2013-08
Language:
English
Subjects
Subjects / Keywords:
climate change
greenhouse gases
solar radiation
troposphere
Notes
Abstract:
The atmospheres of terrestrial planets are expected to be in long-term radiation balance: an increase in the absorption of solar radiation warms the surface and troposphere, which leads to a matching increase in the emission of thermal radiation. Warming a wet planet such as Earth would make the atmosphere moist and optically thick such that only thermal radiation emitted from the upper troposphere can escape to space. Hence, for a hot moist atmosphere, there is an upper limit on the thermal emission that is unrelated to surface temperature. If the solar radiation absorbed exceeds this limit, the planet will heat uncontrollably and the entire ocean will evaporate—the so-called runaway greenhouse. Here we model the solar and thermal radiative transfer in incipient and complete runaway greenhouse atmospheres at line-by-line spectral resolution using a modern spectral database.We find a thermal radiation limit of 282Wm2 (lower than previously reported) and that 294Wm2 of solar radiation is absorbed (higher than previously reported). Therefore, a steam atmosphere induced by such a runaway greenhouse may be a stable state for a planet receiving a similar amount of solar radiation as Earth today. Avoiding a runaway greenhouse on Earth requires that the atmosphere is subsaturated withwater, and that the albedo effect of clouds exceeds their greenhouse effect. A runaway greenhouse could in theory be triggered by increased greenhouse forcing, but anthropogenic emissions are probably insufficient.
Record Information
Source Institution:
Florida International University
Rights Management:
Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
dpSobek Membership
Aggregations:
Sea Level Rise
***This is default web skin for this SobekCM digital library.
Developed for the
University of Florida Digital Collections
For any questions about this system, email
Mark.V.Sullivan@gmail.com
Last updated January 2012 -
4.10.1