Publication:
Long-Term Global Heating from Energy Usage

Thumbnail Image

Date

2008

Published Version

Journal Title

Journal ISSN

Volume Title

Publisher

Wiley-Blackwell
The Harvard community has made this article openly available. Please share how this access benefits you.

Research Projects

Organizational Units

Journal Issue

Citation

Chaisson, Eric J. 2008. “Long-Term Global Heating from Energy Usage.” Eos Trans. AGU 89 (28): 253. doi:10.1029/2008eo280001.

Research Data

Abstract

Even if civilization on Earth stops polluting the biosphere with greenhouse gases, humanity could eventually be awash in too much heat, namely, the dissipated heat by-product generated by any nonrenewable energy source. Apart from the Sun's natural aging—which causes an approximately 1% luminosity rise for each \(10^{8}\) years and thus about 1°C increase in Earths surface temperature—well within 1000 years our technological society could find itself up against a fundamental limit to growth: an unavoidable global heating of roughly 3°C dictated solely by the second law of thermodynamics, a biogeophysical effect often ignored when estimating future planetary warming scenarios.

Description

Other Available Sources

Keywords

Biogeophysics, Biosphere/atmosphere interactions, Thermodynamics

Terms of Use

This article is made available under the terms and conditions applicable to Other Posted Material (LAA), as set forth at Terms of Service

Endorsement

Review

Supplemented By

Referenced By

Related Stories