Abstract
In this continuation of his exchange with Brooke about Brooke’s big-picture model of climate change and human response, Harper argues for careful articulation of what kind of Malthusianism Brooke claims, or does not claim, for or against his model. Harper also challenges Brooke’s description of the paleoclimate known as the Roman Climate Optimum as a period dominated by a persistently positive mode of the North Atlantic Oscillation.
Issue Section:
Comment and Controversy
© 2016 by the Massachusetts Institute of Technology and The Journal of Interdisciplinary History, Inc.
2016
MIT Press
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