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      Closer limits to human tolerance of global heat

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          Most cited references19

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          The burden of heat-related mortality attributable to recent human-induced climate change

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            An adaptability limit to climate change due to heat stress.

            Despite the uncertainty in future climate-change impacts, it is often assumed that humans would be able to adapt to any possible warming. Here we argue that heat stress imposes a robust upper limit to such adaptation. Peak heat stress, quantified by the wet-bulb temperature T(W), is surprisingly similar across diverse climates today. T(W) never exceeds 31 degrees C. Any exceedence of 35 degrees C for extended periods should induce hyperthermia in humans and other mammals, as dissipation of metabolic heat becomes impossible. While this never happens now, it would begin to occur with global-mean warming of about 7 degrees C, calling the habitability of some regions into question. With 11-12 degrees C warming, such regions would spread to encompass the majority of the human population as currently distributed. Eventual warmings of 12 degrees C are possible from fossil fuel burning. One implication is that recent estimates of the costs of unmitigated climate change are too low unless the range of possible warming can somehow be narrowed. Heat stress also may help explain trends in the mammalian fossil record.
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              The emergence of heat and humidity too severe for human tolerance

              Humid heat extremes are rapidly increasing and may have already briefly exceeded humans’ physiological survivability limit.
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                Author and article information

                Contributors
                Journal
                Proc Natl Acad Sci U S A
                Proc Natl Acad Sci U S A
                PNAS
                Proceedings of the National Academy of Sciences of the United States of America
                National Academy of Sciences
                0027-8424
                1091-6490
                13 October 2023
                24 October 2023
                13 April 2024
                : 120
                : 43
                : e2316003120
                Affiliations
                [1] aClimate Change Research Centre, University of New South Wales , Sydney, NSW 2052, Australia
                [2] bAustralian Research Council Centre of Excellence for Climate Extremes, University of New South Wales , Sydney, NSW 2052, Australia
                [3] cAsian School of the Environment and Earth Observatory of Singapore, Nanyang Technological University , Singapore 639798, Singapore
                Author notes
                2To whom correspondence may be addressed. Email: s.sherwood@ 123456unsw.edu.au .

                1S.C.S. and E.E.R. contributed equally to this work.

                Author information
                https://orcid.org/0000-0001-7420-8216
                https://orcid.org/0000-0002-3621-4698
                Article
                202316003
                10.1073/pnas.2316003120
                10614209
                37831746
                2dbd6e28-854b-4800-8e6d-a59906ad3f8c
                Copyright © 2023 the Author(s). Published by PNAS.

                This article is distributed under Creative Commons Attribution-NonCommercial-NoDerivatives License 4.0 (CC BY-NC-ND).

                History
                Page count
                Pages: 3, Words: 1410
                Funding
                Funded by: ARC Centre of Excellence for Climate Extremes;
                Award ID: CE170100023
                Award Recipient : Steven C Sherwood
                Categories
                comm, Commentary
                env-sci-phys, Environmental Sciences
                env-sci-bio, Environmental Sciences
                417
                417
                437
                Commentary
                Physical Sciences
                Environmental Sciences
                Biological Sciences
                Environmental Sciences

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