Preprints
https://doi.org/10.5194/egusphere-2024-3090
https://doi.org/10.5194/egusphere-2024-3090
16 Oct 2024
 | 16 Oct 2024
Status: this preprint is open for discussion.

Long-term impacts of global temperature stabilization and overshoot on exploited marine species

Anne L. Morée, Fabrice Lacroix, William W. L. Cheung, and Thomas L. Frölicher

Abstract. Global warming alters ocean conditions, which can have dramatic consequences for marine species. Yet, the centennial-scale effects and reversibility of habitat viability for marine species, particularly those that are important to fisheries, remain uncertain. Using the Aerobic Growth Index, we quantify the impacts of warming and deoxygenation on the contemporary habitat volume of 46 exploited marine species in novel temperature stabilization and overshoot simulations until 2500. We demonstrate that only around half the simulated loss of contemporary (1995–2014) habitat volume is realized when warming levels are first reached. Moreover, in an overshoot scenario peaking at 2 °C global warming before stabilizing at 1.5 °C, the maximum decrease in contemporary habitat volume occurs more than 150 years post-peak warming. Species’ adaptation may strongly mitigate impacts depending on adaptation rate and pressure. According to our study, marine species will be affected for centuries after temperature stabilization and overshoot, with impacts surpassing those during the transient warming phase.

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Anne L. Morée, Fabrice Lacroix, William W. L. Cheung, and Thomas L. Frölicher

Status: open (until 27 Nov 2024)

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Anne L. Morée, Fabrice Lacroix, William W. L. Cheung, and Thomas L. Frölicher
Anne L. Morée, Fabrice Lacroix, William W. L. Cheung, and Thomas L. Frölicher

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Short summary
Using novel Earth system model simulations and applying the Aerobic Growth Index, we show that only about half of the habitat loss for marine species is realized when temperature stabilization is initially reached. The maximum habitat loss happens over a century after peak warming in an overshoot scenario peaking at 2 °C before stabilizing at 1.5 °C. We also emphasize that species adaptation may play a key role in mitigating the long-term impacts of temperature stabilization and overshoot.