Terhaar Jens, Burger Friedrich A, Vogt Linus, Frölicher Thomas L, Stocker Thomas F
Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland.
Oeschger Center for Climate Change Research, University of Bern, Bern, Switzerland.
Nature. 2025 Mar;639(8056):942-946. doi: 10.1038/s41586-025-08674-z. Epub 2025 Mar 12.
Global ocean surface temperatures were at record levels for more than a year from April 2023 onwards, exceeding the previous record in 2015-2016 by 0.25 °C on average between April 2023 and March 2024. The nearly global extent and unprecedented intensity of this event prompted questions about how exceptional it was and whether climate models can represent such record-shattering jumps in surface ocean temperatures. Here we construct observation-based synthetic time series to show that a jump in global sea surface temperatures that breaks the previous record by at least 0.25 °C is a 1-in-512-year event under the current long-term warming trend (1-in-205-year to 1-in-1,185-year event; 95% confidence interval). Without a global warming trend, such an event would have been practically impossible. Using 270 simulations from a wide range of fully coupled climate models, we show that these models successfully simulate such record-shattering jumps in global ocean surface temperatures, underpinning the models' usefulness in understanding the characteristics, drivers and consequences of such events. These model simulations suggest that the record-shattering jump in surface ocean temperatures in 2023-2024 was an extreme event after which surface ocean temperatures are expected to revert to the expected long-term warming trend.
自2023年4月起,全球海洋表面温度连续一年多处于创纪录水平,在2023年4月至2024年3月期间,平均比2015 - 2016年的前纪录高出0.25°C。这一事件几乎覆盖全球且强度空前,引发了人们对其异常程度以及气候模型能否呈现海洋表面温度这种破纪录跃升的疑问。在此,我们构建基于观测的合成时间序列,以表明在当前长期变暖趋势下,全球海表温度跃升至少0.25°C并打破此前纪录的事件是512年一遇的事件(205年一遇至1185年一遇的事件;95%置信区间)。若无全球变暖趋势,这样的事件几乎不可能发生。通过对一系列完全耦合气候模型进行270次模拟,我们表明这些模型成功模拟了全球海洋表面温度这种破纪录的跃升,这证明了模型在理解此类事件的特征、驱动因素和后果方面的有用性。这些模型模拟表明,2023 - 2024年海洋表面温度的破纪录跃升是一次极端事件,之后海洋表面温度预计将恢复到预期的长期变暖趋势。