Doerr School of Sustainability, Stanford University, Stanford, CA 94305.
Department of Atmospheric Science, Colorado State University, Fort Collins, CO 80523.
Proc Natl Acad Sci U S A. 2023 Feb 7;120(6):e2207183120. doi: 10.1073/pnas.2207183120. Epub 2023 Jan 30.
Leveraging artificial neural networks (ANNs) trained on climate model output, we use the spatial pattern of historical temperature observations to predict the time until critical global warming thresholds are reached. Although no observations are used during the training, validation, or testing, the ANNs accurately predict the timing of historical global warming from maps of historical annual temperature. The central estimate for the 1.5 °C global warming threshold is between 2033 and 2035, including a ±1σ range of 2028 to 2039 in the Intermediate (SSP2-4.5) climate forcing scenario, consistent with previous assessments. However, our data-driven approach also suggests a substantial probability of exceeding the 2 °C threshold even in the Low (SSP1-2.6) climate forcing scenario. While there are limitations to our approach, our results suggest a higher likelihood of reaching 2 °C in the Low scenario than indicated in some previous assessments-though the possibility that 2 °C could be avoided is not ruled out. Explainable AI methods reveal that the ANNs focus on particular geographic regions to predict the time until the global threshold is reached. Our framework provides a unique, data-driven approach for quantifying the signal of climate change in historical observations and for constraining the uncertainty in climate model projections. Given the substantial existing evidence of accelerating risks to natural and human systems at 1.5 °C and 2 °C, our results provide further evidence for high-impact climate change over the next three decades.
利用基于气候模型输出的人工神经网络 (ANNs),我们使用历史温度观测的空间模式来预测达到全球变暖关键阈值的时间。虽然在训练、验证或测试过程中没有使用任何观测数据,但 ANN 可以根据历史年度温度图准确预测历史全球变暖的时间。在中等 (SSP2-4.5) 气候强迫情景下,1.5°C 全球变暖阈值的中心估计值在 2033 年至 2035 年之间,包括 2028 年至 2039 年的±1σ范围,这与之前的评估一致。然而,我们的数据驱动方法也表明,即使在低 (SSP1-2.6) 气候强迫情景下,超过 2°C 阈值的可能性也很大。尽管我们的方法存在局限性,但我们的结果表明,在低情景下达到 2°C 的可能性高于一些之前评估所表明的可能性——尽管不能排除避免 2°C 的可能性。可解释人工智能方法表明,ANN 专注于特定地理区域来预测达到全球阈值的时间。我们的框架提供了一种独特的数据驱动方法,用于量化历史观测中气候变化的信号,并限制气候模型预测的不确定性。鉴于在 1.5°C 和 2°C 时自然和人类系统面临风险加速的大量现有证据,我们的结果为未来三十年的高影响气候变化提供了进一步的证据。