Climate Change Research Team, National Institute of Meteorological Sciences, Jeju, Republic of Korea.
PLoS One. 2022 Jun 3;17(6):e0269267. doi: 10.1371/journal.pone.0269267. eCollection 2022.
The East Asian summer monsoon (EASM) is an influential monsoon system that provides two-thirds of the annual precipitation in the Asian region. Therefore, considerable attention has been paid to the changes in future climate. Thus far, studies on EASM characteristics have not been conducted considering specific global warming level (GWL) using Coupled Model Inter-comparison Project 6 (CMIP6) simulations. We analyze the EASM characteristics in present-day (PD) and the changes in EASM corresponding to the projections at 1.5, 2.0, and 3.0°C GWLs. The newly released 30 CMIP6 models effectively captured the migration of the monsoon in PD with a pattern correlation coefficient of 0.91, which is an improvement over that reported in previous studies. As a result of the separate analysis of the P1 (first primary peak; 33-41 pentad) and P2 (from P1 to the withdrawal; 42-50 pentad) periods, a higher frequency of weak to moderate precipitation in P2 and a smaller amount of moderate to extreme precipitation in P1 are mainly occurred. The CMIP6 models project increasing precipitation of approximately 5.7%°C-1, 4.0%°C-1, and 3.9%°C-1 for the three GWLs, respectively, with longer durations (earlier onset and delayed termination). Under the three GWLs, the projected precipitation frequency decreases below 6 mm d-1 (76th percentile) and significant increases above 29 mm d-1 (97th percentile). These changes in precipitation frequency are associated with an increasing distribution of precipitation amount above 97th percentile. Additionally, these tendencies in P1 and P2 are similar to that of the total period, while the maximum changes occur in 3.0°C GWL. In particular, future changes in EASM accelerate with continuous warming and are mainly affected by enhanced extreme precipitation (above 97th percentile). Our findings are expected to provide information for the implementation of sustainable water management programs as a part of national climate policy.
东亚夏季风(EASM)是一个有影响力的季风系统,为亚洲地区提供了三分之二的年降水量。因此,人们对未来气候的变化给予了相当大的关注。到目前为止,使用耦合模式比较计划第六阶段(CMIP6)模拟,还没有针对特定全球变暖水平(GWL)的东亚夏季风特征研究。我们分析了现今(PD)的东亚夏季风特征以及在 1.5、2.0 和 3.0°C GWL 下的东亚夏季风变化的预测。新发布的 30 个 CMIP6 模型有效地捕捉到了 PD 季风的迁移,模式相关系数为 0.91,这比以前的研究有所提高。通过对 P1(第一主峰值;33-41 候)和 P2(从 P1 到撤退;42-50 候)两个时期的单独分析,发现 P2 时期弱到中度降水的频率较高,而 P1 时期中等到极端降水的量较小。CMIP6 模型预测,在这三个 GWL 下,降水分别增加约 5.7%°C-1、4.0%°C-1 和 3.9%°C-1,持续时间更长(开始更早,结束更晚)。在这三个 GWL 下,预测的降水频率下降到 6 毫米/天以下(第 76 百分位数),显著增加到 29 毫米/天以上(第 97 百分位数)。降水频率的这些变化与降水总量超过第 97 百分位数的分布增加有关。此外,P1 和 P2 的这些趋势与总时段的趋势相似,而最大变化发生在 3.0°C GWL。特别是,东亚夏季风的未来变化随着持续变暖而加速,主要受增强的极端降水(超过第 97 百分位数)影响。我们的研究结果有望为国家气候政策下可持续水资源管理计划的实施提供信息。