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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Multiple possibilities for future precipitation changes in Asia under the Paris Agreement
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Multiple possibilities for future precipitation changes in Asia under the Paris Agreement

机译:根据巴黎协议,亚洲未来降水变化的多种可能性

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摘要

Future precipitation changes impact the availability of water resources and related flood and drought events. Recent studies have focused on the variations in precipitation based on the Representative Concentration Pathways scenarios, which do not reflect the current mitigation commitments of the Paris Agreement to stabilize the global mean temperature below the 2.0 degrees C threshold. This paper analyzes the Asian precipitation response to emissions scenarios from warming. This response is a result of the Intended Nationally Determined Contributions (INDC) pledges (as of August 2018), which would satisfy the Paris Agreement target over the next few decades. Our results demonstrate that by the end of 21st century, mean precipitation in Asia will increase by 12.9% (11.7-14.7%) for a delayed action (No-policy) scenario, 8.0% (6.7-8.8%) for a continued mitigation action (continued INDC-pledge) scenario, and 2.4% (1.9-3.5%) and 4.4% (3.7-5.4%) for scenarios that stabilize the global mean temperature at the 1.5 and 2.0 degrees C levels, respectively. The spatial heterogeneity of precipitation changes, however, reflects the complexity of precipitation responses in future climate projections. Furthermore, heavy rainfall events will become stronger as warming increases; however, the trend of dry spell events varies depending on the region. Considering the impacts of precipitation-related extremes, we determined that the projected population exposure to heavy rainfall and dry spell events will significantly increase in most Asian regions. Limiting warming to lower levels (such as 1.5 or 2.0 degrees C) would reduce the population exposure to heavy rainfall, thereby avoiding impacts associated with precipitation extremes. These results contribute to an improved understanding of the risks related to future climate extremes. Such information is crucial for planning mitigation and adaptation activities in Asia, which is home to nearly 60% of the global population.
机译:未来降水变化会影响水资源和相关洪水和干旱事件的可用性。最近的研究专注于基于代表浓度途径情景的降水的变化,这不反映巴黎协议的当前缓解承诺,以稳定在2.0度C阈值以下的全球平均温度。本文分析了对热化的排放情景的亚洲降水响应。这一响应是预期的国家决定捐款(IDIDC)承诺(截至2018年8月),这将在未来几十年内满足巴黎协定目标。我们的结果表明,到21世纪末,亚洲的平均降水将增加12.9%(11.7-14.7%),延迟行动(无政策)情景,8.0%(6.7-8.8%)继续缓解行动(持续的Indcc-prenge)情景,2.4%(1.9-3.5%)和4.4%(3.7-5.4%),方案分别稳定在1.5和2.0摄氏度下的全球平均温度。然而,降水变化的空间异质性反映了未来的气候预测中降水反应的复杂性。此外,随着变暖的增加,大雨事件将变得更强劲;然而,干法术事件的趋势根据该区域而变化。考虑到降水相关极端的影响,我们确定预计人口暴露在大多数亚洲地区的暴雨和干法拼法案中将大大增加。限制升温到较低水平(例如1.5或2.0摄氏度)将减少人口暴露于大雨,从而避免与极端降水相关的影响。这些结果有助于改善对与未来气候极端相关风险的理解。此类信息对于规划亚洲的规划和适应活动至关重要,这些活动是近60%的全球人口的所在地。

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