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评估尼泊尔气候变化情景下的气候边界变化。

Assessing climate boundary shifting under climate change scenarios across Nepal.

机构信息

Department of Hydrology and Meteorology, Government of Nepal, Kathmandu, Nepal.

Disaster Prevention Research Institute, Kyoto University, Kyoto, Japan.

出版信息

Environ Monit Assess. 2019 Jul 29;191(8):520. doi: 10.1007/s10661-019-7644-4.

Abstract

This study assesses the climate boundary shifts from the historical time to near/mid future by using a slightly modified Köppen-Geiger (KG) classification scheme and presents comprehensive pictures of historical (1960-1990) and projected near/mid future (1950s: 2040-2060/1970s: 2060-2080) climate classes across Nepal. Ensembles of three selected general circulation models (GCMs) under two Representative Concentration Pathways (RCP 4.5 and RCP 8.5) were used for projected future analysis. During the 1950s, annual average temperature is expected to increase by 2.5 °C under RCP 8.5. Similarly, during the 1970s, it is even anticipated to rise by 3.6 °C under RCP 8.5. The rate of temperature rise is higher in the non-monsoon period than in monsoon period. During the 1970s, annual precipitation is projected to increase by 8.1% under RCP 8.5. Even though the precipitation is anticipated to increase in the future in annual scale, winter seasons are estimated to be drier by more than 15%. This study shows significant increments of tropical (Am and Aw) and arid (BSk) climate types and reductions of temperate (Cwa and Cwb) and polar (ET and EF). Noticeably, the reduction of the areal coverage of polar frost (EF) is considerably high. In general, about 50% of the country's area is covered by the temperate climate (Cwa and Cwb) in baseline scenario and it is expected to reduce to 45% under RCP 4.5 and 42.5% under RCP 8.5 during the 1950s, and 42% under RCP 4.5 and 39% under RCP 8.5 during the 1970s. Importantly, the degree of climate boundary shifts is quite higher under RCP 8.5 than RCP 4.5, and likewise, the degree is higher during the 1970s than the 1950s. We believe this study to facilitate the identification of regions in which impacts of climate change are notable for crop production, soil management, and disaster risk reduction, requiring a more detailed assessment of adaptation measures. The assessment of climate boundary shifting can serve as valuable information for stakeholders of many disciplines like water, climate, transport, energy, environment, disaster, development, agriculture, and tourism.

摘要

本研究通过略微修改的柯本-盖格尔(Köppen-Geiger)分类方案评估了从历史时期到近/中期未来的气候边界变化,并展示了尼泊尔历史时期(1960-1990 年)和预测的近/中期未来(1950 年代:2040-2060 年/1970 年代:2060-2080 年)气候类型的综合情况。使用三个选定的通用环流模型(GCM)的集合在两种代表性浓度路径(RCP 4.5 和 RCP 8.5)下进行未来预测分析。在 1950 年代,预计 RCP 8.5 下的年平均温度将升高 2.5°C。同样,在 1970 年代,预计 RCP 8.5 下的温度将升高 3.6°C。非季风期的升温速度高于季风期。在 1970 年代,预计 RCP 8.5 下的年降水量将增加 8.1%。尽管预计未来的年降水量会增加,但冬季的干燥程度预计会增加 15%以上。本研究表明,热带(Am 和 Aw)和干旱(BSk)气候类型显著增加,温带(Cwa 和 Cwb)和极地(ET 和 EF)气候类型减少。值得注意的是,极地霜(EF)的面积覆盖率显著降低。一般来说,尼泊尔约 50%的地区处于温带气候(Cwa 和 Cwb),在基准情景下,预计到 1950 年代,RCP 4.5 下将减少到 45%,RCP 8.5 下将减少到 42.5%,到 1970 年代,RCP 4.5 下将减少到 42%,RCP 8.5 下将减少到 39%。重要的是,RCP 8.5 下的气候边界变化程度明显高于 RCP 4.5,而且在 1970 年代的变化程度高于 1950 年代。我们相信,这项研究将有助于识别对作物生产、土壤管理和减少灾害风险具有显著影响的气候变化区域,需要更详细地评估适应措施。气候边界变化的评估可以为许多学科的利益相关者提供有价值的信息,如水利、气候、交通、能源、环境、灾害、发展、农业和旅游。

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