气候变化背景下尼泊尔甘达基省极端降水时空特征分析

S. Pandey, B. Mishra
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引用次数: 1

摘要

本文对尼泊尔甘达基省的极端降水进行了研究。该研究使用了五个指标来评估气候变化下的极端降水。利用耦合模式比对项目第六阶段(CMIP6)的两个全球气候模式(GCMs)的降水输出对未来6 - 9月降水季(JJAS)和全年日数的极端降水进行了表征。利用北京气候中心和中国气象局的SSP2-4.5和SSP5-8.5情景下的日降水量特征分析极端降水事件;和日本气象研究所(MRI)。考虑到GCM输出具有较大的不确定性和不同的降尺度(包括偏差校正)方法,直接利用GCM输出来寻找未来气候的降水模式变化。对于5年、10年、20年、50年和100年的回归期,采用观测值和预估值分别为24 h和72 h的年最大时间序列来计算回归水平。结果表明,相对于基准年(1995-2014),近期(2021-2040)和远期(2081-2100)简单日强度指数(SDII)呈上升趋势。强降水日数(R50 mm)、强降水日数(R100 mm)、年日最大降水量(RX1day)和年3天最大降水量(RX3day)指数也表现出接近21世纪末极端降水增加的趋势。R50 mm和R100 mm值的近、远未来极端降水日数显著增加(分别为22.6%和63.8%)。Kaski、Nawalparasi东部、Syangja和Tanahun地区的西半部预计将出现过度降水。极端降水的预期增加可能对社会基础设施的长期生存能力以及环境健康构成严重威胁。这些研究的发现将为更好地了解严重事件的起源和CMIP6模式输出估计预期变化的能力提供机会。建议对调节极端事件发生的潜在物理因素进行更多的研究,以期制定相关政策。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spatial and Temporal Analysis of Extreme Precipitation under Climate Change over Gandaki Province, Nepal
This paper presents a research study of expected precipitation extremes across the Gandaki Province, Nepal. The study used five indices to assess extreme precipitation under climate change. Precipitation output of two Global Climate Models (GCMs) of Coupled Model Intercomparison Project Phase Six (CMIP6) were used to characterize the future precipitation extremes during the rainfall season from June to September (JJAS) and overall days of the year. To characterize extreme precipitation events, we used daily precipitation under the SSP2–4.5 and SSP5–8.5 scenarios from the Beijing Climate Center and China Meteorological Administration, China; and Meteorological Research Institute (MRI), Japan. Considering large uncertainties with GCM outputs and different downscaling (including bias correction) methods, direct use of GCM outputs were made to find change in precipitation pattern for future climate. For 5-, 10-, 20-, 50-, and 100-year return periods, observed and projected 24 h and 72 h annual maximum time series were used to calculate the return level. The result showed an increase in simple daily intensity index (SDII) in the near future (2021–2040) and far future (2081–2100), with respect to the base-year (1995–2014). Similarly, heavy precipitation days (R50 mm), very heavy precipitation days (R100 mm), annual daily maximum precipitation (RX1day), and annual three-day maximum precipitation (RX3day) indices demonstrated an increase in extreme precipitation toward the end of the 21st century. A comparison of R50 mm and R100 mm values showed an extensive (22.6% and 63.8%) increase in extreme precipitation days in the near future and far future. Excessive precipitation was forecasted over Kaski, Nawalparasi East, Syangja, and the western half of the Tanahun region. The expected increase in extreme precipitation may pose a severe threat to the long-term viability of social infrastructure, as well as environmental health. The findings of these studies will provide an opportunity to better understand the origins of severe events and the ability of CMIP6 model outputs to estimate anticipated changes. More research into the underlying physical factors that modulate the occurrence of extreme incidences expected for relevant policies is suggested.
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