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南水北调中线工程水源区雨季降水的变化特征及其未来预估

Rainy Season Precipitation Changes and Projections in the Water Source Area of the South-to-North Water Diversion Middle Route Project

  • 摘要: 南水北调中线工程是我国为缓解北方水资源短缺而实施的跨流域调水工程,于2014年12月正式通水,其水源区位于丹江口库区及上游地区。极端降水事件对工程水资源安全有重要影响。本文首先利用1961~2021年逐日降水观测数据,分析了水源区雨季(5~10月)极端降水事件的变化特征。随后,选用参加政府间气候变化专门委员会(IPCC)第六次国际耦合模式比较计划(CMIP6),三种共享社会经济路径(SSP1-2.6、SSP2-4.5和SSP5-8.5)下,12个模式的未来逐日降水预估数据,开展了近期(2026~2050年)和远期(2071~2100年)预估。考虑模式降水偏差,预估前对模式降水进行了delta分位数映射(QDM)误差订正。结果显示:(1)过去61 a,水源区降水频次(RD)减少,暴雨日数(Rr25)和极端降水量(R95PTOT)增多。降水强度(SDII)以0.19 mm d−1 (10 a) −1速率显著增加,尤其是在大巴山和秦岭之间的安康及其上游地区。水汽收支诊断表明,垂直水汽平流项对SDII的增加具有显著正贡献,其中又以动力项贡献最大,非线性项为其次;(2)暴雨日数(Rr25)、单日最大降水量(Rx1day)、极端降水量(R95PTOT)、特极端降水量(R99PTOT)和降水强度(SDII)在1970年代后期发生年代际突变后,于1980年代显著增加;(3)相较于参考期(1961~2014),在低(中、高)排放情境下,近期和远期暴雨日数(Rr25)分别增加10.8%和19.0%(5.0%和19.2%;7.9%和31.8%),极端降水量(R95PTOT)分别增加8.7%和14.7%(2.9%和15.3%;6.4%和26.8%)。空间分布上,伏牛山及丹江口水库区域的极端降水增加更为显著。总之,过去61 a观测资料分析及CMIP6未来预估来看,水源区汛期总降水呈现增加趋势,有利于工程发挥可持续效益,但极端降水增加,给水资源调配和工程安全带来挑战。

     

    Abstract: The Middle Route of the South-to-North Water Diversion Project is a major inter-basin water transfer project in China designed to alleviate water shortages in northern regions. It has been in operation since December 2014, with its water source area located in the Danjiangkou Reservoir and its upstream areas. Extreme precipitation events carry considerable implications for its water resource security. This study analyzed the characteristics of extreme precipitation events during the rainy season (May–October) in the water source area using daily precipitation data from 1961 to 2021. Subsequently, future projections for the near term (2026–2050) and long term (2071–2100) were conducted using daily precipitation estimates from 12 models under 3 Shared Socioeconomic Pathways (SSP1-2.6, SSP2-4.5, and SSP5-8.5) of the Intergovernmental Panel on Climate Change’s Coupled Model Intercomparison Project Phase 6 (CMIP6). Considering model precipitation biases, the quantile delta mapping bias correction algorithm was applied before projections. The results reveal the following: (1) In the past 61 years, precipitation frequency (RD) decreased while heavy rain days (Rr25) and extreme precipitation (R95PTOT) increased. Precipitation intensity (SDII) increased substantially at the rate of 0.19mm d−1 (10 a) −1, especially in Ankang and its upstream regions between the Daba Mountains and the Qinling Mountains. According to the moisture budget diagnosis, the vertical moisture advection term made the dominant contribution to the increase in SDII, with the largest contribution from the dynamic term, followed by the nonlinear term. (2) Rr25, maximum 1-day precipitation (Rx1day), R95PTOT, very extreme precipitation (R99PTOT), and SDII experienced an interdecadal shift in the late 1970s, followed by a significant increase during the 1980s. (3) Compared with the reference period (1961–2014), under low (medium and high) emission scenarios, Rr25 increased by 10.8% and 19.0% (5.0% and 19.2%; 7.9% and 31.8%) for the near and long term, respectively, and R95PTOT increased by 8.8% and 8.7% (1.1% and 12.7%; 8.6% and 25.1%), respectively. Spatially, the most pronounced increases in extreme precipitation occurred in the Funiu Mountains and the Danjiangkou Reservoir. In summary, analyses of observational data over the past 61 years and future projections from CMIP6 indicate that total precipitation during the flood season in the water source area shows an increasing trend, which is beneficial for the sustainability of the South-to-North Water Diversion Project. However, the increase in extreme precipitation poses challenges for water resource management and engineering safety.

     

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