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大峡谷地区近期及未来的降水和温度变化及其对地下水资源的影响。

Recent and projected precipitation and temperature changes in the Grand Canyon area with implications for groundwater resources.

机构信息

U.S. Geological Survey, Arizona Water Science Center, Tucson, AZ, USA.

Reclamation, Water Resources Engineering and Management Group, Denver, CO, USA.

出版信息

Sci Rep. 2020 Nov 12;10(1):19740. doi: 10.1038/s41598-020-76743-6.

Abstract

Groundwater is a critical resource in the Grand Canyon region, supplying nearly all water needs for residents and millions of visitors. Additionally, groundwater discharging at hundreds of spring locations in and near Grand Canyon supports important ecosystems in this mostly arid environment. The security of groundwater supplies is of critical importance for both people and ecosystems in the region and the potential for changes to groundwater systems from projected climate change is a cause for concern. In this study, we analyze recent historical and projected precipitation and temperature data for the Grand Canyon region. Projected climate scenarios are then used in Soil Water Balance groundwater infiltration simulations to understand the state-of-the-science on projected changes to groundwater resources in the area. Historical climate data from 1896 through 2019 indicate multi-decadal cyclical patterns in both precipitation and temperature for most of the time period. Since the 1970s, however, a significant rising trend in temperature is observed in the area. All 10-year periods since 1993 are characterized by both below average precipitation and above average temperature. Downscaled and bias-corrected precipitation and temperature output from 97 CMIP5 global climate models for the water-year 2020-2099 time period indicate projected precipitation patterns similar to recent historical (water-year 1951-2015) data. Projected temperature for the Grand Canyon area, however, is expected to rise by as much as 3.4 °C by the end of the century, relative to the recent historical average. Integrating the effects of projected precipitation and temperature changes on groundwater infiltration, simulation results indicate that > 76% of future decades will experience average potential groundwater infiltration less than that of the recent historical period.

摘要

地下水是大峡谷地区的重要资源,为当地居民和数百万游客提供了几乎所有的用水需求。此外,在大峡谷及其周边地区数百个泉水出露点,地下水的排放支撑了这个大部分干旱地区的重要生态系统。地下水供应的安全性对该地区的人和生态系统都至关重要,预计气候变化对地下水系统的潜在影响令人担忧。在本研究中,我们分析了大峡谷地区最近的历史和预测降水和温度数据。然后,利用土壤水分平衡地下水入渗模拟,根据预测的气候变化情景,了解该地区地下水资源变化的现状。1896 年至 2019 年的历史气候数据表明,在大部分时间内,降水和温度都存在数十年的周期性变化。然而,自 20 世纪 70 年代以来,该地区的温度呈显著上升趋势。自 1993 年以来,所有 10 年期间的降水均低于平均值,而温度则高于平均值。对来自 97 个 CMIP5 全球气候模型的经过下推和偏差校正的降水和温度输出进行分析,结果表明,2020 年至 2099 年水年期间的预测降水模式与最近的历史(1951 年至 2015 年水年)数据相似。然而,预计大峡谷地区的温度到本世纪末将上升 3.4°C,与最近的历史平均水平相比。将预测降水和温度变化对地下水入渗的影响进行综合考虑,模拟结果表明,未来几十年中,超过 76%的时间将经历平均潜在地下水入渗量小于最近历史时期的情况。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/794f/7664996/d9696a6d3159/41598_2020_76743_Fig5_HTML.jpg

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