Future changes in soil salinization across Central Asia under CMIP6 forcing scenarios

IF 3.6 2区 农林科学 Q2 ENVIRONMENTAL SCIENCES
Xin Dong, Jianli Ding, Xiangyu Ge
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Abstract

Soil salinization is a critical environmental and socio-economic concern with global implications, and its severity is expected to amplify under changing climate. The impact of climate change on salinization in Central Asia is still not fully understood. This study addresses this gap by employing a digital soil mapping (DSM) framework. Cubist, random forest (RF), and quantile regression forests (QRF) are utilized to project variations in soil surface salinity (0-10 cm) in Central Asia from 2025 to 2100 under two shared socio-economic pathways (SSPs): SSP2-4.5 and SSP5-8.5. These models are developed using data from 20 global climate models (GCMs) obtained from the Coupled Model Intercomparison Project Phase 6 (CMIP6). The results reveal that the RF model exhibits superior predictive capability in estimating soil salinity. RF performed on the calibration set with a coefficient of determination (R2) of 0.86, root mean square error (RMSE) of 9.84 and 9.90 dS m−1, ratio of performance to interquartile distance (RPIQ) of 3.09 and 3.07, and a Nash–Sutcliffe efficiency (NSE) of 0.86. The multi-GCM ensemble means revealed the potential for varying degrees of salinization in Central Asia, with higher levels predominantly observed in the southeast and southwest of the study area, particularly downstream of the river and in the lakeside areas. Temporal analysis of soil salinity evolution reveals an overall increase in salinity across the region, with more notable changes projected under SSP5-8.5. Specifically, the projected increase rate in soil salinity for Central Asia was 0.0005 dS m−1/year under SSP2-4.5 and 0.01 dS m−1/year under SSP5-8.5. Turkmenistan is notable for possessing the highest regional average of soil salinity, with the exception of a declining trend observed within this area. The remaining regions of Central Asia exhibit an upward trend in average soil salinity, particularly noteworthy under the SSP5-8.5 scenario, where variations in soil salinity are more obvious. These findings hold significant potential in enhancing our understanding of how Central Asia responds to global change, advances toward sustainable development, and enhances comprehension of the dynamics within the region.

中亚地区土壤盐碱化在 CMIP6 强化情景下的未来变化
土壤盐碱化是一个严重的环境和社会经济问题,具有全球性影响,其严重程度预计将在气候变化的情况下进一步加剧。气候变化对中亚盐碱化的影响仍未得到充分认识。本研究通过采用数字土壤制图(DSM)框架来填补这一空白。研究利用 Cubist、随机森林(RF)和量化回归森林(QRF)预测了中亚地区在两种共同的社会经济路径(SSP)下,2025 年至 2100 年土壤表面盐度(0-10 厘米)的变化:SSP2-4.5 和 SSP5-8.5。这些模型是利用从耦合模式相互比较项目第六阶段(CMIP6)获得的 20 个全球气候模式(GCM)的数据开发的。结果表明,RF 模型在估算土壤含盐量方面表现出卓越的预测能力。RF 模型在校准集上的判定系数 (R2) 为 0.86,均方根误差 (RMSE) 为 9.84 和 9.90 dS m-1,性能与四分位数间距离之比 (RPIQ) 为 3.09 和 3.07,纳什-苏特克利夫效率 (NSE) 为 0.86。多全球大气环流模型的集合平均值显示,中亚地区可能存在不同程度的盐碱化,研究区域的东南部和西南部,尤其是河流下游和湖滨地区的盐碱化程度较高。对土壤盐度演变的时间分析表明,整个地区的盐度总体呈上升趋势,预计在 SSP5-8.5 条件下会出现更明显的变化。具体而言,在 SSP2-4.5 和 SSP5-8.5 条件下,中亚地区土壤盐度的预计增长率分别为 0.0005 dS m-1 /年和 0.01 dS m-1 /年。值得注意的是,土库曼斯坦的土壤盐碱度区域平均值最高,但该地区的土壤盐碱度呈下降趋势。中亚其他地区的平均土壤含盐量呈上升趋势,尤其是在 SSP5-8.5 情景下,土壤含盐量的变化更为明显。这些发现对于加深我们对中亚如何应对全球变化、实现可持续发展的理解,以及加深对该地区内部动态的理解具有重要潜力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Land Degradation & Development
Land Degradation & Development 农林科学-环境科学
CiteScore
7.70
自引率
8.50%
发文量
379
审稿时长
5.5 months
期刊介绍: Land Degradation & Development is an international journal which seeks to promote rational study of the recognition, monitoring, control and rehabilitation of degradation in terrestrial environments. The journal focuses on: - what land degradation is; - what causes land degradation; - the impacts of land degradation - the scale of land degradation; - the history, current status or future trends of land degradation; - avoidance, mitigation and control of land degradation; - remedial actions to rehabilitate or restore degraded land; - sustainable land management.
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