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中国西北高寒山区径流变化受多种区域环境因素的综合影响。

The runoff changes are controlled by combined effects of multiple regional environmental factors in the alpine hilly region of Northwest China.

作者信息

Zuo Yafan, Chen Jianhong, Lin Sha, He Kangning

机构信息

Beijing Forestry University, School of Soil and Water Conservation, Beijing 100083, China; Key Laboratory of State Forestry Administration on Soil and Water Conservation, Beijing 100083, China; Beijing Engineering Research Center of Soil and Water Conservation, Beijing 100083, China; Engineering Research Center of Forestry Ecological Engineering of Ministry of Education, Beijing 100083, China.

Qinghai water conservancy and Hydropower Research Institute Co., Ltd, Xining 810000, China.

出版信息

Sci Total Environ. 2023 Mar 1;862:160835. doi: 10.1016/j.scitotenv.2022.160835. Epub 2022 Dec 9.

Abstract

The imbalance between the water supply and demand in arid and semiarid regions is becoming increasingly serious due to global warming and human activities. It is of great significance to reveal the variation characteristics of runoff and its main controlling factors for the sustainable management of regional water resources. However, few previous studies have considered the integrated effects of multiple control factors on runoff variation at different periodic scales. We collected meteorological and hydrological data from 1960 to 2019 in the Huangshui watershed and explored the correlation degree between runoff and regional environment factors such as precipitation (P), potential evaporation (ET), mean temperature (T), normalized difference vegetation index (NDVI). The wavelet coherence indicates that there was a high degree of positive phase consistency between runoff changes and P, ET, T and NDVI at an approximately 12-month period scale, with lag times of approximately 1, 2, 1 and 0 months, respectively. The P was the single factor most closely related to runoff, and its combined with ET dominated the runoff change during the whole study period. The Budyko frame combined with elastic coefficient analysis showed that the climate change were the main reasons for the increase in annual runoff in change period I (1981-1990), and changes in the underlying surface due to human activities and vegetation variation was the main reason for the decrease in runoff in change period II (1991-2019). The wetter climate brought more rainfall input but this did not make runoff appear an obvious upward trend. Therefore, for alpine regions with sensitive and fragile ecological environment, the balance between human water consumption, vegetation ecological water demand, and precipitation should be weighed. The combination of wavelet coherence analysis and Budyko framework is helpful to better determine the potential driving factors of regional runoff change.

摘要

由于全球变暖和人类活动,干旱和半干旱地区的水资源供需失衡日益严重。揭示径流变化特征及其主要控制因素对区域水资源的可持续管理具有重要意义。然而,以往很少有研究考虑多个控制因素在不同周期尺度上对径流变化的综合影响。我们收集了1960年至2019年湟水流域的气象和水文数据,探讨了径流与降水(P)、潜在蒸发散(ET)、平均气温(T)、归一化植被指数(NDVI)等区域环境因素之间的相关程度。小波相干分析表明,在大约12个月的周期尺度上,径流变化与P、ET、T和NDVI之间存在高度正相位一致性,滞后时间分别约为1、2、1和0个月。P是与径流关系最密切的单一因素,在整个研究期间,其与ET共同主导了径流变化。结合弹性系数分析的布迪科框架表明,气候变化是变化期I(1981—1990年)年径流量增加的主要原因,人类活动和植被变化引起的下垫面变化是变化期II(1991—2019年)径流量减少的主要原因。更湿润的气候带来了更多的降雨输入,但这并没有使径流出现明显的上升趋势。因此,对于生态环境敏感脆弱的高寒地区,应权衡人类用水、植被生态需水和降水之间的平衡。小波相干分析和布迪科框架的结合有助于更好地确定区域径流变化的潜在驱动因素。

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