College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China.
College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi 712100, China.
Sci Total Environ. 2021 Feb 20;756:143995. doi: 10.1016/j.scitotenv.2020.143995. Epub 2020 Dec 2.
The limited runoff in cold and arid regions is sensitive to environmental changes, and it is thus urgent to explore the change and controlling factors of runoff under the background of global warming and intensified human activities. However, previous studies have rarely considered the combined effects of multiple controlling factors at varying scales over time. With the headwater region of the Manas River in northwest China as the study area, we investigated the change in runoff for the period of 1954-2016 and its relationship with regional environmental factors (e.g. precipitation PCP, temperature TMP, potential evapotranspiration ET, snow cover extent SCE, land use, and normalized difference vegetation index NDVI) and/or global atmospheric circulation (e.g. North Atlantic Oscillation NAO, Arctic Oscillation AO, Pacific Interdecadal Oscillation PDO, and El Nino Southern Oscillation ENSO). In particular, the combined effects of multiple environmental factors were determined at different scales by the multiple wavelet coherence. The annual runoff significantly increased at a rate of 0.508 × 10 m/decade, and the climate tended to be warmer and wetter. Among the regional and global environmental factors, NDVI and ENSO were the single factor mostly correlated with runoff, while NDVI-TMP and ENSO-PDO were the combined factors with the stronger relations on runoff, respectively. The regional environmental factors had larger impacts on runoff than the global environmental factors, and the natural factors outperformed human activities in controlling runoff. The accelerated melting of snow/glacier induced by the increasing temperature dominated runoff change, and the increasing water inputs from wetter climate may play a second role in runoff. The runoff characteristics in cold and arid regions seem to be different from those regions with little snow/glacier, which should be paid more attention. The employed multiple wavelet coherence is helpful in determining the processes dominating runoff change.
寒冷干旱地区的径流量有限,对环境变化较为敏感,因此迫切需要在全球变暖及人类活动加剧的背景下,探索径流量的变化及其控制因素。然而,以往的研究很少考虑不同时间尺度上多种控制因素的综合影响。以中国西北的玛纳斯河流域源头区为研究区,我们调查了 1954-2016 年期间的径流量变化及其与区域环境因素(如降水量 PCP、气温 TMP、潜在蒸散量 ET、积雪面积 SCE、土地利用和归一化植被指数 NDVI)和/或全球大气环流(如北大西洋涛动 NAO、北极涛动 AO、太平洋十年际振荡 PDO 和厄尔尼诺南方涛动 ENSO)的关系。特别是,通过多小波相干性确定了不同尺度上多种环境因素的综合影响。年径流量以 0.508×10^8m/decade 的速率显著增加,气候趋于暖湿化。在区域和全球环境因素中,NDVI 和 ENSO 是与径流量最相关的单因素,而 NDVI-TMP 和 ENSO-PDO 是与径流量关系更强的综合因素。区域环境因素对径流量的影响大于全球环境因素,自然因素在控制径流量方面优于人类活动。温度升高导致的冰雪加速融化主导了径流量变化,气候湿润带来的更多水分输入可能在径流量变化中起到次要作用。寒冷干旱地区的径流量特征似乎与冰雪较少的地区不同,这一点需要引起更多关注。所采用的多小波相干性有助于确定主导径流量变化的过程。