Comment on Garg et al., . ‘Up‐scaling potential impacts on water flows from agricultural water interventions: opportunities and trade‐offs in the Osman Sagar catchment,Musi sub‐basin,India’. Hydrological Processes 27: 3905–3921          下载免费PDF全文

Jetske A. Bouma  Trent W. Biggs  Laurens M. Bouwer 《水文研究》2014,28(8):3350-3351

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Quantification of human and climate contributions to multi-dimensional hydrological alterations: A case study in the Upper Minjiang River,China     

ZHANG Yuhang  YE Aizhong  YOU Jinjun  JING Xiangyang 《地理学报(英文版)》2021,31(8):1102-1122

Dual factors of climate and human on the hydrological process are reflected not only in changes in the spatiotemporal distribution of water resource amounts but also in the various characteristics of river flow regimes. Isolating and quantifying their contributions to these hydrological alterations helps us to comprehensively understand the response mechanism and patterns of hydrological process to the two kinds of factors. Here we develop a general framework using hydrological model and 33 indicators to describe hydrological process and quantify the impact from climate and human. And we select the Upper Minjiang River(UMR) as a case to explore its feasibility. The results indicate that our approach successfully recognizes the characteristics of river flow regimes in different scenarios and quantitatively separates the climate and human contributions to multi-dimensional hydrological alterations. Among these indicators, 26 of 33 indicators decrease over the past half-century(1961–2012) in the UMR, with change rates ranging from 1.3% to 33.2%, and the human impacts are the dominant factor affecting hydrological processes, with an average relative contribution rate of 58.6%. Climate change causes an increase in most indicators, with an average relative contribution rate of 41.4%. Specifically, changes in precipitation and reservoir operation may play a considerable role in inducing these alterations. The findings in this study help us better understand the response mechanism of hydrological process under changing environment and is conducive to climate change adaptation, water resource planning and ecological construction.  相似文献   

宗教文化旅游对游客的影响研究 ——以武当山道教文化旅游为例     

程绍文  李艳  张晓梅  李照红 《地理科学》2017,37(10):1569-1576

以武当山为研究案例地,通过游客问卷与访谈调查,采用SPSS18.0统计软件定量分析武当山旅游体验对游客认知、思想、行为意愿等的影响。研究结果表明,① 武当山游客的旅游动机有宗教朝圣、文化体验、娱乐放松及感情交流4类;② 宗教文化旅游影响游客对目的地的形象感知及对道教文化的认知、态度及践行意愿;③ 宗教文化旅游对游客的影响强弱因动机而不同,自强至弱依次为宗教朝圣、文化体验、感情交流及娱乐放松。  相似文献   

安徽省人口年龄结构特征及其社会经济影响研究   总被引：1，自引：0，他引：1  

汪静 《地理科学》2017,37(11):1728-1735

根据人口普查和抽样调查的数据资料,采用对比分析、聚类分析等研究方法分析了1953~2015年安徽省人口年龄结构时间特征、空间特征。从时间上看,安徽省人口年龄结构不断演变,少儿人口数量从不断增加转变为不断减少,劳动适龄人口比重比较稳定,人口老龄化程度不断加深,总抚养系数和少年儿童抚养系数大幅度下降,老年抚养系数上升;从空间上看,人口年龄结构存在较大地区差异。安徽省人口年龄结构对社会经济发展的影响主要表现为：① 人口老年化导致劳动生产率和经济增长速度的减缓,家庭规模小型化,并对社会养老保障和医疗卫生的挑战;② 少儿人口的不断减少影响教育资源的配置;③ 人口年龄结构的区域差异进一步加剧了安徽区域发展的不平衡性。为了尽可能地减缓人口年龄结构演变对安徽省社会经济发展的不利影响,建议采取如下措施：一是充分利用“人口红利”机遇期,加快经济发展,不断促进社会进步;二是要加强引导,因地施策;三是完善社会保障制度,努力扩大社会保障制度的覆盖面,力争全覆盖,尽量减小城乡差距;四是大力发展养老产业,探索建立满足居家养老、社区养老、机构养老等多种方式需求的政府主导、政策扶持、社会参与、市场运作的社会化养老服务体系。  相似文献   

Runoff and Soil Erosion on Slope Cropland: A Review     

WANG Shanshan  SUN Baoyang  LI Chaodong  LI Zhanbin  MA Bo 《资源与生态学报(英文版)》2018,9(5):461-470

Soil erosion has become a serious environmental problem worldwide, and slope land is the main source of soil erosion. As a primary cover of slope land, crops have an important influence on the occurrence and development of runoff and soil erosion on slope land. This paper reviews the current understanding of runoff and soil erosion on slope cropland. Crops mainly impact splash detachment, slope runoff, and sediment yield. In this review paper, the effects of crop growth and rainfall on the splash detachment rate and the spatial distribution of splash detachment are summarized. Crop growth has a significant impact on runoff and sediment yield. Rainfall intensity and slope gradient can influence the level of erosive energy that causes soil erosion. Furthermore, other factors such as antecedent soil water content, soil properties, soil surface physical crust, and soil surface roughness can affect soil anti-erodibility. The varying effects of different crops and with different influence mechanisms on runoff and soil erosion, as well as changes in their ability to influence erosion under different external conditions should all remain focal points of future research. The effect of crop vegetation on runoff and soil erosion on slope land is a very important factor in understanding large-scale soil erosion systems, and in-depth study of this topic is highly significant for both theory and practice.  相似文献   

北京不同区域气溶胶辐射效应   总被引：1，自引：0，他引：1       下载免费PDF全文

李德平  程兴宏  孙治安  王黎明  张本志  张天明 《应用气象学报》2018,29(5):609-618

采用大气辐射传输模式SES2以及2013年1月—2015年10月欧洲中期天气预报中心细网格再分析资料计算了北京地区4个观测站地面接收的短波辐射通量,分析了晴天和云天北京城郊气溶胶对总辐射的定量影响时空变化特征。结果表明:北京城区和近郊区气溶胶对总辐射的影响约为远郊区的2倍,北京南部和西部气溶胶对辐射的影响较大,晴天和云天北京城区和近郊区气溶胶对总辐射的削减值分别为146.23~180.99 W·m-2和202.11~217.02 W·m-2,晴天总辐射削减空间差异较大;秋冬季气溶胶对总辐射的影响明显大于春夏季,北京市观象台秋冬季气溶胶对总辐射的削减作用最大可达60%,较春夏季高10%~20%;北京城郊总辐射和直接辐射削减率与气溶胶光学厚度变化均呈线性关系,近地面PM_2.5浓度对辐射的影响不容忽视。  相似文献   

Evolution and changes of permafrost on the Qinghai-Tibet Plateau during the Late Quaternary     

XiaoLi Chang  HuiJun Jin  RuiXia He  LanZhi L&#;  Stuart A. Harris 《寒旱区科学》2017,9(1):1-19

Due to the uplift of Qinghai-Tibet Plateau(QTP), the cryosphere gradually developed on the higher mountain summits after the Neocene, becoming widespread during the Late Quaternary. During this time, permafrost on the QTP experienced repeated expansion and degradation. Based on the remains and cross-correlation with other proxy records such as those from glacial landforms, ice-core and paleogeography, the evolution and changes of permafrost and environmental changes on the QTP during the past 150,000 years were deduced and are presented in this paper. At least four obvious cycles of the extensive and intensive development, expansion and decay of permafrost occurred during the periods of 150–130, 80–50, 30–14 and after 10.8 ka B.P.. During the Holocene, fluctuating climatic environments affected the permafrost on the QTP, and the peripheral mountains experienced six periods of discernible permafrost changes:(1) Stable development of permafrost in the early Holocene(10.8 to 8.5–7.0 ka B.P.);(2) Intensive permafrost degradation during the Holocene Megathermal Period(HMP, from 8.5–7.0 to 4.0–3.0 ka B.P.);(3) Permafrost expansion during the early Neoglacial period(ca. 4,000–3,000 to 1,000 a B.P.);(4) Relative degradation during the Medieval Warm Period(MWP, from 1,000 to 500 a B.P.);(5) Expansion of permafrost during the Little Ice Age(LIA, from 500 to 100 a B.P.);(6) Observed and predicted degradation of permafrost during the 20 th and 21 st century. Each period differed greatly in paleoclimate, paleoenvironment, and permafrost distribution, thickness, areal extent, and ground temperatures, as well as in the development of periglacial phenomena. Statistically, closer dating of the onset permafrost formation, more identification of permafrost remains with richer proxy information about paleoenvironment, and more dating information enable higher resolution for paleo-permafrost reconstruction. Based on the scenarios of persistent climate warming of 2.2～2.6 °C in the next 50 years, and in combination of the monitored trends of climate and permafrost changes, and model predictions suggest an accelerated regional degradation of plateau permafrost. Therefore, during the first half of the 21 st century, profound changes in the stability of alpine ecosystems and hydro(geo)logical environments in the source regions of the Yangtze and Yellow rivers may occur. The foundation stability of key engineering infrastructures and sustainable economic development in cold regions on the QTP may be affected.  相似文献   

中国全球气候变化影响研究方法的进展   总被引：28，自引：4，他引：24  

李克让  陈育峰 《地理研究》1999,18(2):214-219

着重介绍了中国全球气候变化影响研究中有关方法的最新进展,其中包括实验室、农田和野外观测实验;冰芯、树木年轮和历史文献方法;数值模式研究,特别是静态模式和动态模式研究。最后,指出了存在的问题,以及研究展望。  相似文献   

气候变化对湖库水环境的潜在影响研究进展   总被引：4，自引：3，他引：1  

张晨  来世玉  高学平  刘汉安 《湖泊科学》2016,28(4):691-700

本文着重归纳气候变化对湖库热力特性、冰期、溶解氧、营养盐、浮游植物和水生植物等方面的影响规律,探讨气候变化对湖库水环境潜在影响的区域差异,讨论现有研究方法的优缺点和发展前景.研究表明,气候变暖对湖库物理过程的影响最为显著;热带草原气候和温带海洋性气候对于气候变暖和降雨变化的响应较其他气候类型突出;气候变化对湖库水环境的影响效果具有两面性.通过分析各气候类型中气候变暖对磷水平的潜在影响差异表明,亚热带季风气候的湖库更可能受气候变暖的影响趋于富营养状态.在今后研究中,建议深入开展各气候类型中区域性气候变化对湖库水环境影响的实例研究.  相似文献   

Response of fish communities in rivers subjected to a high sediment load     

《Limnologica》2017

Erosion and sediment yield are a significant problem in the Guadalquivir River basin. Such phenomena are largely driven by a land use devoted to intensive cultivation of olive trees, with a large socioeconomic influence in Andalusia. This sediment overload in rivers causes serious impacts on all fluvial ecosystem components.In this study we assess the chronic effect of sediment yield on fish communities at 104 river sites located in two different sub-catchments – the Bembézar and Guadajoz rivers – both with different lithological composition and erosion rates. Sediment yield was estimated using a semi-quantitative Factorial Score Model (FSM), developed specifically for Spanish rivers. The fish populations of both basins were evaluated in composition and abundances by the study of Fernández-Delgado et al., 2014. The influence of sediment yield on the fish community was analyzed using General Additive Models.The sediment yield was higher in the Guadajoz basin (921 T/Km2 per year) than in Bembézar (701 T/Km2 per year). In the former, fish communities were poorer in both fish density and diversity, with Luciobarbus sclateri as the only substantially present species and a significant relationship between sediment yield and load, and fish density. In contrast, in the Bembézar basin, sediment yield was correlated with total fish density, including Luciobarbus sclateri, Pseudochondrostoma willkommii, Cobitis paludica, Iberochondrostoma lemmingii, Anaecypris hispanica, and Cyprinus carpio. Intermediate values of sediment yield led to maximum densities, while those higher decreased the density of these species.  相似文献