三峡大坝下游水位变化与河道形态调整关系研究（英文）

In this study, data measured from 1955–2016 were analysed to study the relationship between the water level and river channel geometry adjustment in the downstream of the Three Gorges Dam(TGD) after the impoundment of the dam. The results highlight the following facts:(1) for the same flow, the low water level decreased, flood water level changed little, lowest water level increased, and highest water level decreased at the hydrological stations in the downstream of the dam;(2) the distribution of erosion and deposition along the river channel changed from "erosion at channels and deposition at bankfulls" to "erosion at both channels and bankfulls;" the ratio of low-water channel erosion to bankfull channel erosion was 95.5% from October 2002 to October 2015, with variations between different impoundment stages;(3) the low water level decrease slowed down during the channel erosion in the Upper Jingjiang reach and reaches upstream but sped up in the Lower Jingjiang reach and reaches downstream; measures should be taken to prevent the decrease in the channel water level;(4) erosion was the basis for channel dimension upscaling in the middle reaches of the Yangtze River; the low water level decrease was smaller than the thalweg decline; both channel water depth and width increased under the combined effects of channel and waterway regulations; and(5) the geometry of the channels above bankfulls did not significantly change; however, the comprehensive channel resistance increased under the combined effects of riverbed coarsening, beach vegetation, and human activities; as a result, the flood water level increased markedly and moderate flood to high water level phenomena occurred, which should be considered. The Three Gorges Reservoir effectively enhances the flood defense capacity of the middle and lower reaches of the Yangtze River; however, the superposition effect of tributary floods cannot be ruled out.     

长江通过江湖水文水动力交互对其支流水域东洞庭湖的影响（英文）

The blocking or reversing effect of the downstream trunk river on its tributary lakes is an essential aspect of river-lake hydraulics.To measure how and the extent to which a trunk river can influence its tributary lakes,we made a case study in Changjiang River and one of its tributary lakes,Lake East Dongting(Lake ED)during a 35-year study period(1980–2014).Specifically,we investigated Lake ED’s discharge ability into Changjiang River using stage-discharge relationship curves,and hence the changes of the lake discharge ability under different hydrologic conditions of the Changjiang River.The results show that (1) the Changjiang River does exert a huge impact on the water regimes of Lake ED.And this impact varies seasonally.A variation of 3000in Changjiang River’s runoff would change the lake water level by about 1.1 min dry seasons,by 0.4 min wet seasons,and by 0.6 m during severe summer floods.(2)Changes in the Changjiang River runoff triggered by the Three Gorges Dam since 2003 have led to dramatic water regime variations in Lake ED.Other factors,including reduction of lake inflow and the lake bed erosion,also exacerbated the water regime variations in Lake ED.     

基于能量的鄱阳湖——长江相互作用表征指标研究（英文）

The complex relationship between the Yangtze River and Poyang Lake controls the exchange of water and sediment between the two,and exerts effects on water resources,flooding,shipping,and the ecological environment.The theory of energy is applied in this paper to investigate the physical mechanisms that determine the nature of the contact between the Yangtze River and Poyang Lake and to establish an energy differenceindex to quantify the interactions between the two systems.Data show that Fe values for this interaction have increased since the 1950s,indicating a weakening in the river effect while the lake effect has been enhanced.Enclosure of the Three Gorges Reservoir(TGR)has also significantly influenced the relationship between the river and the lake by further reducing the impacts of the Yangtze River.The river effect also increases slightly during the dry season,and decreases significantly at the end of the flooding period,while interactions between the two to some extent influence the development of droughts and floods within the lake area.Data show that when the flow of the five rivers within this area is significant and a blocking effect due to the Yangtze River is also clearly apparent,floods occur easily;in contrast,when the opposite is true and the flow of the five rivers is small,and the Yangtze River can accommodate the flow,droughts occur frequently.Construction and enclosure of the TGR also means that the lake area is prone to droughts during September and October.     

东亚地缘政治格局演变对东北亚资源合作的影响研究（英文）

以美国实施亚太再平衡战略和中国推进丝绸之路经济带建设为背景,本研究总结了地缘政治、地缘经济、地缘战略的基本概念和相互之间的关系,并回顾了基本的地缘政治理论及其研究进展。继而在概括东亚地缘政治环境变化特点的基础上,论文总结了中蒙之间、中俄之间地缘政治关系发展趋势,认为美国亚太再平衡战略打破了亚太地缘力量平衡格局,中国利益受到来自日本、越南、菲律宾等国的强力挑战。随后,论文以东北亚能源市场为例探讨了地缘环境变化对区域资源市场的影响。其中,对中国而言,建设丝绸之路经济带是应对地缘环境危机的策略;与此同时,俄罗斯在受到西方制裁后将眼光投向亚洲,加之中俄之间具有很强的经济互补性,双方的资源合作水平有望进一步提高;蒙古国经济上对中国依赖很大,美国重返亚洲之后,蒙古国调整了自己的地缘战略,企图借美国力量制衡中俄在蒙古国的影响力,虽然中蒙之间的地缘政治关系总体上是向好发展,但美国的介入增加了中蒙资源合作的不确定性;因日韩为美国盟友,中俄与美国的地缘利益冲突将减少其在东北亚资源市场上的份额;对朝鲜来说,因其经济总量很小,对区域资源市场影响不大。     

成渝经济圈生态效率时空动态演变及其影响因素（英文）

为了响应国家十四五规划,更好地探索促进区域协调绿色发展的新战略,本文采用super-SBM模型和马尔可夫链对成渝经济圈2004–2018年的生态效率值进行了测算与时序分析,同时,利用地理加权回归模型对生态效率进行了空间分析。虽然成渝经济圈生态效率在研究期间有所提高,但其经济发展仍然是生态无效的,这意味着成渝迫切需要提高资源利用效率,促进技术创新。在研究期间,成渝经济圈的生态效率的演变呈现为“π”字形状,并伴随着“俱乐部趋同”的现象,此现象表明生态效率有保持原状的强烈趋势,说明生态效率缺乏足够的改善动力,因此很难实现跨越式转移。从空间上看,生态效率从西北向东南呈高–低–高效率分布,生态效率的时空差异缩小,但集聚效应相对较弱且呈现两极分化趋势。进一步的研究表明,城镇化发展水平、对外开放水平、技术水平、环境规制和产业结构高级化是导致生态效率空间差异的原因。成渝经济圈应针对各自弱点相应采取改善措施提高生态效率,从而促进整个区域的绿色发展。     

中国生态旅游政策演变定量研究（英文）

生态旅游发展的复杂性要求人们了解影响其发展效果的各类因素,因此,公共部门逐渐关注相关政策的制定以推动生态旅游发展并进行效果评估。本文的目的在于通过对各阶段中国生态旅游政策的梳理探究中国生态旅游政策的演进特征以及政策演进与生态旅游发展的关系。本文对1994–2016年中央政府及相关部委生的91个生态旅游政策样本统计数据入手,对样本政策的数量与内容结构、政策力度、政策工具以及政策制定部门进行统计分析。结果显示:(1)政策演化中国体现生态旅游发展的目标、内容和方式的转变;(2)政策主题主要围绕生态保护,演进方式为渐进调适;(3)政策工具由微观规制向宏观调控过渡,但未能形成较为完整的政策体系;(4)政策制定部门范畴不断扩大,政策力度值稳步提升。在生态文明建设和《旅游法》实施双重背景下,宏观调控、微观自主是未来生态旅游政策的发展方向,认证标准体系建设是生态旅游政策完善的重点,多部门参与协同是生态旅游政策制定和执行的有力保障,生态旅游发展中的业态融合、利益相关者福利与行为规制、生态旅游发展模式及配套等将是未来中国生态旅游政策关注的重点。     

京津冀干旱时空演变规律分析（英文）

Spatio-temporal patterns of drought from 1961 to 2013 over the Beijing-Tianjin-Hebei(BTH) region of China were analyzed using the Palmer Drought Severity index(PDSI) based on 21 meteorological stations. Overall, changes in the mean-state of drought detected in recent decades were due to decreases in precipitation and potential evapotranspiration. The Empirical Orthogonal Functions(EOF) method was used to decompose drought into spatio-temporal patterns, and the first two EOF modes were analyzed. According to the first leading EOF mode(48.5%), the temporal variability(Principal Components, PC1) was highly positively correlated with annual series of PDSI(r=+0.99). The variance decomposition method was further applied to explain the inter-decadal temporal and spatial variations of drought relative to the total variation. We find that 90% of total variance was explained by time variance, and both total and time variance dramatically decreased from 1982 to 2013. The total variance was consistent with extreme climate events at the inter-decadal scale(r=0.71, p0.01). Comparing the influence of climate change on the annual drought in two different long-term periods characterized by dramatic global warming(P1: 1961–1989 and P2: 1990–2013), we find that temperature sensitivity in the P2 was three times more than that in the P1.     

西藏旱灾变化趋势及其风险演变（英文）

The risk posed by natural disasters can be largely reflected by hazard and vulnerability. The analysis of long-term hazard series can reveal the mechanisms by which risk changes. Drought disasters are one of the main types of disaster in the Tibet Region(TR) of China. In this study, using statistical drought disasters data in the TR from 1912 to 2012 and socio-economic statistics for five periods between 1965 and 2015, and adopting standard statistical analyses, a wavelet analysis, and a risk assessment model, we first construct the index system for drought disaster risk assessment, and then assess the risk of drought disasters and analyze the mechanisms of changes in risk. The results showed that the occurrence of drought in the TR had three distinct cycles during this study periods, with durations of 5, 15, and 27 years respectively. The frequency of drought in the TR showed increasing trends, and the cycle of drought had been prolonged. From 1965 to 2015, the risk of drought disaster in the TR is significantly increased with the growth rate of 6.8% in high-risk area. In addition, the severity of drought had enhanced, especially in Qamdo. The increased vulnerability locally and significantly enhanced hazard of drought disaster, with a shrinkage of 16.3% in the low-value area and an expansion of 7.4% in the high-value area, being the determinants of drought disaster risk. Therefore, agricultural areas of the TR are the focal locations where risk of drought disaster needs to be managed.     

气候变化对里海水位的影响（英文）

目前,关于里海的两个主要问题是水位变化及其生态条件。历史上,里海的海水入侵和衰退对该区域的生活和生产有很大影响。应用地质数据、历史数据和考古数据,以及观测数据,本文对地质历史时期里海水位的变化、年度和季度变化以及短期的波动进行了研究。文章对解释里海水位波动的两种不同的方法进行了论述,并认为里海水位变化是受地质、水文气候和水量平衡以及人类活动等因素的影响的多级过程,其中主要影响因素为水文气候的变化。     

长江三峡水坝下游河道悬沙恢复和床沙补给机制研究（英文）

River basin reservoir construction affects water and sediment transport processes in downstream reaches. The downstream impact of the Three Gorges Projects(TGP) has started to become apparent:(1) reduction in flood duration and discharge, and significant reduction in sediment load. Although there was some restoration in downstream sediment load, the total amount did not exceed the pre-impoundment annual average;(2) in 2003–2014, the d 0.125 mm(coarse sand) load was restored to some degree, and to a maximum at Jianli Station, which was mainly at the pre-impoundment average. After restoration, erosion and deposition characteristics of the sediment was identical to that before impoundment. The degree of restoration during 2008–2014 was less than during 2003–2007;(3) after TGP impoundment, there was some restoration in d 0.125 mm(fine sand) sediment load, however, it was lower than the pre-impoundment average;(4) due to riverbed compensation, the d 0.125 mm sediment load recovered to a certain degree after impoundment, however, the total did not exceed 4400×10~4 t/y. This was mainly limited by flood duration and the average flow rate, and was less affected by upstream main stream, tributaries, or lakes. Restoration of d 0.125 mm suspended sediment was largely controlled by upstream main stream, tributaries, and lakes, as well as by riverbed compensation. Due to bed armoring, riverbed fine suspended sediment compensation capability was weakened;(5) during 2003–2007 and 2008–2014, Yichang to Zhicheng and upper Jingjiang experienced coarse and fine erosion,lower Jingjiang experienced coarse deposition and fine erosion, Hankou to Datong had coarse deposition and fine erosion, and Chenglingji and Hankou was characterized by coarse deposition and fine sand erosion in 2003–2007, and coarse and fine erosion in 2008–2014. This difference was controlled by flood duration and number at Luoshan Station.     

北京城市副中心（通州区）土地利用演变格局与模拟（英文）

北京城市副中心（通州区）承接着北京中心城区的非首都核心功能,其快速建设发展亟需对区域内土地利用演变格局的科学认识。本文分析了改革开放40年来通州区土地利用演变格局,根据土地利用历史演变特征与城市发展规划目标,结合文旅发展驱动要素,运用FLUS模型模拟城镇化加速、减速和可持续发展3种情景下2035年北京城市副中心（通州区）土地利用空间分布格局。结果表明：（1）北京城市副中心（通州区）以城镇发展建设为主,1980—2010年高速城镇化阶段形成“沿六环顺运河”的城市扩张格局,2010—2020年低速城镇化阶段用地分布稳定,通州区形成从西北至东南城乡分异、土地集约化发展格局,副中心作为通州区城镇化的典型区域具有与通州整体相似的时空演变特征;（2）到2035年,3种情景间土地利用变化幅度和空间分布存在显著差异,城镇可持续发展情景下生态用地面积与分布最优,有利于实现城市可持续发展。在与三大副中心分区规划的契合程度分析中,可持续发展情景下预测模拟与市政府发布的《北京城市副中心控制性详细规划（街区层面）（2016—2035年）》（简称《规划》）用地高度契合,但文化旅游功能区和宜居生活风貌区中模拟预测与...     

河北省县域城乡发展时空演变及影响因素分析（英文）

城乡融合发展是实现乡村振兴和农业农村现代化的重要手段之一,充分了解不同地区的城乡融合发展水平对制定城乡融合发展战略至关重要。以河北省118个县域为研究对象,构建河北省县域城乡融合水平测度指标体系,运用熵值法、核密度分析、ESDA空间探索性数据分析方法和地理探测器审视并分析了2005-2020年河北省县域城乡融合水平、时空演变特征及其影响因素。结果表明：（1）河北省县域城乡融合发展推进有序且态势良好,2005-2020年16年间城乡融合指数呈波动上升趋势。其中,2005-2010年为波动发展阶段,2011-2020年为城乡融合水平快速发展阶段。（2）河北省县域城乡融合水平呈现一定的高低值锁定现象,发展较快的地区恒快,较慢的地区恒慢。（3）河北省城乡融合水平影响因素逐渐趋向多元化演变,主导因素从相对单一逐渐转变为相对多元化。     

水汽对气候变化海拔依赖性的影响（英文）

气候变化的海拔依赖性在世界上大多数山脉地区已有报道,但导致这种变异的原因尚不明确。本研究利用中国四个不同的观测和再分析资料数据集,主要研究气候变暖对海拔的依赖性,结果表明:无论是在青藏高原地区还是中国其他地区,气候变暖的程度与海拔高度的一致性并不明显。但是,气候变暖与不同海拔水汽的变异具有很好的相关性。比湿度较低时,气温变化随比湿度的增加而升高;当比湿度上升到一定值,气温变化则随比湿度的增加而下降。而地表温度变化的最大值出现在比湿度2.0–3.0 g kg~(-1)范围内。因此,本研究揭示了水汽对气候变暖的海拔依赖性起到调节作用。     

山体效应对生态垂直格局的影响（英文）

The varied altitudinal gradient of climate and vegetation is further complicated by mass elevation effect(MEE), especially in high and extensive mountain regions. However, this effect and its implications for mountain altitudinal belts have not been well studied until recently. This paper provides an overview of the research carried out in the past 5 years. MEE is virtually the heating effect of mountain massifs and can be defined as the temperature difference on a given elevation between inside and outside of a mountain mass. It can be digitally modelled with three factors of intra-mountain base elevation(MBE), latitude and hygrometric continentality; MBE usually acts as the primary factor for the magnitude of MEE and, to a great extent, could represent MEE. MEE leads to higher treelines in the interior than in the outside of mountain masses. It makes montane forests to grow at 4800–4900 m and snowlines to develop at about 6000 m in the southern Tibetan Plateau and the central Andes, and large areas of forests to live above 3500 m in a lot of high mountains of the world. The altitudinal distribution of global treelines can be modelled with high precision when taking into account MEE and the result shows that MEE contributes the most to treeline distribution pattern. Without MEE, forests could only develop upmost to about 3500 m above sea level and the world ecological pattern would be much simpler. The quantification of MEE should be further improved with higher resolution data and its global implications are to be further revealed.     

尼泊尔生态服务消费模式演变研究（英文）

本研究基于FAOSTAT数据库中尼泊尔林业数据和食物消费数据,采用实物量核算方法,依据生物产品生产性土地类型归类,研究了尼泊尔农田、森林、草地、水域及综合生态系统的消费水平、结构及生态服务消费模式的动态变化,揭示了尼泊尔生态服务消费模式演变的主要因素。研究结果表明,1961–2018年尼泊尔农田、森林、草地、水域及综合生态系统服务消费总量平均分别为7.26 Tg yr^-1、6.38 Tg yr^-1、1.10 Tg yr^-1、0.02 Tg yr^-1和14.76 Tg yr^-1,均呈现波动增长态势;除年人均森林消费量波动降低外,其余生态系统和综合生态系统年人均消费量均波动增加,且增速持续增大。1961–2018年尼泊尔生态服务消费可分为1961–1984、1985–2007和2008–2018年三个时期,生态服务消费模式依次为“木–谷–奶”模式、“木–谷–蔬–根-奶-糖”模式和“木–谷–蔬–根–糖–果–奶”模式。驱动因素分析表明,生态系统供给能力(生产能力、进口能力和出口能力)和...     

新疆小河墓地附近全新世环境演变及其对人类活动的影响（英文）

The Xiaohe Cemetery archaeological site(Cal.4–3.5 ka BP)is one of the most important Bronze Age sites in Xinjiang,China.Although the surrounding environment is an extremely arid desert now,abundant archaeological remains indicate that human occupation was common during certain periods in the Holocene.Field investigations and laboratory analyses of a sediment profile near the Xiaohe Cemetery indicate that while the regional environment was arid desert throughout the Holocene there were three episodes of lake formation near the site in the periods 4.8–3.5 ka BP,2.6–2.1 ka BP and 1.2–0.9 ka BP.Geomorphic and hydrological investigations reveal that a lake or lakes formed in a low-lying area when water was derived initially from the Kongque River and then shunted into the Xiaohe River basin.Low amounts of active chemical elements in lacustrine sediment between 4.8–3.5 ka BP indicate abundant and continuous water volume in the lake;the content of active chemical elements increased between 2.6–2.1 ka BP but was still at a relatively low level,suggesting a declining amount of water and diminished inflow.Between 1.2–0.9 ka BP there was a very high content of active elements,suggesting decreased water volume and indicating that the lake was stagnate.In contrast,the general climate condition shows that there had a warm-humid stage at 8–6 ka BP,a cool-humid stage at 6–2.9 ka BP and a warm-dry stage at2.9–0.9 ka BP in this region.The hydrological evolutions around Xiaohe Cemetery did not have one-to-one correspondence with climate changes.Regional comparison indicates that broad-scale climatic conditions played an important role through its influences on the water volume of the Tarim River and Kongque River.But,the formation of the lakes and their level were controlled by geomorphic conditions that influenced how much water volume could be shunted to Xiaohe River from Kongque River.Human occupation of the Xiaohe Cemetery and nearby regions during the Bronze Age and Han-Jin period(202 BC–420 AD)corresponded to the two earlier lake periods,while no human activities existed in the third lake period because of the decreased water volume.     

长江中下游阻隔性河段作用机理初步研究（英文）

Alluvial channel has always adjusted itself to the equilibrium state of sediment transport after it was artificially or naturally disturbed.How to maintain the equilibrium state of sediment transport and keep the river regime stable has always been the concerns of fluvial geomorphologists.The channel in the middle and lower reaches of the Yangtze River is characterized by the staggered distribution of the bifurcated river and the single-thread river.The change of river regime is more violently in the bifurcated river than in the single-thread river.Whether the adjustment of the river regime in the bifurcated river can pass through the single-thread river and propagate to the downstream reaches affects the stabilities of the overall river regime.Studies show that the barrier river reach can block the upstream channel adjustment from propagating to the downstream reaches;therefore,it plays a key role in stabilizing the river regime.This study investigates 34 single-thread river reaches in the middle and lower reaches of the Yangtze River.On the basis of the systematic summarization of the fluvial process of the middle and lower reaches of the Yangtze River,the control factors of barrier river reach are summarized and extracted:the planar morphology of single-thread and meandering;with no flow deflecting node distributed in the upper or middle part of the river reach;the hydraulic geometric coefficient is less than 4;the longitudinal gradient is greater than 12‰,the clay content of the concave bank is greater than 9.5%,and the median diameter of the bed sediment is greater than 0.158 mm.From the Navier-Stokes equation,the calculation formula of the bending radius of flow dynamic axis is deduced,and then the roles of these control factors on restricting the migration of the flow dynamic axis and the formation of the barrier river reach are analyzed.The barrier river reach is considered as such when the ratio of the migration force of the flow dynamic axis to the constraint force of the channel boundary is less than 1 under different flow levels.The mechanism of the barrier river reach is such that even when the upstream river regime adjusts,the channel boundary of this reach can always constrain the migration amplitude of the flow dynamic axis and centralize the planar position of the main stream line under different upstream river regime conditions,providing a relatively stable incoming flow conditions for the downstream reaches,thereby blocking the upstream river regime adjustment from propagating to the downstream reaches.     

长江河口的演变规律与水动力作用

本文应用流体运动的最小阻力原理导出了长江河口崇明岛发育长度的理论公式。论述了科里奥利力在河道分流中的作用与河口演变的混沌现象。文中指出,在未来当崇明岛归并北岸时南支可能发生的环境问题．     

水库修建后黄河下游的河床演变（英文）

Evolution of the river channel downstream of reservoirs is a complex process that is closely related to the operational mode of the reservoirs and the channel boundary conditions. Numerous studies have been carried out on the fluvial processes of downstream reservoirs. However, only a few of them have focused on the relationship between runoff-sediment conditions and channel pattern indicators. Also, the impacts of river training works on fluvial processes are seldom dealt with. In this paper, the evolutionary processes of three sections in the Lower Yellow River, including Tiexie-Yiluo River mouth reach, Huayuankou-Heigangkou reach and Jiahetan-Gaocun reach, were analyzed for variations in the channel boundary line and the mainstream between 1960 and 2015. Channel pattern indicators such as sinuosity, mainstream wandering range and width/depth ratio were analyzed based on field measurements obtained by the Hydrological Department of the Yellow River Conservancy Commission. The effects of river training works on the channel evolution are then described. Since 1960, numerous medium- and large-sized reservoirs have been built on the Yellow River, including Longyangxia Reservoir, Liujiaxia Reservoir and Xiaolangdi Reservoir. These reservoirs impound the runoff from upstream and retain the sediment, which changes the runoff and sediment conditions in the downstream reach. As a consequence, annual runoff and the frequency and peak of flooding have all decreased. As a result, the flow dynamics and their action on the river channel are also reduced, which changes the dynamic state of the river course. The discrimination results obtained using the single parameter discrimination rule and the discrimination equation show that the degree of wandering is weakened in the reaches studied. The variations in the channel pattern indicators show that the sinuosity increases and the wandering range decreases with a reduction in the total annual volume of water. However, the degree of wandering has little relationship to the sediment concentration. In addition, river training works play an important role in controlling the river course. Due to improvements in the river training works, the river course has become more stable under the same runoff and sediment conditions. A new discrimination rule that takes into account the impacts of the river training works is proposed. The discrimination results were found to fit well with the actual river pattern, which shows that the discrimination rule is applicable to the Lower Yellow River. The results show that the runoff and sediment conditions are the most important factors in the evolution of the river course. The river training works have at the same time limited the wandering range of the mainstream and played an important role in the fluvial processes. Both factors combined lead to the stabilization of the river.