DOCSLIB.ORG

TECHNICAL PROGRAMME August 12, 2006 10:43 RPS/Trim Size: 8.27In X 11.69In for Programme Booklet Hic06program

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
TECHNICAL PROGRAMME August 12, 2006 10:43 RPS/Trim Size: 8.27In X 11.69In for Programme Booklet Hic06program August 12, 2006 10:43 RPS/Trim Size: 8.27in x 11.69in for Programme Booklet hic06program HIC 2006 TECHNICAL PROGRAMME August 12, 2006 10:43 RPS/Trim Size: 8.27in x 11.69in for Programme Booklet hic06program Monday, 4 September 2006 OPENING CEREMONY Date: Monday, 04 Sept 2006 Time: 09:00 – 10:20 hrs Room: Athena Session 1A1 – Physical Simulation Modelling Date: Monday, 04 Sept 2006 Time: 10:40 – 12:40 hrs Room: Calliope Chair: A. Barnett 1A1-1 Inverse Modelling for Flood Propagation R. K. Price, W. A. Y. S. Fernando and D. P. Solomatine 1A1-2 Two Dimensional Flood Simulation using the Cartesian Cut-Cell Method A. G. Morris, D. M. Ingram and C. G. Mingham 1A1-3 Modelling Flow Transitions at Street Junctions with 1D and 2D Models Z. Vojinovic, J. Bonillo, C. Kaushik and R. Price 1A1-4 Large-Scale Urban Floods Modelling and Two-Dimensional Shallow Water Models with Porosity J. Lhomme, S. Soares-Fraz˜ao, V. Guinot and Y. Zech 1A1-5 A Large Eddy Simulation Based 3-D Numerical Model to Predict Density Driven Currents and Associated Instabilities in an Infinite Channel S. K. Ooi, G. Constantinescu and L. Weber 3 August 12, 2006 10:43 RPS/Trim Size: 8.27in x 11.69in for Programme Booklet hic06program 4 Technical Programme Session 1B1 – Study Cases Date: Monday, 04 Sept 2006 Time: 10:40 – 12:40 hrs Room: Uranie Chair: J. Ball 1B1-1 Three-Dimensional Numerical Modelling of Flow Conditions in a River Bend during a 100-Year Flood using Polyhedral Finite Volumes M. Tritthart 1B1-2 Numerical Simulation of Unsteady Flood Flows with Unknown Boundary Conditions S. Onda, T. Hosoda, T. Uchida and N. Jacimovic 1B1-3 Flood-Peak Estimation in Ghezel-Owzan River using the Hayami’s Model A. Norouzi and A. R. Ghavasieh 1B1-4 LES Investigation of Horseshoe Vortex System at the Base of a Bridge Abutment at Equilibrium Bed Scour Conditions M. Koken and G. Constantinescu 1B1-5 Estimating Water Depths using Artificial Neural Networks P. A. Conrads and E. A. Roehl 1B1-6 Using Artificial Neural Network Models to Integrate Hydrologic and Ecological Studies of the Snail Kite Falcon in the Everglades, USA P. A. Conrads, E. A. Roehl, R. Daamen and W. M. Kitchens Session 1C1 – Web-based Modelling Systems and Applications Date: Monday, 04 Sept 2006 Time: 10:40 – 12:40 hrs Room: Erato Chair: R. Falconer 1C1-1 Data Exchange between Hydro Engineering Web Services G. Hildebrandt and P. Holz 1C1-2 Web Services for Distributed A Hydro-Information System J. Horak, A. Orlik, J. Stromsky and V. Marsik August 12, 2006 10:43 RPS/Trim Size: 8.27in x 11.69in for Programme Booklet hic06program Technical Programme 5 1C1-3 The Fifth Generation of Modelling in Hydroinformatics M. B. Abbott, E. Tumwesigye and Z. Vojinovic 1C1-4 Mass Customised Advice-Serving Systems in Hydroinformatics M. B. Abbott, K. N. Thein and Y. Huang 1C1-5 Technical Information System and Modeling of Irrigation Networks at the Soci´et´edu Canal de Provence G. Cardo¨en and D. Roland 1C1-6 Developing WebGIS-Based System for Rainfall-Runoff Forecast and Real-Time Water Resources Assessment in Beijing Metropolis Y. W. Jia, H. L. Zhao, C. W. Niu, J. Liang, H. Gan, Y. Z. Jiang, C. M. Han, J. Li, X. L. Zhao, Y. Xue, Z. X. Zhao, L. G. Du, Q. T. Yang, D. Zhou and Y. J. Wang Session 1D1 – Verification, Validation and Confirmation of Numerical Models Date: Monday, 04 Sept 2006 Time: 10:40 – 12:40 hrs Room: Thalie Chair: V. Guinot 1D1-1 Geometry Measurement Versus Roughness Calibration: Application to Amazon River G. Belaud, J. P. Baume, B. Le Guennec and J. M. Martinez 1D1-2 Technology of Identification of Two-Dimensional Functions Describing the Morphometry and Hydraulics of River Channel in One-Dimensional Model of Unsteady Flow A . V. R o m a n o v a n d V. V. Ilin ich 1D1-3 Calibrating a Large Scale Fractured Aquifer Model for Extreme Events Prediction using a Dual-Permeability Approach G. Lods, P. Gouze, A. Cartalade and R. Gu´erin 1D1-4 Open Sources Model Codes: Critical Review on the Routing Modules of the Soil and Water Assessment Tool (SWAT) A. Van Griensven, K. Holvoet and J. Yang August 12, 2006 10:43 RPS/Trim Size: 8.27in x 11.69in for Programme Booklet hic06program 6 Technical Programme 1D1-5 On the Estimation of Soil Moisture Parameters in Physically Based Hydrological Models M. Ostrowski and A. Klawitter 1D1-6 Exploring Parameter Identifiability and Temporal Parameter Changes in Complex Hydrological Models G. Wriedt and M. Rode Session 1E1 – Advanced Application of Modelling Date: Monday, 04 Sept 2006 Time: 10:40 – 12:40 hrs Room: Clio Chair: A. Mynett 1E1-1 Ensemble Weather Forecasts and Operational Management of Regional Water Systems S. J. Van Andel and A. H. Lobbrecht 1E1-2 Non-Linear, Multivariate Forecasting of Hydrologic and Anthropogenic Responses to Meterological Forcing E. A. Roehl Jr. and T. Murray 1E1-3 Snowmelt Flood Frequency Estimation using Physically Based Model Coupled with Weather Generator (with Estimation’s Uncertainty) A. N. Gelfan 1E1-4 An Experiment of Rainfall Prediction over the Odra-Catchment by Combining Weather Radar and a Numerical Weather Model I. D. Cluckie, M. A. Rico-Ramirez, Y. Xuan and W. Szalinska 1E1-5 Stochastic Real-Time Forecasting with Radar Image Extrapolation and a Distributed Hydrologic Model S. M. Kim, Y. Tachikawa and K. Takara 1E1-6 Estimating and Reducing Forecast Uncertainty in Real-Time Flood Forecasting M. B. Butts, A. K. V. Falk, H. Madsen and J. Hartnack August 12, 2006 10:43 RPS/Trim Size: 8.27in x 11.69in for Programme Booklet hic06program Technical Programme 7 Session 1A2 – International Graduate Programmes Experiences Date: Monday, 04 Sept 2006 Time: 14:00 – 15:40 hrs Room: Calliope Chair: P. Goodwin 1A2-1 EuroAquae: A New Paradigm for Hydroinformatics Joint Master of Science P. Gourbesville, K. P. Holz, J. Jozsa, M. Gomez and V. Kutija 1A2-2 Erasmus Mundus Framework: Perspective of Euro-Aquae Students J. M. Crozet, Md. Atiquzzaman, K. Yamagata, B. Angamuthu, O. K. Mahabadi, A. Bozhko, G. Corestein, A. Kerroux, R. Herman, M. Terminet, L. Pouget, N. Ratnikova, L. Laureau, G. Tamagnan, D. Quatrelivre and R. Concha 1A2-3 HydroEurope Intensive Programme: Collaborative Engineering and Hydroinformatics P. Gourbesville 1A2-4 Hydro-Europe: Experience of Euro Aquae Students J. M. Crozet, Md. Atiquzzaman, K. Yamagata, B. Angamuthu, O. K. Mahabadi, A. Bozhko, G. Corestein, A. Kerroux, R. Herman, M. Terminet, N. Ratnikova, L. Pouget, L. Laureau, G. Tamagnan, D. Quatrelivre and R. Concha 1A2-5 Hands on Teaching for Real-Time Control of Open-Channels X. Litrico, P. O. Malaterre, G. Harran and J. F. Alquier Session 1B2 – Physical Simulation Modelling Date: Monday, 04 Sept 2006 Time: 14:00 – 15:40 hrs Room: Uranie Chair: M. Abbott 1B2-1 Adaptation of an Upwind Conservative Finite-Volume Scheme to Depth Averaged Turbidity Current Equations J. Gonzalez, A. Tamburrino and Y. Ni˜no 1B2-2 An Adaptation of Preissmann’s Scheme for Transcritical Flows C. Sart, J. P. Baume, P. O. Malaterre and V. Guinot August 12, 2006 10:43 RPS/Trim Size: 8.27in x 11.69in for Programme Booklet hic06program 8 Technical Programme 1B2-3 An Approximate-State Riemann Solver for the Shallow Water Equations J. Lhomme and V. Guinot 1B2-4 Semi-Implicit Modelling of Rapidly Varied Flows with Transitions A. Balzano and E. Torricelli 1B2-5 A Low Diffusion Two-Dimensional Extension of the Discontinuous Profile Method (DPM) for Advection Simulations F. Badrot-Nico, V. Guinot and F. Brissaud Session 1C2 – Geographic Information System and Virtual Imaging Date: Monday, 04 Sept 2006 Time: 14:00 – 15:40 hrs Room: Erato Chair: A. Tskhay 1C2-1 Remote Sensing for Water Quality Monitoring of Lakes Case Study: Lake Manzala N. Donia and M. Ahmed 1C2-2 GIS-Based Nutrient Transport Model for Watershed-Scale Water Quality Problems T. Kato and T. Satoshi 1C2-3 Application of a GIS-Based Nutrient Loading and Water Balance Tool to Support Assimilative Capacity Studies in the Lake Simcoe and Nottawasaga River Basins, Ontario, Canada T. Boston, B. Evans, M. Walters and M. Richardson 1C2-4 An Integration of GIS and 1D River Model in Floodplain Mapping T. Thaveevouthti and V. Kutija 1C2-5 Development of HyGIS Extension Module for SWAT K. T. Kim and Y. S. Choi August 12, 2006 10:43 RPS/Trim Size: 8.27in x 11.69in for Programme Booklet hic06program Technical Programme 9 Session 1D2 – Verification, Validation and Confirmation of Numerical Models Date: Monday, 04 Sept 2006 Time: 14:00 – 15:40 hrs Room: Thalie Chair: R. Funke 1D2-1 Validation of a Fully 3D Large Eddy Simulation Model to Predict Removal of a Neutrally Buoyant or a Dense Miscible Contaminant from a Bottom River Cavity by a Fully Turbulent Overflow K. Chang, G. Constantinescu and S. Park 1D2-2 A Two Dimensional Hydrodynamic Model for the Study of Instream Flows in Rivers C. Alvarez,´ J. A. Juanes, J. A. Revilla and A. Garcia 1D2-3 The Numerical Investigation of Two Algorithms of Surface-Tracking Method for Free Surface Calculation J. Zeng, G. Constantinescu and L. Weber 1D2-4 Dike-Break Induced Flood Wave Propagation S. Roger, E. B¨usse and J. K¨ongeter 1D2-5 Three-Dimensional Modeling of Density Current in Straight Channel E. Aram and B. Firoozabadi Session 1E2 – Advanced Application of Modelling Date: Monday, 04 Sept 2006 Time: 14:00 – 15:40 hrs Room: Clio Chair: S. Maskey 1E2-1 Individual Based Modelling in Ecosystem Dynamics A.
Load more

Recommended publications
  • Bibliography [PDF]
    Bibliography, Ancient TL, Vol. 35, No. 2, 2017 Bibliography _____________________________________________________________________________________________________ Compiled by Sebastien Huot From 15th May 2017 to 1st December 2017 Various geological applications - aeolian Arbogast, A.F., Luehmann, M.D., William Monaghan, G., Lovis, W.A., Wang, H., 2017. Paleoenvironmental and geomorphic significance of bluff-top dunes along the Au Sable River in Northeastern Lower Michigan, USA. Geomorphology 297, 112-121, http://dx.doi.org/10.1016/j.geomorph.2017.09.017. Guedes, C.C.F., Giannini, P.C.F., Sawakuchi, A.O., DeWitt, R., Paulino de Aguiar, V.Â., 2017. Weakening of northeast trade winds during the Heinrich stadial 1 event recorded by dune field stabilization in tropical Brazil. Quaternary Research 88, 369-381, http://dx.doi.org/10.1017/qua.2017.79. Ho, L.-D., Lüthgens, C., Wong, Y.-C., Yen, J.-Y., Chyi, S.-J., 2017. Late Holocene cliff-top dune evolution in the Hengchun Peninsula of Taiwan: Implications for palaeoenvironmental reconstruction. Journal of Asian Earth Sciences 148, 13-30, http://dx.doi.org/10.1016/j.jseaes.2017.08.024. Hu, G., Yu, L., Dong, Z., Lu, J., Li, J., Wang, Y., Lai, Z., 2018. Holocene aeolian activity in the Zoige Basin, northeastern Tibetan Plateau, China. Catena 160, 321-328, http://dx.doi.org/10.1016/j.catena.2017.10.005. Huntley, D.H., Hickin, A.S., Lian, O.B., 2016. The pattern and style of deglaciation at the Late Wisconsinan Laurentide and Cordilleran ice sheet limits in northeastern British Columbia. Canadian Journal of Earth Sciences 54, 52-75, http://dx.doi.org/10.1139/cjes-2016-0066.
    [Show full text]
  • Dams on the Mekong
    Dams on the Mekong A literature review of the politics of water governance influencing the Mekong River Karl-Inge Olufsen Spring 2020 Master thesis in Human geography at the Department of Sociology and Human Geography, Faculty of Social Sciences UNIVERSITY OF OSLO Words: 28,896 08.07.2020 II Dams on the Mekong A literature review of the politics of water governance influencing the Mekong River III © Karl-Inge Olufsen 2020 Dams on the Mekong: A literature review of the politics of water governance influencing the Mekong River Karl-Inge Olufsen http://www.duo.uio.no/ IV Summary This thesis offers a literature review on the evolving human-nature relationship and effect of power struggles through political initiatives in the context of Chinese water governance domestically and on the Mekong River. The literature review covers theoretical debates on scale and socionature, combining them into one framework to understand the construction of the Chinese waterscape and how it influences international governance of the Mekong River. Purposive criterion sampling and complimentary triangulation helped me do rigorous research despite relying on secondary sources. Historical literature review and integrative literature review helped to build an analytical narrative where socionature and scale explained Chinese water governance domestically and on the Mekong River. Through combining the scale and socionature frameworks I was able to build a picture of the hybridization process creating the Chinese waterscape. Through the historical review, I showed how water has played an important part for creating political legitimacy and influencing, and being influenced, by state-led scalar projects. Because of this importance, throughout history the Chinese state has favored large state-led scalar projects for the governance of water.
    [Show full text]
  • 9781107069879 Index.Pdf
    Cambridge University Press 978-1-107-06987-9 — The Qing Empire and the Opium War Mao Haijian , Translated by Joseph Lawson , Peter Lavelle , Craig Smith , Introduction by Julia Lovell Index More Information Index 18th Regiment , 286 , 306 35 – 37 , 45 , 119 – 21 , 122 , 209 ; coastal , 34 , 26th Regiment , 205 , 242 , 286 35 – 36 , 38 , 115 ; concealed , 208 ; early- 37th Regiment , 257 warning , 199 ; fortii ed , vi , 36 , 121 , 209 , 37th Regiment of Madras Native Infantry , 206 218 – 20 , 281 , 493 ; sand- bagged , 210 , 218 , 49th Regiment , 205 , 286 232 , 309 55th Regiment , 286 , 306 Battle at Dinghai, showing the British attacks, 98th Regiment , 384 Qing defensive positions, and the walled town of Dinghai , 305 Ackbar , 385 Battle at Guangzhou, showing British Aigun , 500 attacks , 241 American citizens , 452 , 456 – 58 , 460 , 462 , Battle at Humen, showing the British attacks 463 – 64 , 465 – 68 , 475 , 478 , 511 , 513 and Qing defensive positions , 198 American envoys , 458 – 59 , 461 Battle at Wusong, showing British attacks and American merchants , 96 , 97 – 99 , 152 , 218 , Qing defensive positions , 380 227 , 455 – 57 , 503 Battle at Xiamen, showing main British American ships , 103 , 456 – 57 , 467 attacks and Qing defensive positions , 287 American treaties , 478 Battle at Zhapu, showing Qing defensive Amoy , 427 , 452 positions and British attacks , 376 Anhui , 50 – 51 , 88 , 111 , 163 – 64 , 178 , 324 , 328 , Battle at Zhenhai, showing the Qing defensive 331 , 353 – 54 , 358 positions and British attacks , 311 Ansei
    [Show full text]
  • Application of Envisat ASAR Image in Near Real Time Flood Monitoring
    Application of Envisat ASAR Image in Near Real Time Flood monitoring and Assessment in China Huang, Shifeng Prof., Remote Sensing Technology Application Center, China Institute of Water Resources and Hydropower Research, Beijing, China ABSTACT: China is one of the countries in which flood occurs most frequently in the world and with the current economic growth; flood disaster causes more and more economic losses. Chinese government pays more attention to flood monitoring and assessment by space technology. Since1983, NOAA(AVHRR), Landsat-TM, LANDSAT-ETM+, JERS-1, SPOT, ERS-2, Radarsat-1, CBERS-1, Envisat have been used for flood monitoring and assessment. Due to the bad weather conditions during flood, microwave remote sensing is the major tools for flood monitoring. Envisat is one of the best satellite with powerful SAR. Its application for flood monitoring has been studied and its near real time(NRT) application can be realized on the basis of real-time delivery of image. During the 2005, 2006 and 2007 flood seasons, over the 31 NRT flood monitoring based on Envisat, had been carried out in Yangtze, Songua, Huaihe, pearl river basin. The result shows that Envisat SAR is very useful data source for flood disaster monitoring and assessment. 1. INTRODUCTION China is one of the countries in which flood occurs most frequently in the world and with the current economic growth; flood disaster causes more and more economic losses. Remote sensing ( RS ) technology has its special superiority and potentiality for disaster monitoring and assessment , so it has been applied for this purpose for a long time in the whole world, especially for the disaster resulting from floods and waterlogging.
    [Show full text]
  • Impact of Changes in Land Use and Climate on the Runoff in Dawen River Basin Based on SWAT Model - 2849
    Zhao et al.: Impact of changes in land use and climate on the runoff in Dawen River Basin based on SWAT model - 2849 - IMPACT OF CHANGES IN LAND USE AND CLIMATE ON THE RUNOFF BASED ON SWAT MODEL IN DAWEN RIVER BASIN, CHINA ZHAO, Q.* – GAO, Q. – ZOU, C. H. – YAO, T. – LI, X. M. School of Water Conservancy and Environment, University of Jinan 336 Nanxinzhuang West Road, Jinan 250022, Shandong Province, China (phone: +86-135-8910-8827) *Corresponding author e-mail: [email protected]; phone: +86-135-8910-8827 (Received 8th Oct 2018; accepted 25th Jan 2019) Abstract. A distributed hydrological model (SWAT), which is widely used both domestically and internationally, was selected to quantitatively analyze the impact of land use and climate change on runoff in this paper in Dawen River Basin, China. The calibration and validation results obtained at Daicunba and Laiwu hydrological stations yield R2 values of 0.83 and 0.80 and 0.73 and 0.69 and the Ens values of 0.79 and 0.76 and 0.71 and 0.72, respectively. Taking 1980-1990 as the reference period, the annual runoff increased by 288 million m3, which was caused by changes in the land use of basin from 1991 to 2004, whereas the annual runoff decreased by 132 million m3 due to climate change. Land use changed from 2005 to 2015, which resulted in an increase in annual runoff of 13 million m3, and annual changes in climate caused a decrease in annual runoff of 61 million m3. An extreme land use scenario simulation analysis shows that, compared to the current land use simulation in 2000, the runoff of cultivated land scenarios and forest land scenarios was reduced by 38.3% and 19.8%, respectively, and the runoff of grassland scenarios increased by 4.3%.
    [Show full text]
  • Modelling and Analysis of River Networks Based on Complex Networks Theory
    Proceedings of the 2012 2nd International Conference on Computer and Information Application (ICCIA 2012) Modelling and analysis of river networks based on complex networks theory Xuewen Wu, Ling Li, Yonggang Qu College of Computer and Information Hohai University Nanjing 210098, Jiangsu, China [email protected], [email protected], [email protected] Abstract—River systems are open and self-organizing rivers, water pumps and so on. They are divided into two complex systems. Complex networks theory can well combine categories in terms of hydraulic function: natural nodes and rivers' macro properties with their microscopic properties. engineering nodes, as shown in Fig.1. Different methods are This paper builds a river network model based on complex taken in different nodes. networks theory and describes its characteristics. After the Natural nodes include river sources, river confluences, analysis of the model used in Haihe River Basin, it shows that river bifurcations, river outlets and so forth. These nodes do Haihe River Basin network has the small-world characteristics. not contain any water conservancy facilities, which only This work provides a new approach to research the properties have the characteristics of natural laws of the river itself. of river networks, so that to predict and control its behavior. Engineering nodes include hydropower stations, Key words-river network; complex networks; modelling; reservoirs, and sluices, pumping stations, water transfer Haihe projects, comprehensive engineering and other water conservancy project facilities as shown in Fig. 1. These water conservancy facilities play an important role in I. INTRODUCTION regulation and distribution of water resources, which can With certain hydraulic connections, A large number of change the river flow under manual control and result in the rivers, intersections, and water conservancy facilities significant different characteristics between upstream and together constitute a criss-cross river networks system, which downstream.
    [Show full text]
  • The Extent and Composition of Disaster Relief After China's 1823 Flood: New Archival Evidence
    The extent and composition of disaster relief after China's 1823 flood: New archival evidence Ni Yuping History Department, Tsinghua University Martin Uebele Faculty of Arts, University of Groningen Abstract: In 1823, large parts of China were drowned in one of the heaviest floods of the whole Qing dynasty (1644-1911), but detailed data on its impact and government responses have so far been scattered. Due to a recent reorganization of China’s First Historical Archives, however, this paper is able to provide new evidence about the flood’s impact as well as the extent and composition of central government disaster relief. This matters especially because many scholars believe that because of this flood, China entered into the “Daoguang Depression” providing the background for China’s “lost century” in connection with interior and exterior security issues such as the First Opium War (1839-42), and the Taiping rebellion (1850-64). Our evidence thus may help to understand if these combined challenges exceeded state capacity when modernization would have required internal reform more than ever. We find that in the 17 provinces for which we have data at least 20 percent of all counties were flooded, half of them seriously. The combination of tax relief, water works and direct payments grew proportionally with the share of counties affected by the flood and totaled to about 26 million taels of silver, more than half of annual fiscal revenue of the Qing state. Key words: Daoguang Depression, disaster relief, China, 19th century, state capacity 1. Introduction No matter if from the perspective of meteorological, disaster or economic history, the year of 1823 (the third year of the Daoguang emperor’s rule) was an all-important node.
    [Show full text]
  • Recent Anthropogenic Curtailing of Yellow River Runoff and Sediment Load Is Unprecedented Over the Past 500 Y
    Recent anthropogenic curtailing of Yellow River runoff and sediment load is unprecedented over the past 500 y Yu Liua,b,c,d,1, Huiming Songa,b,e, Zhisheng Ana,b,e,1, Changfeng Suna,b, Valerie Trouetf, Qiufang Caia,b,c, Ruoshi Liud, Steven W. Leavittf, Yi Songa, Qiang Lia,b,e, Congxi Fanga, Weijian Zhoua,b, Yinke Yangg, Zhao Jina,b, Yunqiang Wanga,b, Junyan Suna, Xingmin Muh, Ying Leia, Lu Wanga, Xuxiang Lid, Meng Rena, Linlin Cuia, and Xueli Zenga aThe State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, 710061 Xi’an, China; bCAS Center for Excellence in Quaternary Science and Global Change, Chinese Academy of Sciences, 710061 Xi’an, China; cOpen Studio for Oceanic-Continental Climate and Environment Changes, Pilot National Laboratory for Marine Science and Technology, 266061 Qingdao, China; dSchool of Human Settlements and Civil Engineering, Xi’an Jiaotong University, 710049 Xi’an, China; eInterdisciplinary Research Center of Earth Science Frontier, Beijing Normal University, 100875 Beijing, China; fLaboratory of Tree-Ring Research, The University of Arizona, Tucson, AZ 85721; gSchool of Environmental Science and Engineering, Chang’an University, 710054 Xi’an, China; and hState Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences & Ministry of Water Resources, 712100 Yangling, China Contributed by Zhisheng An, May 29, 2020 (sent for review December 26, 2019; reviewed by Achim Bräuning and Hongyan Liu) The Yellow River (YR) is the fifth-longest and the most sediment- load of the YR has declined by ∼90% over the past 60 y (10), laden river in the world.
    [Show full text]
  • The Need for Integrated Management for the Endangered Miyun Resevoir
    Quenching Beijing’s Thirst: The Need for Integrated Management for the Endangered Miyun Resevoir By Christoph Peisert and Eva Sternfeld Miyun reservoir, a large reservoir northeast of Beijing municipality, is the Chinese capital’s most important source of drinking water. For many years the Beijing municipal government has made great efforts to protect the reservoir and its catchment area. However, successful implementation has been hampered by numerous user conflicts. This paper investigates the origin and various types of conflicts, which include inter-provincial, city-county disputes, as well as conflicts between county government and local residents living in the water protection zone. The magnitude of these conflicts and continued deteriorating quality of the reservoir underline the need for integrated watershed management approaches as stipulated in the 2002 revised Water Law, and the adoption of a water economy that includes the costs for water protection and compensation for those required to carry out watershed protection activities. he large Miyun reservoir, built during the Great Natural Determinants of the Beijing Water Crisis Leap Forward period (1958-1960) in the Beijing municipality is located in the dry northeast Tnortheast of Beijing municipality, is a critical edge of the North China Plain bordering the Mongolian source of drinking water for the 14 million people living Plateau in central Hebei province. Since the last in this booming metropolis. Considering the huge administrative reforms in 1958, the Chinese capital population reliant on the catchment for drinking water, and its rural hinterland were expanded to cover a total Miyun reservoir is one of the most important water area of 16,800 square kilometers (km2) with about protection areas in the world.
    [Show full text]
  • IWHR Annual Report 2018
    Printed on recycled paper ANNUAL REPORT IWHR China Institute of Water Resources and Hydropower Research 中国水利水电科学研究院 ANNUAL REPORT IWHR China Institute of Water Resources and Hydropower Research 中国水利水电科学研究院 ANNUAL REPORT IWHR China Institute of Water Resources and Hydropower Research 中国水利水电科学研究院 WELCOME MESSAGE Annual Report 2018 CHINA INSTITUTE OF WATER RESOURCES AND HYDROPOWER RESEARCH The year 2018 is undoubtedly an unusual year for IWHR as it originality recognized by national and provincial prizes. Covering 18 research disciplines marks the 40th anniversary of China’s adoption of Reform and and 93 research directions now, IWHR has established 4 national and 8 ministerial research Opening-up Policy and the 60th anniversary of IWHR, which centers, 1 state key laboratory and 2 ministerial key laboratories, representing China’s is more special to the Institute itself. In Chinese culture, 60 largest research center and training base of water resources and hydropower with the most decades is called a Jiazi which means a cycle of development complete disciplines and best research conditions. and is therefore of special significance. During the sixty years of development, IWHR people have worked with all our efforts Over the 60 years, IWHR has always been aiming high with global vision. As China keeps to pursue the prosperity of the nation and happiness of the rising, IWHR has accelerated its international cooperation and exchange and made people, bearing this in mind as our mission and responsibility remarkable achievement. IWHR has established cooperative relationship with over 100 as we went ups and down with the country. We have proudly foreign academic organizations and overseas research institutes and universities.
    [Show full text]
  • LCSH Section Y
    Y-Bj dialects Yabakei (Japan) Yacatas Site (Mexico) USE Yugambeh-Bundjalung dialects BT Valleys—Japan BT Mexico—Antiquities Y-cars Yabakei (Japan) Yaccas USE General Motors Y-cars USE Yaba Valley (Japan) USE Xanthorrhoea Y chromosome Yabarana Indians (May Subd Geog) Yachats River (Or.) UF Chromosome Y UF Yaurana Indians BT Rivers—Oregon BT Sex chromosomes BT Indians of South America—Venezuela Yachats River Valley (Or.) — Abnormalities (May Subd Geog) Yabbie culture UF Yachats Valley (Or.) BT Sex chromosome abnormalities USE Yabby culture BT Valleys—Oregon Y Fenai (Wales) Yabbies (May Subd Geog) Yachats Valley (Or.) USE Menai Strait (Wales) [QL444.M33 (Zoology)] USE Yachats River Valley (Or.) Y-G personality test BT Cherax Yachikadai Iseki (Haga-machi, Tochigi-ken, Japan) USE Yatabe-Guilford personality test Yabby culture (May Subd Geog) USE Yachikadai Site (Haga-machi, Tochigi-ken, Y.M.C.A. libraries [SH380.94.Y32] Japan) USE Young Men's Christian Association libraries UF Yabbie culture Yachikadai Site (Haga-machi, Tochigi-ken, Japan) Y maze Yabby farming This heading is not valid for use as a geographic BT Maze tests BT Crayfish culture subdivision. Y Mountain (Utah) Yabby farming UF Yachikadai Iseki (Haga-machi, Tochigi-ken, BT Mountains—Utah USE Yabby culture Japan) Wasatch Range (Utah and Idaho) YABC (Behavioral assessment) BT Japan—Antiquities Y-particles USE Young Adult Behavior Checklist Yachinaka Tate Iseki (Hinai-machi, Japan) USE Hyperons Yabe family (Not Subd Geog) USE Yachinaka Tate Site (Hinai-machi, Japan) Y-platform cars Yabem (Papua New Guinean people) Yachinaka Tate Site (Hinai-machi, Japan) USE General Motors Y-cars USE Yabim (Papua New Guinean people) This heading is not valid for use as a geographic subdivision.
    [Show full text]
  • Attribution of Runoff Variation in the Headwaters of the Yangtze River
    International Journal of Environmental Research and Public Health Article Attribution of Runoff Variation in the Headwaters of the Yangtze River Based on the Budyko Hypothesis Junlong Liu , Jin Chen *, Jijun Xu, Yuru Lin, Zhe Yuan and Mingyuan Zhou Changjiang Scientific Research Institute of Changjiang Water Resources Commission, Wuhan 430010, China * Correspondence: [email protected] Received: 30 May 2019; Accepted: 11 July 2019; Published: 13 July 2019 Abstract: Quantifying the contributions of climate change and human activities on runoff changes is of great importance for water resource management, sustainable water resource utilization, and sustainable development of society. In this study, hydrological and climatic data from hydrological and meteorological stations in the headwaters of the Yangtze River (YRHA) from 1966 to 2013 were used to quantitatively attribute the runoff change to the impacts of climate change and human activities separately. Firstly, the change trends in precipitation, runoff depth and potential evapotranspiration were analyzed by the Mann-Kendall test method. Three methods, secondly, including ordered clustering, Mann-Kendall and cumulative anomaly curve were adopted to detect the change points of runoff at Zhimenda hydrological station and partition the whole study period into two sub-periods at the change point (base and impacted periods). Then, the elasticity coefficient method based on the Budyko hypothesis was applied to calculate elasticity coefficients of runoff to precipitation, potential evapotranspiration and land use/cover during the two periods, and to evaluate the contributions of climate change and human activities. Results indicated that during 1966–2013, runoff depth, precipitation and potential evapotranspiration all showed a significant increasing trend, 1 1 1 with increasing rates of 7.26 mm decade− , 18.725 mm decade− and 7.228 mm decade− , respectively.
    [Show full text]