Challenges and Opportunities of International University Partnerships to Support Water Management
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Flash Flood in the Himalayas for June 5.Indd
Information on the Occasion of World Environment Day, June 2007 Flash Floods in the Himalayas The Himalayas are one of the youngest mountain ranges on earth and represent a high energy environment very much prone to natural disasters. High relief, steep slopes, complex geological structures with active tectonic processes and continued seismic activities, and a climate characterised by great seasonality in rainfall, all combine to make natural disasters, especially water-induced hazards, common phenomena. Flash fl oods are among the more devastating types of hazard as they occur rapidly with little Figure 1: a. types of water-related disasters; b. distribution of water related lead time for warning, and transport tremendous disasters by continents; c. different types of fl oods (data source: Jonkman 2005) amounts of water and debris at high velocity (Fig. 1). Flash fl oods affect thousands of people in the Himalayan region every year – their lives, homes, and livelihoods – along with expensive infrastructure Figure 2: Different types of fl ash fl oods in the HKH region There are several different types of fl ash fl ood. The most common include intense rainfall fl oods (IRF); glacial lake outburst fl oods (GLOFs), landslide dam outburst fl oods (LDOF), and fl ash fl oods caused by rapid snowmelt (RSM) and ice (Fig. 2). Failure of dams and other hydraulic structures can also lead to fl ash fl oods. Intense rainfall Intense rainfall is the most common cause of fl ash fl oods in the Himalayan region. These events may last from several minutes to several days. Such events may happen anywhere but are more common to mountain catchments. -
Landslide Dam Lakes and Glacial Lakes
Chapter 3: Landslide Dam Lakes and Glacial Lakes Chapter 3: Landslide Dam Lakes and Glacial Lakes The triggers of flash floods in the Hindu Kush Himalayas include catastrophic failure of landslide dams that retain landslide dam lakes, and of moraine or ice dams that retain glacial lakes. Flash flooding caused by landslide dam failure is a significant hazard in the region and is particularly common in the high rugged mountain areas of China, India, Nepal, and Pakistan (Zhu and Li 2000). The previous chapter looked at ways of preventing the formation of landslide dams by reducing the prevalence of landslides and debris flows. Another important approach to mitigating flash floods is to reduce the likelihood of dam failure, and/or to put in place warning and avoidance mechanisms to reduce the risk in the case of failure. In order to design appropriate measures, it is important first to understand the formation process, failure mechanism, and risk mitigation techniques for both types of lake. Landslide Dam Lakes Formation Landslide dam lakes can be created as a result of a broad range of mass movements in different geomorphological settings. Dams form most frequently as a result of rock and earth slumps and slides, debris and mudflows, and rock and debris avalanches in areas where narrow river valleys are bordered by steep and rugged mountain slopes (Zhu and Li 2000). A lake then forms behind the dam as a result of the continuous inflow of water from the river (Figure 4). Only a small amount of material is needed to form a dam in a narrow valley, and even a small mass movement can be sufficient. -
Geosites and Geotouristic Attractions Proposed for the Project Geopark Colca and Volcanoes of Andagua, Peru
Geoheritage (2018) 10:707–729 https://doi.org/10.1007/s12371-018-0307-y ORIGINAL ARTICLE Geosites and Geotouristic Attractions Proposed for the Project Geopark Colca and Volcanoes of Andagua, Peru Andrzej Gałaś1 & Andrzej Paulo1 & Krzysztof Gaidzik2,3 & Bilberto Zavala4 & Tomasz Kalicki5 & Danitza Churata4 & Slávka Gałaś1 & Jersey Mariño4 Received: 15 July 2016 /Accepted: 18 May 2018 /Published online: 7 June 2018 # The Author(s) 2018 Abstract The Colca Canyon (Central Andes, Southern Peru), about 100 km long and 1–3 km deep, forms a magnificent cross section of the Earth’s crust giving insight into mutual relations between lithostratigraphical units, and allowing relatively easy interpretation of the fascinating geological history written in the rocky beds and relief. Current activity of tectonic processes related to the subduction of the Nazca plate beneath the South American Plate exposed the geological heritage within study area. Well- developed tectonic structures present high scientific values. The volcanic landforms in the Valley of the Volcanoes and around the Colca Canyon include lava flows, scoria cones and small lava domes. They represent natural phenomena which gained recognition among tourists, scientists and local people. Studies performed by the Polish Scientific Expedition to Peru since 2003 recognized in area of Colca Canyon and Valley of the Volcanoes high geodiversity, potential for geoturism but also requirements for protectection. The idea of creating geopark gained recently the approval of regional and local authorities with support from the local National Geological Survey (INGEMMET). The Geopark Colca and Volcanoes of Andagua would strengthen the relatively poor system of the protected areas in the Arequipa department, increasing the touristic attractiveness and determine constraints for sustained regional development. -
UGEL ESPINAR O Cerro Salla Lori
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Investigating the Effectiveness of a Variety of Household Water Treatment Systems on Microbially Contaminated Water in Arequipa, Peru 2004
INVESTIGATING THE EFFECTIVENESS OF A VARIETY OF HOUSEHOLD WATER TREATMENT SYSTEMS ON MICROBIALLY CONTAMINATED WATER IN AREQUIPA, PERU 2004 By: Amber Jaycocks Jennifer Lappin Robert Malies Supervisor: Susan Murcott Supported by MIT Undergraduate Research Opportunity Program (UROP) Massachusetts Institute of Technology Department of Civil and Environmental Engineering Summer, 2004 Acknowledgement: This project could not have been undertaken without the assistance of the team’s host, Padre Alex Busutil of Arequipa, the mentoring of Tom Clasen, Lecturer, London School of Hygiene and Tropical Medicine, or the technical support of CEPIS (Center for Sanitary Engineering and Environmental Sciences, Pan American Health Organization. 1 Table of Contents 1.0 MIT Agua Peru Investigation 1 1.1 Design Overview 1 1.2 Filter Descriptions 2 1.2.1 Household Slow Sand Filter, HSSF 2 1.2.2 Pozzani Ceramic Candle Filters, Two Candles 3 1.2.3 Katadyn Ceramic Candle Filters, Two Candles 5 1.2.4 Table Filter, Filtro de Mesa 6 1.3 Filter Construction and Assemblage 7 1.4 Obtaining Materials 8 1.5 Sample Water Characteristics 9 2.0 Testing Procedures 9 2.1 General Procedures for TTC and Turbidity 9 2.1.1 TTC Design 11 2.1.2 Turbidity 11 2.2 Flow Rate 12 2.3 Chlorine 12 3.0 Field Results and Discussion 13 3.1 Study Site 13 3.1.1 Demographics 13 3.1.2 Water Resources and Uses 14 3.2 Water Supplies to Households 16 3.2.1 La Joya, Arequipa 17 3.2.2 Cerrito Buena Vista 19 3.2.3 Raw Water Sources 20 4.0 Filter Results and Discussions 20 4.1 Household Slow Sand Filter, -
Plugs Or Flood-Makers? the Unstable Landslide
Geomorphology 248 (2015) 237–251 Contents lists available at ScienceDirect Geomorphology journal homepage: www.elsevier.com/locate/geomorph Plugs or flood-makers? The unstable landslide dams of eastern Oregon E.B. Safran a,⁎, J.E. O'Connor b,L.L.Elyc, P.K. House d,G.Grante,K.Harrityf,1,K.Croallf,1,E.Jonesf,1 a Environmental Studies Program, Lewis & Clark College, MSC 55, 0615 SW Palatine Hill Road, Portland, OR 97219, USA b U.S. Geological Survey, Geology, Minerals, Energy, and Geophysics Science Center, 2130 SW 5th Avenue, Portland, OR 97201, USA c Department of Geological Sciences, Central Washington University, Ellensburg, WA 98926, USA d U.S. Geological Survey, Geology, Minerals, Energy, and Geophysics Science Center, 2255 N. Gemini Drive, Flagstaff, AZ 86001, USA e U.S. Forest Service, Pacific Northwest Research Station, 3200 SW Jefferson Way, Corvallis, OR 97331, USA f Lewis & Clark College, 0615 SW Palatine Hill Road, Portland, OR 97219, USA article info abstract Article history: Landslides into valley bottoms can affect longitudinal profiles of rivers, thereby influencing landscape evolution Received 25 November 2014 through base-level changes. Large landslides can hinder river incision by temporarily damming rivers, but cata- Received in revised form 26 June 2015 strophic failure of landslide dams may generate large floods that could promote incision. Dam stability therefore Accepted 26 June 2015 strongly modulates the effects of landslide dams and might be expected to vary among geologic settings. Here, Available online 8 July 2015 we investigate the morphometry, stability, and effects on adjacent channel profiles of 17 former and current landslide dams in eastern Oregon. -
A Preliminary Study of the Failure Modes and Process of Landslide Dams Due to Upstream Flow
water Article A Preliminary Study of the Failure Modes and Process of Landslide Dams Due to Upstream Flow Xinghua Zhu 1 , Jianbing Peng 1,*, Cheng Jiang 2 and Weilong Guo 3 1 College of Geological Engineering and Surveying of Chang’an University/Key Laboratory of Western China, Mineral Resources and Geological Engineering, Xi’an 710054, China; [email protected] 2 School of Environmental Science and Engineering, Chang’an University, Xi’an 710054, China; [email protected] 3 Shaanxi Institute of Engineering Prospecting Co. Ltd., Xi’an 710068, China; [email protected] * Correspondence: [email protected]; Tel.: +86-158 9139 1126 Received: 5 May 2019; Accepted: 24 May 2019; Published: 28 May 2019 Abstract: In the process of mineral development, large-scale flash floods (or debris flows) can be induced by the failure of landslide dams formed by the disorganized stacking of mine waste. In this study, the modes and processes of mine waste dam failures were explored using 13 experimental tests based on the field investigation of landslide dams in the Xiaoqinling gold mining area in China. Our 13 mine waste dam experiments exhibited three failure modes: (i) Piping, overtopping, and erosion; (ii) overtopping and soil collapse; and (iii) overtopping and erosion. In addition, the failure processes of the landslide dams included impoundment, seepage, overtopping, and soil erosion. Different experimental conditions would inevitably lead to different failure processes and modes, with the failure modes being primarily determined by the seepage characteristics. Overtopping was the triggering condition for dam failure. The landslide dam failure process was determined based on the particle size of the mine waste and the shape of the dam. -
Comprender La Agricultura En Los Andes Peruanos: Religión En La Comunidad De Yanque (Caylloma, Arequipa)
Comprender la agricultura en los Andes Peruanos: Religión en la comunidad de Yanque (Caylloma, Arequipa) Item Type info:eu-repo/semantics/article Authors Sánchez Dávila, Mario Elmer Publisher Centro de Estudios Antropológicos Luis Eduardo Valcárcel Rights info:eu-repo/semantics/openAccess Download date 02/10/2021 15:30:07 Link to Item http://hdl.handle.net/10757/622562 Comprender la agricultura en los Andes Peruanos: Religión en la comunidad de Yanque (Caylloma, Arequipa) Understanding agriculture in the Peruvian Andes: Religión in the community of Yanque (Caylloma, Arequipa) MARIO E. SÁNCHEZ DÁVILA1 Pontificia Universidad Católica del Perú (PUCP) Universidad Peruana de Ciencias Aplicadas (UPC) [email protected] Recibido: 04 de julio de 2017 Aceptado: 01 de septiembre de 2017 Resumen Este artículo analiza la agricultura en el mundo Andino a través del caso la comunidad de Yanque, distrito de la provincia de Caylloma, departamento de Arequipa (Perú). La agricultura es su principal actividad social debido a la importancia colectiva no sólo de sus manifestaciones económicas y políticas, sino también religiosas. Por eso, este artículo se enfoca en las expresiones religiosas más visibles: el sincretismo católico-quechua y la fiesta laboral ritualizada del Yarqa Aspiy. Palabras clave: andes, agricultura, religión, Perú Abstract This paper analyzes agriculture in the Andean world through the case of the community of Yanque, district of Caylloma province, department of Arequipa (Perú). Agriculture comes to have an organizing force in this community not only for its economic and political effects, but also for its religious dimensions. For this reason, this paper focuses on one of the community’s most visible religious expressions: the Yarqa Aspiy, describing the ways in which this festival ritualizes labor in performances of Catholic-Quechua syncretism. -
INDIGENOUS LIFE PROJECTS and EXTRACTIVISM Ethnographies from South America Edited by CECILIE VINDAL ØDEGAARD and JUAN JAVIER RIVERA ANDÍA
INDIGENOUS LIFE PROJECTS AND EXTRACTIVISM Ethnographies from South America Edited by CECILIE VINDAL ØDEGAARD and JUAN JAVIER RIVERA ANDÍA APPROACHES TO SOCIAL INEQUALITY AND DIFFERENCE Approaches to Social Inequality and Difference Series Editors Edvard Hviding University of Bergen Bergen, Norway Synnøve Bendixsen University of Bergen Bergen, Norway The book series contributes a wealth of new perspectives aiming to denaturalize ongoing social, economic and cultural trends such as the processes of ‘crimigration’ and racialization, fast-growing social-economic inequalities, depoliticization or technologization of policy, and simultaneously a politicization of difference. By treating naturalization simultaneously as a phenomenon in the world, and as a rudimentary analytical concept for further development and theoretical diversification, we identify a shared point of departure for all volumes in this series, in a search to analyze how difference is produced, governed and reconfigured in a rapidly changing world. By theorizing rich, globally comparative ethnographic materials on how racial/cultural/civilization differences are currently specified and naturalized, the series will throw new light on crucial links between differences, whether biologized and culturalized, and various forms of ‘social inequality’ that are produced in contemporary global social and political formations. More information about this series at http://www.palgrave.com/gp/series/14775 Cecilie Vindal Ødegaard Juan Javier Rivera Andía Editors Indigenous Life Projects and Extractivism Ethnographies from South America Editors Cecilie Vindal Ødegaard Juan Javier Rivera Andía University of Bergen Universitat Autònoma de Barcelona Bergen, Norway Barcelona, Spain Approaches to Social Inequality and Difference ISBN 978-3-319-93434-1 ISBN 978-3-319-93435-8 (eBook) https://doi.org/10.1007/978-3-319-93435-8 Library of Congress Control Number: 2018954928 © The Editor(s) (if applicable) and The Author(s) 2019. -
Final Project Report
STRENGTHENING CAPACITIES FOR DISASTER RISK REDUCTION AND INCREASING RESILIENCE IN COMMUNITIES OF CAYLLOMA, AREQUIPA. FINAL PROJECT REPORT OCTOBER 2018 – DECEMBER 2019 GENERAL PROJECT INFORMATION STRENGTHENING CAPACITIES FOR DISASTER RISK Project Title REDUCTION AND INCREASING RESILIENCE IN COMMUNITIES OF CAYLLOMA, AREQUIPA. Award number 72OFDA18GR00319 Registration number REQ-OFDA-18-000751 Start date October 01, 2018 Duration 15 months Country / region: Peru / department of Arequipa, province of Caylloma. Reported period: October 2018 – December 2019 Date of report: February 21, 2020 Adventist Development and Relief Agency International - ADRA INTERNATIONAL Report for: Debra Olson, Program Manager, Program Implementation Unit. Nestor Mogollon, Director of Monitoring and Evaluation. Adventist Development and Relief Agency Perú – ADRA Perú Víctor Huamán, Project Manager. Report by: cell phone: 51 - 997 555 483 - email: [email protected] Erick Quispe, Project Field Coordinator. cell phone: 51 - 966 315 430 - email: [email protected] REPORTE ANUAL: OCTUBRE 2018 – SETIEMBRE 2019 1. EXECUTIVE SUMMARY Since 2016, the Sabancaya volcano has registered permanent eruptive activity with gas, ash and earthquake emissions, which together with other natural events such as earthquakes, frost, intense rains and landslides interrupt local development and affect thousands of people in the Caylloma province. For this reason, the project aimed to integrate disaster risk management into institutional management tools of local governments in the Caylloma Province, with the participation of the population and collaboration at the regional and national levels. The project " Allichakusun ante desastres" (“Preparing ourselves for disasters”) began in October 2018 and ended in December 2019. It executed 100% of the financing received from USAID, also achieving an income of S/. -
Advancing Employment in Apec for Persons with Disabilities
ADVANCING EMPLOYMENT IN APEC FOR PERSONS WITH DISABILITIES A BASELINE STUDY OF OPPORTUNITIES IN THE REGION September 2017 This publication was produced by Nathan Associates Inc. for review by the United States Agency for International Development. ADVANCING EMPLOYMENT IN APEC FOR PERSONS WITH DISABILITIES A BASELINE STUDY OF OPPORTUNITIES IN THE REGION DISCLAIMER This document is made possible by the support of the American people through the United States Agency for International Development (USAID). Its contents are the sole responsibility of the author(s) and do not necessarily reflect the views of USAID or the U. S. government. CONTENTS Acronyms i Acknowledgements ii Executive Summary 1 Introduction 3 The Economic Case for Advancing the Employment of Persons with Disabilities 3 Key Disability Concepts 5 Disability: Causes and Prevalence 7 Trends and Challenges in Increasing Employment of Persons with Disabilities 10 Employment-related Barriers Facing Persons with Disabilities 10 Inter-relationship of employment with social benefits 12 The Business Case for Hiring Persons with Disabilities 12 International Frameworks of Disability 13 Recent International Frameworks 13 Convention on the Rights of Persons with Disabilities 13 UNESCAP Incheon Strategy 14 Early ILO and UN Efforts 14 APEC Economy Laws, Regulations, and Policies 15 General Trends in APEC Economies 15 Topical Economy Highlights 15 Quotas, Targets, and Incentives for Hiring Persons with Disabilities 21 Quota and Target Systems 21 Use of Quotas 21 Targets in the United States -
Gold Standard Local Stakeholder Consultation Report CONTENTS
Gold Standard Local Stakeholder Consultation Report CONTENTS A. Invitations 1. Invitation tracking table 2. Text of invitations or newspaper ads B. Meeting 1. Program 2. Non-technical summary 3. Participants i. list ii. feedback forms 4. Pictures 5. Outcomes of consultation i. Minutes of the meeting ii. Assessment of comments iii. Revisit sustainable development assessment iv. Summary of alterations based on comments C. Sustainable development matrix 1. Own sustainable development assessment 2. Outcome blind exercise stakeholders 3. Consolidated sustainable development matrix D. Preparation of Stakeholder Feedback Round Annex 1: Participant list Annex 2: Feedback forms Gold Standard Local Stakeholder Consultation SECTION A. Invitations A.1. Invitation tracking table [See Toolkit 2.6 and Toolkit Annex J] The Regional Government of Arequipa (RGA) has a Unit operator called COPASA which executes with the support of UNDP a cook stoves project in the Arequipa region. In fulfillment of the agreement signed with MICROSOL, RGA is part of Qori Q‟oncha, a PoA for diffusion of improved stoves in Peru that has been registered under the Gold Standard. The objective of the meeting was to explain the characteristics of the project to the stakeholders and to know their opinions and suggestions about the indicators matrix referred to that. This activity was developed on Thursday, June 28th of 2012 at the Auditorium of the District Municipality of Chivay from the Caylloma Province, region of Arequipa. It was organized by the Regional Government of Arequipa in coordination with the managing entity Microsol, and had the support of the Municipalities of the districts where RGA implements the improved cook stoves project.