Disaster Management Partners in Nepal
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Pin Information for the Arria® GX EP1AGX50C/D Device Version 1.4 Bank VREF Group Pin Name/Function Optional Function(s) Configuration x8/x9 Mode x16/x18 Mode x36 Mode Number Function EP1AGX50DF780 EP1AGX50CF484 EP1AGX50DF1152 DQ group for DQS DQS for group DQ (F1152) mode DQS for group DQ (F780, F484) mode (1) DQS for group DQ (F1152) mode DQS for group DQ (F780, F484) mode (1) DQS for group DQ (F1152) mode VCCD_PLL7 K25 VCCA_PLL7 J26 GNDA_PLL7 K26 GNDA_PLL7 J25 B2 VREFB2N0 FPLL7CLKp INPUT C34 B2 VREFB2N0 FPLL7CLKn INPUT C33 B2 VREFB2N0 IO DIFFIO_TX41p J28 B2 VREFB2N0 IO DIFFIO_TX41n K27 B2 VREFB2N0 IO DIFFIO_RX40p E34 B2 VREFB2N0 IO DIFFIO_RX40n D34 B2 VREFB2N0 IO DIFFIO_TX40p J30 B2 VREFB2N0 IO DIFFIO_TX40n J29 B2 VREFB2N0 IO DIFFIO_RX39p F32 B2 VREFB2N0 IO DIFFIO_RX39n F31 B2 VREFB2N0 IO DIFFIO_TX39p K30 B2 VREFB2N0 IO DIFFIO_TX39n K29 B2 VREFB2N0 VREFB2N0 VREFB2N0 R30 T21 J18 B2 VREFB2N0 IO DIFFIO_RX38p F34 B2 VREFB2N0 IO DIFFIO_RX38n F33 B2 VREFB2N0 IO DIFFIO_TX38p L26 B2 VREFB2N0 IO DIFFIO_TX38n L25 B2 VREFB2N0 IO DIFFIO_RX37p G33 B2 VREFB2N0 IO DIFFIO_RX37n G32 B2 VREFB2N0 IO DIFFIO_TX37p M26 B2 VREFB2N0 IO DIFFIO_TX37n M25 B2 VREFB2N0 IO DIFFIO_RX36p H32 C28 B20 B2 VREFB2N0 IO DIFFIO_RX36n H31 C27 B19 B2 VREFB2N0 IO DIFFIO_TX36p K28 H23 D19 B2 VREFB2N0 IO DIFFIO_TX36n L28 H22 D18 B2 VREFB2N0 IO DIFFIO_RX35p G34 D28 A17 B2 VREFB2N0 IO DIFFIO_RX35n H34 D27 B17 B2 VREFB2N0 IO DIFFIO_TX35p L29 F24 C20 PT-EP1AGX50C/D-1.4 Copyright © 2009 Altera Corp. Pin List Page 1 of 47 Pin Information for the Arria® GX EP1AGX50C/D Device Version -
Damage Mapping of April 2015 Nepal Earthquake Using Small
J-Rapid Final Workshop 21 June, 2016, Kathmandu Inventory mapping of landslides induced by the Gorkha earthquake 2015 and a proposal for hazard mapping of future landslides for making a plan of better reconstruction "Impact on infrastructure by Gorkha earthquake 2015 induced landslides" Masahiro CHIGIRA Masahiro CHIGIRA Professor, Disaster Prevention Research Institute, Professor, Disaster Prevention Research Institute, Kyoto University Kyoto University Vishnu DANGOL Vishnu DANGOL Professor, Department of Geology, Professor, Department of Geology, Tribhuvan University Tribhuvan University Objective 1. to make an inventory mapping on landslides, cracks, and landslide dams induced by the Nepal earthquake and to investigate their formative mechanisms 2. to detect displaced areas of slope surfaces, of which future susceptibility to landslides would be evaluated on the basis of geology, geomorphology, and groundwater conditions. 3. propose a methodology of hazard mapping for earthquake-induced landslides in Nepal. Members (Japan side) 1. Masahiro CHIGIRA (Kyoto Univ.) PI Applied Geology 2. Daisuke HIGAKI (Hirosaki Univ.) Landslide control 3. Hiroshi YAGI (Yamagata Univ.) Landslide susceptibility mapping 4. Akihiko WAKAI (Gunma Univ.) Geotechnical analysis of landslide 5. Hiroshi, P. SATO (Nihon Univ.) Remote sensing 6. Go, SATO (Teikyo Heisei Univ.) Geomorphology 7. Ching-Ying, TSOU (Hirosaki Univ.) GIS analysis 8. Akiyo YATAGAI (Res. Inst. Humanity and Nature) Meteorology Members (Nepali side) 1. Vishnu DANGOL (Tribhuvan Univ.) PI Applied Geology 2. Smajwal BAJRACHARYA (ICIMOD) Remote sensing 3. Shanmukhesh Chandra AMATYA (DWIDP) Hydrogeology 4. Tuk Lal ADHIKARI (ITECO-Nepal) Geotechnical Field survey • Trishuli River catchment from Trishuli to Syabrubesi (29 October to 1 November, 2015) • Sun Kosi and Bhote Kosi River catchments from Bansaghu to Kodari. -
Assessment of Water Availability in Major River Basins of Western Nepal
XIIIth World Water Congress, 1- 4 September, 2008, Montpellier, France ASSESSMENT OF WATER AVAILABILITY IN MAJOR RIVER BASINS OF WESTERN NEPAL. Mr. Jagat K. Bhusal, Senior Divisional Hydrologists, Department of Hydrology and Meteorology, Nepal Mr. Om Ratna Bajracharya Senior Divisional Hydrologists, Department of Hydrology and Meteorology, Nepal Mr. Lekh Nath Bagale, Hydrologist Engineer, Department of Hydrology and Meteorology, Nepal ABSTRACT Nepal gets about 80 % of annual rainfall during monsoon which lasts about 100 days only. Most rivers drain more than 75 % of the runoff during same period. In spite of limited arable land and poor irrigation facility, the backbone of Nepalese economy is still dependant on agriculture. Knowledge of the seasonal variability of rainfall and runoff plays a vital role in maximizing the yield. Integrated approach on utilizing the available water for irrigation development, hydropower generation, water supply and other uses are also other challenges in water resource management. This paper is based on study made by Nepal Irrigation Sector Project (NISP) on 77 basins of Western Nepal. Regional analyses were carried out. Long-term data of 35 basins were used to estimate the key hydrological parameters in the remaining 42 basins. Estimation on the natural flow, recurring floods and low flows, runoff- rainfall relationships, water balance, consumptive and non-consumptive water-use were made. Inter-basin groundwater flow is noticed in some areas. Hydropower development would be wise wise-uses of water resources in Nepal. Keywords: Western Nepal, Monsoon, Basins, Ground water. Rainfall, Runoff. INTRODUCTION River basins of Nepal Nepalese can be grouped broadly into (i) High Himalayan river basins, (ii) High mountain river basins (iii) Middle Mountain river basins (iv) Siwalik river basins and (v) Tarai river basins High Himal region have more snow and ice melt contribution where as High mountains and the Middle mountains find base flow sources with less frozen winter melt. -
All Change at Rasuwa Garhi Sam Cowan [email protected]
Himalaya, the Journal of the Association for Nepal and Himalayan Studies Volume 33 | Number 1 Article 14 Fall 2013 All Change at Rasuwa Garhi Sam Cowan [email protected] Follow this and additional works at: http://digitalcommons.macalester.edu/himalaya Recommended Citation Cowan, Sam (2013) "All Change at Rasuwa Garhi," Himalaya, the Journal of the Association for Nepal and Himalayan Studies: Vol. 33: No. 1, Article 14. Available at: http://digitalcommons.macalester.edu/himalaya/vol33/iss1/14 This Research Report is brought to you for free and open access by the DigitalCommons@Macalester College at DigitalCommons@Macalester College. It has been accepted for inclusion in Himalaya, the Journal of the Association for Nepal and Himalayan Studies by an authorized administrator of DigitalCommons@Macalester College. For more information, please contact [email protected]. Research Report | All Change at Rasuwa Garhi Sam Cowan From time immemorial, pilgrims, traders, artisans, and Kyirong to aid the transshipment of goods and to carry religious teachers going to Lhasa from Kathmandu had to out major trading on their own account. Jest records that decide between two main routes. One roughly followed as late as 1959 there were forty five Newar households in the line of the present road to Kodari, crossed the border Kyirong and forty in Kuti (Jest 1993). where Friendship Bridge is built and followed a steep trail The two routes were used for the invasion of Tibet in 1788 to Kuti (Tib. Nyalam). Loads were carried by porters up to and 1791 by the forces of the recently formed Gorkha this point but pack animals were used for the rest of the state under the direction of Bahadur Shah, which led to journey. -
Geo-Hydrological Hazards Induced by Gorkha Earthquake 2015
Geo-hydrological hazards induced by Gorkha Earthquake 2015: A Case of Pharak area, Everest Region, Nepal Buddhi Raj Shrestha, Narendra Raj Khanal, Joëlle Smadja, Monique Fort To cite this version: Buddhi Raj Shrestha, Narendra Raj Khanal, Joëlle Smadja, Monique Fort. Geo-hydrological hazards induced by Gorkha Earthquake 2015: A Case of Pharak area, Everest Region, Nepal. The Geograph- ical Journal of Nepal, Central Department of Geography, Faculty of Humanities and Social Studies, Tribhuvan University, 2020, 13, pp.91 - 106. 10.3126/gjn.v13i0.28154. halshs-02933571 HAL Id: halshs-02933571 https://halshs.archives-ouvertes.fr/halshs-02933571 Submitted on 17 Sep 2020 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. The Geographical Journal of Nepal Vol. 13: 91-106, 2020 Doi: http://doi.org/10.3126/gjn.v13i0.28154 Central Department of Geography, Tribhuvan University, Kathmandu, Nepal Geo-hydrological hazards induced by Gorkha Earthquake 2015: A Case of Pharak area, Everest Region, Nepal Buddhi Raj Shrestha1,4*, Narendra Raj Khanal1,4, Joëlle Smadja2,4, Monique Fort3,4 1 Central Department of Geography, Tribhuvan University, Kirtipur, Kathmandu Nepal 2 Centre for Himalayan Studies, UPR 299. CNRS, 7 rue Guy Môquet, 94800 Villejuif, France 3 Université Paris Diderot, GHES, Case 7001, UMR 8586 PRODIG CNRS, Paris Cedex 75013, France 4 ANR-13-SENV-0005-02 PRESHINE (* Corresponding Author: [email protected]) Received: 8 November 2019; Accepted: 22 January 2020; Published: March 2020 Abstract Nepal experienced disastrous earthquake events in 2015. -
Flood Management Strategy for Ganga Basin Through Storage
Flood Management Strategy for Ganga Basin through Storage by N. K. Mathur, N. N. Rai, P. N. Singh Central Water Commission Introduction The Ganga River basin covers the eleven States of India comprising Bihar, Jharkhand, Uttar Pradesh, Uttarakhand, West Bengal, Haryana, Rajasthan, Madhya Pradesh, Chhattisgarh, Himachal Pradesh and Delhi. The occurrence of floods in one part or the other in Ganga River basin is an annual feature during the monsoon period. About 24.2 million hectare flood prone area Present study has been carried out to understand the flood peak formation phenomenon in river Ganga and to estimate the flood storage requirements in the Ganga basin The annual flood peak data of river Ganga and its tributaries at different G&D sites of Central Water Commission has been utilised to identify the contribution of different rivers for flood peak formations in main stem of river Ganga. Drainage area map of river Ganga Important tributaries of River Ganga Southern tributaries Yamuna (347703 sq.km just before Sangam at Allahabad) Chambal (141948 sq.km), Betwa (43770 sq.km), Ken (28706 sq.km), Sind (27930 sq.km), Gambhir (25685 sq.km) Tauns (17523 sq.km) Sone (67330 sq.km) Northern Tributaries Ghaghra (132114 sq.km) Gandak (41554 sq.km) Kosi (92538 sq.km including Bagmati) Total drainage area at Farakka – 931000 sq.km Total drainage area at Patna - 725000 sq.km Total drainage area of Himalayan Ganga and Ramganga just before Sangam– 93989 sq.km River Slope between Patna and Farakka about 1:20,000 Rainfall patten in Ganga basin -
Water Resources of Nepal in the Context of Climate Change
Government of Nepal Water and Energy Commission Secretariat Singha Durbar, Kathmandu, Nepal WATER RESOURCES OF NEPAL IN THE CONTEXT OF CLIMATE CHANGE 2011 Water Resources of Nepal in the Context of Climate Change 2011 © Water and Energy Commission Secretariat (WECS) All rights reserved Extract of this publication may be reproduced in any form for education or non-profi t purposes without special permission, provided the source is acknowledged. No use of this publication may be made for resale or other commercial purposes without the prior written permission of the publisher. Published by: Water and Energy Commission Secretariat (WECS) P.O. Box 1340 Singha Durbar, Kathmandu, Nepal Website: www.wec.gov.np Email: [email protected] Fax: +977-1-4211425 Edited by: Dr. Ravi Sharma Aryal Mr. Gautam Rajkarnikar Water and Energy Commission Secretariat Singha Durbar, Kathmandu, Nepal Front cover picture : Mera Glacier Back cover picture : Tso Rolpa Lake Photo Courtesy : Mr. Om Ratna Bajracharya, Department of Hydrology and Meteorology, Ministry of Environment, Government of Nepal PRINTED WITH SUPPORT FROM WWF NEPAL Design & print : Water Communication, Ph-4460999 Water Resources of Nepal in the Context of Climate Change 2011 Government of Nepal Water and Energy Commission Secretariat Singha Durbar, Kathmandu, Nepal 2011 Water and its availability and quality will be the main pressures on, and issues for, societies and the environment under climate change. “IPCC, 2007” bringing i Acknowledgement Water Resource of Nepal in the Context of Climate Change is an attempt to show impacts of climate change on one of the important sector of life, water resource. Water is considered to be a vehicle to climate change impacts and hence needs to be handled carefully and skillfully. -
1730769411Annual Extreme Precipitation.Pdf
Government of Nepal Ministry of Energy, Water Resource and Irrigation Department of Hydrology and Meteorology Climate Division Babarmahal, Kathmandu Annual Extreme Precipitation The precipitation extremes are usually recorded in Nepal during the monsoon months (June-September) especially in the month of July and August. There are a few cases that the extremes are recorded in other months. In this report, daily extreme precipitation information of major 20 stations shown in map 1 is presented. Among these stations, the highest daily extreme precipitation of 423.1mm was recorded at Birendranagar, Surkhet on 15 August 2014. Trend and its significance of daily extreme precipitation are shown in Table 1 and ever recorded daily extreme precipitation is shown in Table 2. Government of Nepal Ministry of Energy, Water Resource and Irrigation Department of Hydrology and Meteorology Climate Division Babarmahal, Kathmandu Government of Nepal Ministry of Energy, Water Resource and Irrigation Department of Hydrology and Meteorology Climate Division Babarmahal, Kathmandu Government of Nepal Ministry of Energy, Water Resource and Irrigation Department of Hydrology and Meteorology Climate Division Babarmahal, Kathmandu Government of Nepal Ministry of Energy, Water Resource and Irrigation Department of Hydrology and Meteorology Climate Division Babarmahal, Kathmandu Government of Nepal Ministry of Energy, Water Resource and Irrigation Department of Hydrology and Meteorology Climate Division Babarmahal, Kathmandu Government of Nepal Ministry of Energy, -
The Conservation Action Plan the Ganges River Dolphin
THE CONSERVATION ACTION PLAN FOR THE GANGES RIVER DOLPHIN 2010-2020 National Ganga River Basin Authority Ministry of Environment & Forests Government of India Prepared by R. K. Sinha, S. Behera and B. C. Choudhary 2 MINISTER’S FOREWORD I am pleased to introduce the Conservation Action Plan for the Ganges river dolphin (Platanista gangetica gangetica) in the Ganga river basin. The Gangetic Dolphin is one of the last three surviving river dolphin species and we have declared it India's National Aquatic Animal. Its conservation is crucial to the welfare of the Ganga river ecosystem. Just as the Tiger represents the health of the forest and the Snow Leopard represents the health of the mountainous regions, the presence of the Dolphin in a river system signals its good health and biodiversity. This Plan has several important features that will ensure the existence of healthy populations of the Gangetic dolphin in the Ganga river system. First, this action plan proposes a set of detailed surveys to assess the population of the dolphin and the threats it faces. Second, immediate actions for dolphin conservation, such as the creation of protected areas and the restoration of degraded ecosystems, are detailed. Third, community involvement and the mitigation of human-dolphin conflict are proposed as methods that will ensure the long-term survival of the dolphin in the rivers of India. This Action Plan will aid in their conservation and reduce the threats that the Ganges river dolphin faces today. Finally, I would like to thank Dr. R. K. Sinha , Dr. S. K. Behera and Dr. -
Going Nepal Pvt. Ltd Arun Valley with Everest Base Camp Trek, Everest
Going Nepal Pvt. Ltd Arun Valley with Everest Base Camp Trek Arun Valley with Everest Base Camp Trek Best Season: March-April-May and September-October-November Arun Valley with Everest Base Camp Trek, Everest Region Trekking lie in Sagarmatha and Makalu-Barun National Park. It is the most extreme hard and famous trekking to visit the panoramic view of above eight thousand mountains in the world. The Arun valley and Everest base camp provide really superb views of both Mt Everest and Mount Makalu. The trek requires stamina and fitness to fully appreciate the beauty of the region, which provides some outstanding mountain views. Commencing with a flight to Tumlingtar to the East of Everest, the first week is spent trekking through virgin territory into the Solu Khumbu region before a push up on the main Everest trail to Kala Pattar for tremendous close-ups of Everest Nuptse and Lhotse along with many others before a journey back to Lukla and a flight to Kathmandu. An Arun valley trek is still remote but there are available tea house facilities for a small group and it is easy trekking routes up to Lukla follow to the Arun River. It will be trekking on these trails. This trekking is possible to operate in any season. If anyone would like to walk back to Jiri and take a bus to Kathmandu it is also possible or keeps continues to Everest base camp as well. Culturally, the Arun Trek is very interesting - moving from Sherpa through to Rai villages, then down to Chhetri and Brahmin villages. -
2.3 Nepal Road Network
2.3 Nepal Road Network Overview Primary Roads in Nepal Major Road Construction Projects Distance Matrix Road Security Weighbridges and Axle Load Limits Road Class and Surface Conditions Province 1 Province 2 Bagmati Province Gandaki Province Province 5 Karnali Province Sudurpashchim Province Overview Roads are the predominant mode of transport in Nepal. Road network of Nepal is categorized into the strategic road network (SRN), which comprises of highways and feeder roads, and the local road network (LRN), comprising of district roads and Urban roads. Nepal’s road network consists of about 64,500 km of roads. Of these, about 13,500 km belong to the SRN, the core network of national highways and feeder roads connecting district headquarters. (Picture : Nepal Road Standard 2070) The network density is low, at 14 kms per 100 km2 and 0.9 km per 1,000 people. 60% of the road network is concentrated in the lowland (Terai) areas. A Department of Roads (DoR’s) survey shows that 50% of the population of the hill areas still must walk two hours to reach an SRN road. Two of the 77 district headquarters, namely Humla, and Dolpa are yet to be connected to the SRN. Page 1 (Source: Sector Assessment [Summary]: Road Transport) Primary Roads in Nepal S. Rd. Name of Highway Length Node Feature Remarks N. Ref. (km) No. Start Point End Point 1 H01 Mahendra Highway 1027.67 Mechi Bridge, Jhapa Gadda chowki Border, East to West of Country Border Kanchanpur 2 H02 Tribhuvan Highway 159.66 Tribhuvan Statue, Sirsiya Bridge, Birgunj Connects biggest Customs to Capital Tripureshwor Border 3 H03 Arniko Highway 112.83 Maitighar Junction, KTM Friendship Bridge, Connects Chinese border to Capital Kodari Border 4 H04 Prithvi Highway 173.43 Naubise (TRP) Prithvi Chowk, Pokhara Connects Province 3 to Province 4 5 H05 Narayanghat - Mugling 36.16 Pulchowk, Naryanghat Mugling Naryanghat to Mugling Highway (PRM) 6 H06 Dhulikhel Sindhuli 198 Bhittamod border, Dhulikhel (ARM) 135.94 Km. -
Food Insecurity and Undernutrition in Nepal
SMALL AREA ESTIMATION OF FOOD INSECURITY AND UNDERNUTRITION IN NEPAL GOVERNMENT OF NEPAL National Planning Commission Secretariat Central Bureau of Statistics SMALL AREA ESTIMATION OF FOOD INSECURITY AND UNDERNUTRITION IN NEPAL GOVERNMENT OF NEPAL National Planning Commission Secretariat Central Bureau of Statistics Acknowledgements The completion of both this and the earlier feasibility report follows extensive consultation with the National Planning Commission, Central Bureau of Statistics (CBS), World Food Programme (WFP), UNICEF, World Bank, and New ERA, together with members of the Statistics and Evidence for Policy, Planning and Results (SEPPR) working group from the International Development Partners Group (IDPG) and made up of people from Asian Development Bank (ADB), Department for International Development (DFID), United Nations Development Programme (UNDP), UNICEF and United States Agency for International Development (USAID), WFP, and the World Bank. WFP, UNICEF and the World Bank commissioned this research. The statistical analysis has been undertaken by Professor Stephen Haslett, Systemetrics Research Associates and Institute of Fundamental Sciences, Massey University, New Zealand and Associate Prof Geoffrey Jones, Dr. Maris Isidro and Alison Sefton of the Institute of Fundamental Sciences - Statistics, Massey University, New Zealand. We gratefully acknowledge the considerable assistance provided at all stages by the Central Bureau of Statistics. Special thanks to Bikash Bista, Rudra Suwal, Dilli Raj Joshi, Devendra Karanjit, Bed Dhakal, Lok Khatri and Pushpa Raj Paudel. See Appendix E for the full list of people consulted. First published: December 2014 Design and processed by: Print Communication, 4241355 ISBN: 978-9937-3000-976 Suggested citation: Haslett, S., Jones, G., Isidro, M., and Sefton, A. (2014) Small Area Estimation of Food Insecurity and Undernutrition in Nepal, Central Bureau of Statistics, National Planning Commissions Secretariat, World Food Programme, UNICEF and World Bank, Kathmandu, Nepal, December 2014.