Morphotectonic Indices of Drainage And
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How Do They Add to the Disaster Potential in Uttarakhand?
South Asia Network on Dams, Rivers and People Uttarakhand: Existing, under construction and proposed Hydropower Projects: How do they add to the disaster potential in Uttarakhand? As Uttarakhand faced unprecedented flood disaster and as the issue of contribution of hydropower projects in this disaster was debated, one question for which there was no clear answer is, how many hydropower projects are there in various river basins of Uttarakhand? How many of them are operating hydropower projects, how many are under construction and how many more are planned? How projects are large (over 25 MW installed capacity), small (1-25 MW) and mini-mirco (less than 1 MW installed capacity) in various basins at various stages. This document tries to give a picture of the status of various hydropower projects in various sub basins in Uttarakhand, giving a break up of projects at various stages. River Basins in Uttarakhand Entire Uttarakhand is Uttarakhand has 98 operating hydropower part of larger Ganga basin. The Ganga River is a projects (all sizes) with combined capacity trans-boundary river of India and Bangladesh. The close to 3600 MW. However, out of this 2,525 km long river rises in the western Himalayas capacity, about 1800 MW is in central sector in the Indian state of Uttarakhand, and flows south and 503 MW in private sector, making it and east through the Gangetic Plain of North India into Bangladesh, where it empties into the Bay of uncertain how much power from these Bengal. The Ganga begins at the confluence of the projects the state will get. -
Climate-Glacier Relationship in the Monsoon-Arid Transition Zone: a Case Study in Himachal Pradesh, India
Climate-Glacier relationship in the monsoon-arid transition zone : A Case study in Himachal Pradesh, India Farooq Azam Mohd To cite this version: Farooq Azam Mohd. Climate-Glacier relationship in the monsoon-arid transition zone : A Case study in Himachal Pradesh, India. Earth Sciences. Université de Grenoble, 2014. English. NNT : 2014GRENU032. tel-01230980 HAL Id: tel-01230980 https://tel.archives-ouvertes.fr/tel-01230980 Submitted on 19 Nov 2015 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. THESIS Submitted to obtain the degree of DOCTOR OF THE UNIVERSITY OF GRENOBLE Speciality : Earth Sciences, Universe and Environment Arrêté ministériel : 1 November 2011 Presented by Mohd Farooq AZAM Thesis directed by Patrick Wagnon and co-directed by Christian Vincent & Ramanathan Alagappan Prepared in the Laboratoire de Glaciologie et de Géophysique de l’Environnement/Laboratoire d'Etudes des Transferts en Hydrologie et Environnement, UJF/CNRS in Doctoral school Earth Sciences, Universe and Environment Climate-Glacier relationship in the monsoon-arid transition zone: A Case study in Himachal Pradesh, India. Defended publicly : 17 December 2014, Before the jury : Mr. Gerhard KRINNER Research Director, CNRS, LGGE (France), President Mr. Martin HOELZLE Professor, University of Fribourg (Switzerland), Reporter Mr. -
Gori River Basin Substate BSAP
A BIODIVERSITY LOG AND STRATEGY INPUT DOCUMENT FOR THE GORI RIVER BASIN WESTERN HIMALAYA ECOREGION DISTRICT PITHORAGARH, UTTARANCHAL A SUB-STATE PROCESS UNDER THE NATIONAL BIODIVERSITY STRATEGY AND ACTION PLAN INDIA BY FOUNDATION FOR ECOLOGICAL SECURITY MUNSIARI, DISTRICT PITHORAGARH, UTTARANCHAL 2003 SUBMITTED TO THE MINISTRY OF ENVIRONMENT AND FORESTS GOVERNMENT OF INDIA NEW DELHI CONTENTS FOREWORD ............................................................................................................ 4 The authoring institution. ........................................................................................................... 4 The scope. .................................................................................................................................. 5 A DESCRIPTION OF THE AREA ............................................................................... 9 The landscape............................................................................................................................. 9 The People ............................................................................................................................... 10 THE BIODIVERSITY OF THE GORI RIVER BASIN. ................................................ 15 A brief description of the biodiversity values. ......................................................................... 15 Habitat and community representation in flora. .......................................................................... 15 Species richness and life-form -
Impact of Climate Change in Kalabaland Glacier from 2000 to 2013 S
The Asian Review of Civil Engineering ISSN: 2249 - 6203 Vol. 3 No. 1, 2014, pp. 8-13 © The Research Publication, www.trp.org.in Impact of Climate Change in Kalabaland Glacier from 2000 to 2013 S. Rahul Singh1 and Renu Dhir2 1Reaserch Scholar, 2Associate Professor, Department of CSE, NIT, Jalandhar - 144 011, Pubjab, India E-mail: [email protected] (Received on 16 March 2014 and accepted on 26 June 2014) Abstract - Glaciers are the coolers of the planet earth and the of the clearest indicators of alterations in regional climate, lifeline of many of the world’s major rivers. They contain since they are governed by changes in accumulation (from about 75% of the Earth’s fresh water and are a source of major snowfall) and ablation (by melting of ice). The difference rivers. The interaction between glaciers and climate represents between accumulation and ablation or the mass balance a particularly sensitive approach. On the global scale, air is crucial to the health of a glacier. GSI (op cit) has given temperature is considered to be the most important factor details about Gangotri, Bandarpunch, Jaundar Bamak, Jhajju reflecting glacier retreat, but this has not been demonstrated Bamak, Tilku, Chipa ,Sara Umga Gangstang, Tingal Goh for tropical glaciers. Mass balance studies of glaciers indicate Panchi nala I , Dokriani, Chaurabari and other glaciers of that the contributions of all mountain glaciers to rising sea Himalaya. Raina and Srivastava (2008) in their ‘Glacial Atlas level during the last century to be 0.2 to 0.4 mm/yr. Global mean temperature has risen by just over 0.60 C over the last of India’ have documented various aspects of the Himalayan century with accelerated warming in the last 10-15 years. -
Lulc Classifications Using Gis and Remote Sensing Techniques in Gori Ganga Watershed of Kumaun Himalaya, Uttarakhand
EPRA International Journal of Agriculture and Rural Economic Research (ARER)- Peer-Reviewed Journal Volume: 9 | Issue: 8| August 2021 | Journal DOI: 10.36713/epra0813| Impact Factor SJIF (2021) : 7.604| ISSN: 2321 - 7847 LULC CLASSIFICATIONS USING GIS AND REMOTE SENSING TECHNIQUES IN GORI GANGA WATERSHED OF KUMAUN HIMALAYA, UTTARAKHAND D. S. Parihar and Deepak Department of Geography, Kumaun University, S.S.J. Campus, Almora, Uttarakhand (India) 263601. ABSTRACT Present research paper is an attempt to classifications of the Land Use Land Cover (LULC) by using supervised classification in the Gori Ganga watershed of Kumaun Himalaya, Uttarakhand (India). Geographical distribution of LULC status of Gori Ganga watershed in 2018 about 26.50% (580.86 km2) area was covered with snow, 3.85% (84.33 km2) area was covered with glacier, 1.93% (42.39 km2) area was covered with barren land, 5.63% (123.31 km2) area was covered with Sand cover area, 10.02% (219.53 km2) area was covered with water body, 50.39% (1104.49 km2) area was covered with vegetation and 1.68% (36.72 km2) area was covered with agriculture area. A brief account of these results it’s discussed in the following paragraphs. KEY WORD: LULC, Gori Ganga Watershed, Kumaun Himalaya, GIS and Remote Sensing 1.0 INTRODUCTION maximum likelihood algorithm of supervised The most commonly terms used are basin, classification was used for pixel clustering. Identified catchment and watershed. In the glossary of three types of LULC were in the study area like geographical terms, a basin is “the whole tract of a vegetation, built-up land and others (Rawat et al., country drained by a river and its tributaries” (Stamp 2013). -
Rupsiyabagar-Khasiyabara Hydroelectric Power Project
CENTREFOR WILDLIFESTUDIES August3,2012 Admln. Ofrice: # {669, 31st Cross, l6th Main, Banashankari 2nd Stage, Dr.P.J. Dilip Kumar, IFS Bengaluru - 560 070, Indla. Chair,Forest Advisory Committee Tel. : +91 80 26715364,Tele Fax : +9'l 80 26715255 DirectorGeneral of Forests WEBSITE : rrvwwwcslndia.org Regd. Oflice: 26-2,Aga Abbas Ali Road (Apt.403) Ministryof Environmentand Forests Bengaluru - 560 042, lndia. ParyavaranBhavan CGOComplex, Lodhi Road NewDelhi-1 10003 Sub:Final Report of thesub-committee of the FACon the Rupsiyabagar Khasiyabarahydroelectric project i n Munsiyari (RKH PP), Uttarakhand. Sir, This reportpertains to the site inspectionthat I had carriedout withAIGF Sri HC Choudhryon April21-22,2012. The site inspection was relatedto the 261 MW Rupsiyabagar-KhasiyabaraHydro-Power Project ("RK HPP" for short)in Pithoragarhdistrict of Uttarakhand,proposed by the NationalThermalPower CorporationLimited (henceforth NTPC). The StateGovernment of Uttarakhand videtheir letter dated 21.12.2009 submitted a proposalto obtainprior approval of CentralGovernment under the Forest(Conservation) Act, 1980 for diversionof 217.522 hectare of forestland for 30 years,in favourof the useragency. The proposalwas examinedby the ForestAdvisory Committee ('FAC", for short)on 25.05.2010and rejected. As you are aware,in responseto a representationfonryarded by the Nodal Officer,Forest (Conservation)Act, 1980 (Government of Uttarakhand)in his letterdated 15.09.2010, requesting the MoEFto re-considerits decision to declineapproval of the CentralGovernment, the ForestAdvisory Committee set- up a sub-committeeto undertakea site inspection. Accordingly,the abovesub-committee of the FAC,headed by me, inspectedthe site identifiedfor constructionof the RK HPP in orderto assessfirst-hand the floraand faunaavailable in and aroundthe forestland proposed for diversion and the ecologicalvalue of the area.The mandatedinspection was carriedon 21stand 22nd April 2012. -
Timber Line Delineations Using NDVI Techniques in the Gori Ganga Watershed of Kumaun Himalaya, Uttarakhand
Quest Journals Journal of Research in Environmental and Earth Sciences Volume 7 ~ Issue 4 (2021) pp: 40-45 ISSN(Online) :2348-2532 www.questjournals.org Research Paper Timber Line Delineations Using NDVI Techniques in the Gori Ganga Watershed of Kumaun Himalaya, Uttarakhand D. S. Parihar Department of Geography, Kumaun University, S.S.J Campus, Almora (Uttarakhand), India-263601 ABSTRACT Present research paper is an attempt to delineations the timber line by using Normalized Difference Vegetation Index (NDVI) in the Gori Ganga watershed, Kumaun Himalaya, Uttarakhand (India). The objective of the present study is delineation of vegetation lines of the Gori Ganga watershed in time space. For the study of detect timber line used of Landsat-5, 8 and Cartosat-1 satellite imageries of three different time periods like Landsat-5 Thematic Mapper (TM) of 1990, Landsat-5 (TM) of 1999 and Landsat-8 Operational Land Imager and Thermal Infrared Sensor (OLI and TIRS) of 2016 and Cartosat-1 of 2008. Geographical distribution of timber line average height reveals that in 1990 was about 3516.11 m (± 369 m) which varies between 1729 m to 4560 m, in 1999 was about 3680.69 m (± 362 m) which varies between 2654 m to 6093 m and in 2016 was about 4060.58 m (± 619 m) which varies between 3125 m to 5185 m. KEY WORDS: NDVI Techniques, Timber line, Remote Sensing and GIS Received 25 April, 2021; Revised: 06 May, 2021; Accepted 08 May, 2021 © The author(s) 2021. Published with open access at www.questjournals.org I. INTRODUCTION Ecosystem provides various forms of services through payment mechanism which contributes surplus money to national income and supports to improve the local livelihoods (Khanal et al., 2014). -
Climate Vulnerability in North Western Himalayas
Climate Vulnerability in North Western Himalayas Mukesh Ray, NeerajDoshi, NishantAlag and R.Sreedhar Environics Trust, 2011 A Contribution to the Ongoing Nation-wide Climate Studies Vulnerability in Various Ecoregions of India, 2011 Indian Network on Ethics and Climate Change (INECC) CONTENTS 1.0 INTRODUCTION 2.0 THE HIMALAYAS - PHYSIOGRAPHIC FEATURES 3.0 VULNERABILITY OF THE NORTH WESTERN HIMALAYAS 4.0 ENVIRONMENTS OF CONCERN 5.0 REDUCING RISKS DUE TO CLIMATE CHANGE 1.0 INTRODUCTION Global warming induced climate change has triggered events such as melting glaciers, rising sea levels and changing weather patterns.This in turn has lead to storms, droughts, flash floods, cloudbursts, change in vegetation. Growing body of scientific evidence has established that this phenomenon is directly linked to unprecedented amount of GHG gases released in the atmosphere largely due to burning of fossil fuels since the beginning of industrialization in last century. The situation is likely to worsenas countries with low industrialization including China and India began to pursue the same path of carbon based economic growth. However, the impact of climate change is not distributed evenly across the world. Mountain eco-systems are more sensitive to the habitat and climate change due to the interaction of tectonic, geomorphic, ecological and climate agents. For instance, temperatures are rising more rapidly in the Himalayas than the global average. Over the last decade the average temperature in Nepal has risen 0.6 degrees, compared with an increase in average temperatures globally of 0.7 degrees over the last hundred years (Gravgaard, 2010). In another Himalayan region, Tibetan Plateau, temperatures have gone up over three times the global average (Schell, 2010). -
Homestay in Kumaon
HomesHomesin taytay Kumaon For enquiries, contact: Kumaon Mandal Vikas Nigam Ltd. Oak Park House, Mallital, Nainital - 263001 (India) Phone No: (05942) 231436, 236936, 235656 Mobile No: +91-8650002520 E-mail: [email protected] (Photo Credit: Vishal Rathod, Thimmarayaswamy Krishnappa, Amit Sah, Dhiraj Singh Garbyal, Rohit Umrao, Vikas Gupta, jassubhai.blogspot.in, Deepak K. Chaturvedi, Ashok Pande, Rushir Shah, Sabine Leder) Kumaon Mandal Vikas Nigam Ltd. omestay tourism is a recently-evolved fast-emerging tourism concept. Our country can be a classical Cultural-heritage and its geographical structure makes Kumaon one of the most suitable destinations for homestay homestay model for the variety of its potentialities -natural grandeur, a plethora of heritages, tourism. In this concept, the environment and culture are both commoditized; market value is created with the Hethno-cultural richness, ingenuous social settings, agreeable hospitality and many more unexplored demand of visitors. This provides financial reward to the local indigenous community for conservation of the reserves that are aspirations for experts of tourism and travellers alike. environment and their culture. Under this approach tourism is considered to be a component of development, giving emphasis to explore ways of expanding positive impacts and reducing negative impacts. Homestay tourism is based on three major features namely service, facility and charm. A Homestay is staying in Home stay tourism is a major player when it comes to the reduction of rural poverty. It integrates all activities of some one's home as a paying guest for short time period. But such guests are provided accommodation and tourism such as trekking, cultural tourism, agro-tourism, health tourism, and eco tourism. -
Tourist Spots Chaukori Chaukori Is Imbued with the Breathtaking Beauty of Pithoragarh District
Tourist Spots Chaukori Chaukori is imbued with the breathtaking beauty of Pithoragarh district. chaukori offers a magnificent view of the Panchchuli peaks and has few rivals for spectacular Himalayan sunrises and sunsets. Visitors to chaukori lesser-known part of Pithoragarh . Tourist in chaukori can enjoy nature at her pristine best. Forests of pine, oak and rhododendron are interspersed with cornfields and orchards. Chaukori holds the promise of an idyllic vacation, and a close communication with nature. Gangolihat The sacred site is famous for the Hatkalika Fair held on the ashtami of Chaitra month at the Kalika temple. Devotees visit the shrine during this time with drums and flags to pay homage to Goddess Kalika Berinag Is a small hilly town. A beautiful temple of Berinag (Nag Devta) is there. Earlier it was also famous for tea gardens. All major peaks of himaliyas can seen. The famous cave of Patal Bhuweshner is also nerby to berinag.. Pithorahgarh Once the bastion of the Chand rulers, Pithoragarh town is littered with temples and forts belonging to that era. The town is set in a valley popularly known as Soar and lies in the centre of four hills Chandak, Dhwaj, Kumdar and Thal Kedar, and stretches in the southern flank to Jhulaghat demarcated by the Kali river adjoining the barren peaks of Nepal Hills. Narayan Ashram The ashram was established by Narayan Swami in 1936, about 136 km north of Pithoragarh and 14 km from Tawaghat. This spiritual cum-socio educational centre is set at an altitude of 2734 metres amidst scenic surroundings. It has a school for local children's and imparts training to local youth. -
Uttarakhand Emergency Assistance Project (UEAP)
Initial Environment Examination Project Number: 47229-001 July 2016 IND: Uttarakhand Emergency Assistance Project (UEAP) Package: Construction of FRP huts in disaster affected district of Kumaon (District Bageshwar) Uttarakhand Submitted by Project implementation Unit –UEAP, Tourism (Kumaon), Nainital This initial environment examination report has been submitted to ADB by Project implementation Unit – UEAP, Tourism (Kumaon), Nainital and is made publicly available in accordance with ADB’s public communications policy (2011). It does not necessarily reflect the views of ADB. This initial environment examination report is a document of the borrower. The views expressed herein do not necessarily represent those of ADB's Board of Directors, Management, or staff, and may be preliminary in nature. In preparing any country program or strategy, financing any project, or by making any designation of or reference to a particular territory or geographic area in this document, the Asian Development Bank does not intend to make any judgments as to the legal or other status of any territory or area. ADB Project Number: 3055-IND April 2016 IND: Uttarakhand Emergency Assistance Project Submitted by Project implementation Unit, UEAP, Kumaon Mandal Vikas Nigam limited, Nainital 1 This report has been submitted to ADB by the Project implementation Unit, UEAP, Kumaon Mandal Vikas Nigam, Nainital and is made publicly available in accordance with ADB’s public communications policy (2011). It does not necessarily reflect the views of ADB. Asian Development Bank 2 Initial Environmental Examination April 2016 INDIA: CONSTRUCTION OF FRP HUTS IN DISASTER AFFECTED DISTRICT OF KUMAON (DISTRICT BAGESHWAR) UTTARAKHAND Prepared by State Disaster Management Authority, Government of India, for the Asian Development Bank. -
Lichen Diversity Assessment of Darma Valley, Pithoragarh, Uttarakhand
G- Journal of Environmental Science and Technology 5(6): 64-68 (2018) ISSN (Online): 2322-0228 (Print): 2322-021X G- Journal of Environmental Science and Technology (An International Peer Reviewed Research Journal) Available online at http://www.gjestenv.com RESEARCH ARTICLE Lichen Diversity Assessment of Darma Valley, Pithoragarh, Uttarakhand Krishna Chandra1* and Yogesh Joshi2 1Department of botany, PG College Ranikhet, Almora– 263645, Uttarakhand, INDIA 2Lichenology Laboratory, Department of Botany, S.S.J. Campus, Kumaun University, Almora– 263601, Uttarakhand, INDIA ARTICLE INFO ABSTRACT Received: 25 May 2018 The Himalaya recognized for its biodiversity owing varied landscape and vegetation, provides Revised: 25 Jun 2018 luxuriant growth of lichens. Various geographical regions were explored for lichens study but till date, many alpine meadows are unexplored condition in this regard. The present study focused on Accepted: 28 Jun 2018 lichen diversity of an alpine / sub temperate regions of Darma valley, Pithoragarh district and providing an inventory of 90 species of lichens belonging 54 genera and 21 families. The Key words: Rhizocarpon distinctum is being reported for the first time as new to Uttarakhand, previously this species was reported from Maharashtra. Alpine - sub temperate, Darma valley, Diversity, Lichens, Uttarakhand 1) INTRODUCTION extends to about 100 km [10], comprises of a total of 12 India, a country known for its huge geographical region and villages in which 07 villages namely Nagling, Baling, Dugtu, climatic variations, having a rich diversity of lichens Dagar, Tidang, Marcha, and Sipu were surveyed for lichen represented by more than 2714 species contributes nearly collection, extending altitude 2870 to 3478 m sal (Table 1) and 13.57% of the total 20,000 species of lichens so far recorded covers approx 21 km.