Compilation on Geography Questions
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Shankar Ias Academy Test 18 - Geography - Full Test - Answer Key
SHANKAR IAS ACADEMY TEST 18 - GEOGRAPHY - FULL TEST - ANSWER KEY 1. Ans (a) Explanation: Soil found in Tropical deciduous forest rich in nutrients. 2. Ans (b) Explanation: Sea breeze is caused due to the heating of land and it occurs in the day time 3. Ans (c) Explanation: • Days are hot, and during the hot season, noon temperatures of over 100°F. are quite frequent. When night falls the clear sky which promotes intense heating during the day also causes rapid radiation in the night. Temperatures drop to well below 50°F. and night frosts are not uncommon at this time of the year. This extreme diurnal range of temperature is another characteristic feature of the Sudan type of climate. • The savanna, particularly in Africa, is the home of wild animals. It is known as the ‘big game country. • The leaf and grass-eating animals include the zebra, antelope, giraffe, deer, gazelle, elephant and okapi. • Many are well camouflaged species and their presence amongst the tall greenish-brown grass cannot be easily detected. The giraffe with such a long neck can locate its enemies a great distance away, while the elephant is so huge and strong that few animals will venture to come near it. It is well equipped will tusks and trunk for defence. • The carnivorous animals like the lion, tiger, leopard, hyaena, panther, jaguar, jackal, lynx and puma have powerful jaws and teeth for attacking other animals. 4. Ans (b) Explanation: Rivers of Tamilnadu • The Thamirabarani River (Porunai) is a perennial river that originates from the famous Agastyarkoodam peak of Pothigai hills of the Western Ghats, above Papanasam in the Ambasamudram taluk. -
Snow Depth on Arctic Sea Ice
1814 JOURNAL OF CLIMATE VOLUME 12 Snow Depth on Arctic Sea Ice STEPHEN G. WARREN,IGNATIUS G. RIGOR, AND NORBERT UNTERSTEINER Department of Atmospheric Sciences, University of Washington, Seattle, Washington VLADIMIR F. R ADIONOV,NIKOLAY N. BRYAZGIN, AND YEVGENIY I. ALEKSANDROV Arctic and Antarctic Research Institute, St. Petersburg, Russia ROGER COLONY International Arctic Research Center, University of Alaska, Fairbanks, Alaska (Manuscript received 5 December 1997, in ®nal form 27 July 1998) ABSTRACT Snow depth and density were measured at Soviet drifting stations on multiyear Arctic sea ice. Measurements were made daily at ®xed stakes at the weather station and once- or thrice-monthly at 10-m intervals on a line beginning about 500 m from the station buildings and extending outward an additional 500 or 1000 m. There were 31 stations, with lifetimes of 1±7 yr. Analyses are performed here for the 37 years 1954±91, during which time at least one station was always reporting. Snow depth at the stakes was sometimes higher than on the lines, and sometimes lower, but no systematic trend of snow depth was detected as a function of distance from the station along the 1000-m lines that would indicate an in¯uence of the station. To determine the seasonal progression of snow depth for each year at each station, priority was given to snow lines if available; otherwise the ®xed stakes were used, with an offset applied if necessary. The ice is mostly free of snow during August. Snow accumulates rapidly in September and October, moderately in November, very slowly in December and January, then moderately again from February to May. -
Comparison of Remote Sensing Extraction Methods for Glacier Firn Line- Considering Urumqi Glacier No.1 As the Experimental Area
E3S Web of Conferences 218, 04024 (2020) https://doi.org/10.1051/e3sconf/202021804024 ISEESE 2020 Comparison of remote sensing extraction methods for glacier firn line- considering Urumqi Glacier No.1 as the experimental area YANJUN ZHAO1, JUN ZHAO1, XIAOYING YUE2and YANQIANG WANG1 1College of Geography and Environmental Science, Northwest Normal University, Lanzhou, China 2State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources/Tien Shan Glaciological Station, Chinese Academy of Sciences, Lanzhou, China Abstract. In mid-latitude glaciers, the altitude of the snowline at the end of the ablating season can be used to indicate the equilibrium line, which can be used as an approximation for it. In this paper, Urumqi Glacier No.1 was selected as the experimental area while Landsat TM/ETM+/OLI images were used to analyze and compare the accuracy as well as applicability of the visual interpretation, Normalized Difference Snow Index, single-band threshold and albedo remote sensing inversion methods for the extraction of the firn lines. The results show that the visual interpretation and the albedo remote sensing inversion methods have strong adaptability, alonger with the high accuracy of the extracted firn line while it is followed by the Normalized Difference Snow Index and the single-band threshold methods. In the year with extremely negative mass balance, the altitude deviation of the firn line extracted by different methods is increased. Except for the years with extremely negative mass balance, the altitude of the firn line at the end of the ablating season has a good indication for the altitude of the balance line. -
Glacier (And Ice Sheet) Mass Balance
Glacier (and ice sheet) Mass Balance The long-term average position of the highest (late summer) firn line ! is termed the Equilibrium Line Altitude (ELA) Firn is old snow How an ice sheet works (roughly): Accumulation zone ablation zone ice land ocean • Net accumulation creates surface slope Why is the NH insolation important for global ice• sheetSurface advance slope causes (Milankovitch ice to flow towards theory)? edges • Accumulation (and mass flow) is balanced by ablation and/or calving Why focus on summertime? Ice sheets are very sensitive to Normal summertime temperatures! • Ice sheet has parabolic shape. • line represents melt zone • small warming increases melt zone (horizontal area) a lot because of shape! Slightly warmer Influence of shape Warmer climate freezing line Normal freezing line ground Furthermore temperature has a powerful influence on melting rate Temperature and Ice Mass Balance Summer Temperature main factor determining ice growth e.g., a warming will Expand ablation area, lengthen melt season, increase the melt rate, and increase proportion of precip falling as rain It may also bring more precip to the region Since ablation rate increases rapidly with increasing temperature – Summer melting controls ice sheet fate* – Orbital timescales - Summer insolation must control ice sheet growth *Not true for Antarctica in near term though, where it ʼs too cold to melt much at surface Temperature and Ice Mass Balance Rule of thumb is that 1C warming causes an additional 1m of melt (see slope of ablation curve at right) -
Snow Cover and Glacier Change Study in Nepalese Himalaya Using Remote Sensing and Geographic Information System
26 A. B. Shrestha & S. P. Joshi August 2009 Snow Cover and Glacier Change Study in Nepalese Himalaya Using Remote Sensing and Geographic Information System Arun Bhakta Shrestha1 and Sharad Prasad Joshi2 1 International Centre for Integrated Mountain Development, Nepal E-mail: [email protected] 2 Water and Energy Commission Secretariat, Nepal ABSTRACT Snow cover and glaciers in the Himalaya play a major role in the generation of stream flow in south Asia. Various studies have suggested that the glaciers in the Himalaya are in general condition of retreat. The snowline is also found to be retreating. While there are relatively more studies on glaciers fluctuation in the Himalaya, studies on snow cover is relatively sparse. In this study, snow cover and glacier fluctuation in the Nepalese Himalaya were studied using remote sensing techniques and geographic information system. The study was carried out in two spatial scales: catchments scale and national scale. In catchments scale two catchments: Langtang and Khumbu were studied. Intermittent medium resolution satellite imageries (Landsat) were used to study the fluctuation in snow cover and glacier area in the two catchments. In the national scale study coarse resolution (MODIS) imageries were used to derive seasonal variations in snow cover. An indication of decreasing trend in snow cover is shown by this study, although this result needs verification with more data. The snowline elevation is in general higher in Khumbu compared to Langtang. In both catchments, snowline elevation are higher in east, south-east, south and south-west aspects. The areas of snow cover in those aspects are also greater. -
World Map Outline Find and Shade: Andes, Alps, Rockies, Himalayas, Caucasus Mountains, East Africa Mountains, Alaska/Yukon Ranges, Sentinel Range, Sudiman Range
World Map Outline Find and shade: Andes, Alps, Rockies, Himalayas, Caucasus Mountains, East Africa Mountains, Alaska/Yukon Ranges, Sentinel Range, Sudiman Range 1 The World’s Highest Peaks 2 Earth Cross-Section 3 Mountain Climates Fact Sheet • How high a mountain is affects what its climate is like. Moving 300 metres up is the same as moving 350 miles towards one of the poles! • Air pressure also changes as one gains altitude. At the top of Mount Everest (8848 m) the pressure is around 310-360 millibars, compared to around 1013 mb at sea level. • As a result of falling air pressure, rising air expands and cools (although, dry air cools faster than moist air because, as the moist air rises, the water vapour condenses – like in clouds – and this gives off some heat). The higher you are the cooler it gets. That is why we often have snow on mountaintops, even along the equator. • Mountains therefore act as a barrier to moisture-laden winds. Air rising to pass over the mountains cools and the water vapour condenses, turning into either clouds, rain, or if it is cold enough, snow. This is why on one side of a mountain you can experience a wet climate, while on the other side of the same mountain you find an arid one. • A large mountain range can affect the weather of the land beyond it. The Himalayas influence the climate of the rest of India by sheltering it from the cold air mass of central Asia. • In high mountains the first snow may fall several weeks earlier than it does in the surrounding area. -
Sgp National Strategy Global Environment Facility (Gef Sgp) in the Republic of Tajikistan (2015-2018)
SGP NATIONAL STRATEGY GLOBAL ENVIRONMENT FACILITY (GEF SGP) IN THE REPUBLIC OF TAJIKISTAN (2015-2018) SGP NATIONAL STRATEGY GLOBAL ENVIRONMENT FACILITY (GEF SGP) IN THE REPUBLIC OF TAJIKISTAN (2015-2018) Country: Tajikistan Funds for the sixth Operational Phase ($) ??? USD a. Funds of the GEF Small Grants Programme ??? USD b. Residual balance (for the fivth Operational Phase): ??? USD c. STAR funds: ??? USD d. Other funds which should be involved: ??? USD (project co –financing ) This strategy serves as a fundamental document for the Small Grants Programme of the Global Environment Facility in Tajikistan (hereinafter - the GEF SGP), determining the thematic and geographical scope of work of the GEF SGP in the country, as well as governing the rules and procedures of programme work. The National Strategy has been developed in accordance with the guidelines and strategic priorities of the GEF on the GEF-VI operational period (2015-2018), as well as the strategic priorities for the environmental preservation in the Republic of Tajikistan and the guidance documents of the GEF SGP for all participating countries. The National Programme Strategy to be reviewed for the next GEF–VII operational period. Table of Contents Acronyms 6 1. General information on the GEF SGP results in the framework of OP5 7 1.1. Brief summary of the GEF SGP Strategy in Tajikistan 9 1.2. Base terms for the GEF SGP in Tajikistan 11 Socio-economic context 11 Geographical context 11 Biodiversity context 13 Protected areas 13 Existing legal terms 13 Institutional context 15 2. Programme niche of the GEF SGP Country Strategy 16 Setting priorities 18 POPs / chemicals 22 Environmental management and economic benefits 25 Geographical and thematic coverage 27 2.1. -
Adivasis of India ASIS of INDIA the ADIV • 98/1 T TIONAL REPOR an MRG INTERNA
Minority Rights Group International R E P O R T The Adivasis of India ASIS OF INDIA THE ADIV • 98/1 T TIONAL REPOR AN MRG INTERNA BY RATNAKER BHENGRA, C.R. BIJOY and SHIMREICHON LUITHUI THE ADIVASIS OF INDIA © Minority Rights Group 1998. Acknowledgements All rights reserved. Minority Rights Group International gratefully acknowl- Material from this publication may be reproduced for teaching or other non- edges the support of the Danish Ministry of Foreign commercial purposes. No part of it may be reproduced in any form for com- Affairs (Danida), Hivos, the Irish Foreign Ministry (Irish mercial purposes without the prior express permission of the copyright holders. Aid) and of all the organizations and individuals who gave For further information please contact MRG. financial and other assistance for this Report. A CIP catalogue record for this publication is available from the British Library. ISBN 1 897693 32 X This Report has been commissioned and is published by ISSN 0305 6252 MRG as a contribution to public understanding of the Published January 1999 issue which forms its subject. The text and views of the Typeset by Texture. authors do not necessarily represent, in every detail and Printed in the UK on bleach-free paper. in all its aspects, the collective view of MRG. THE AUTHORS RATNAKER BHENGRA M. Phil. is an advocate and SHIMREICHON LUITHUI has been an active member consultant engaged in indigenous struggles, particularly of the Naga Peoples’ Movement for Human Rights in Jharkhand. He is convenor of the Jharkhandis Organi- (NPMHR). She has worked on indigenous peoples’ issues sation for Human Rights (JOHAR), Ranchi unit and co- within The Other Media (an organization of grassroots- founder member of the Delhi Domestic Working based mass movements, academics and media of India), Women Forum. -
Agricultural Public Expenditure Review
Public Disclosure Authorized Public Disclosure Authorized Public Disclosure Authorized TAJIKISTAN AGRIFOOD SECTOR AND PUBLIC EXPENDITURE REVIEW Europe and Central Asia Region Public Disclosure Authorized TAJIKISTAN AGRIFOOD SECTOR AND PUBLIC EXPENDITURE REVIEW Europe and Central Asia Region © 2020 The World Bank Group 1818 H Street NW Washington, DC 20433 Telephone: 202-473-1000 Internet: www.worldbank.org All rights reserved This work is a product of the staff of The World Bank. The findings, interpretations, and conclusions expressed in this work do not necessarily reflect the views of the Executive Directors of The World Bank or the governments they represent. The World Bank does not guarantee the accuracy of the data included in this work. The boundaries, colors, denominations, and other information shown on any map in this work do not imply any judgment on the part of The World Bank concerning the legal status of any territory or the endorsement or acceptance of such boundaries. Rights and Permissions The material in this work is subject to copyrighted. Because the World Bank encourages dissemination of its knowledge, this work may be reproduced, in whole or in part, for noncommercial purposes as long as full attribution to this work is given. Attribution Cite the work as follows: World Bank. 2021. “Tajikistan: Agrifood Sector and Public Expenditure Review,” World Bank, Washington, D.C. All queries on rights and licenses, including subsidiary rights, should be addressed to the Office of the Publisher, The World Bank Group, 1818 H -
Mountains of Asia a Regional Inventory
International Centre for Integrated Asia Pacific Mountain Mountain Development Network Mountains of Asia A Regional Inventory Harka Gurung Copyright © 1999 International Centre for Integrated Mountain Development All rights reserved ISBN: 92 9115 936 0 Published by International Centre for Integrated Mountain Development GPO Box 3226 Kathmandu, Nepal Photo Credits Snow in Kabul - Madhukar Rana (top) Transport by mule, Solukhumbu, Nepal - Hilary Lucas (right) Taoist monastry, Sichuan, China - Author (bottom) Banaue terraces, The Philippines - Author (left) The Everest panorama - Hilary Lucas (across cover) All map legends are as per Figure 1 and as below. Mountain Range Mountain Peak River Lake Layout by Sushil Man Joshi Typesetting at ICIMOD Publications' Unit The views and interpretations in this paper are those of the author(s). They are not attributable to the International Centre for Integrated Mountain Development (ICIMOD) and do not imply the expression of any opinion concerning the legal status of any country, territory, city or area of its authorities, or concerning the delimitation of its frontiers or boundaries. Preface ountains have impressed and fascinated men by their majesty and mystery. They also constitute the frontier of human occupancy as the home of ethnic minorities. Of all the Mcontinents, it is Asia that has a profusion of stupendous mountain ranges – including their hill extensions. It would be an immense task to grasp and synthesise such a vast physiographic personality. Thus, what this monograph has attempted to produce is a mere prolegomena towards providing an overview of the regional setting along with physical, cultural, and economic aspects. The text is supplemented with regional maps and photographs produced by the author, and with additional photographs contributed by different individuals working in these regions. -
Status of the Cordillera Vilcanota, Including the Quelccaya Ice Cap, Northern Central Andes, Peru
The Cryosphere, 8, 359–376, 2014 Open Access www.the-cryosphere.net/8/359/2014/ doi:10.5194/tc-8-359-2014 The Cryosphere © Author(s) 2014. CC Attribution 3.0 License. Glacial areas, lake areas, and snow lines from 1975 to 2012: status of the Cordillera Vilcanota, including the Quelccaya Ice Cap, northern central Andes, Peru M. N. Hanshaw and B. Bookhagen Department of Geography, University of California, Santa Barbara, CA, USA Correspondence to: M. N. Hanshaw ([email protected]) Received: 14 December 2012 – Published in The Cryosphere Discuss.: 25 February 2013 Revised: 19 December 2013 – Accepted: 10 January 2014 – Published: 3 March 2014 Abstract. Glaciers in the tropical Andes of southern Peru as glacial regions have decreased, 77 % of lakes connected have received limited attention compared to glaciers in to glacial watersheds have either remained stable or shown other regions (both near and far), yet remain of vital im- a roughly synchronous increase in lake area, while 42 % of portance to agriculture, fresh water, and hydropower sup- lakes not connected to glacial watersheds have declined in plies of downstream communities. Little is known about area (58 % have remained stable). Our new and detailed data recent glacial-area changes and how the glaciers in this on glacial and lake areas over 37 years provide an important region respond to climate changes, and, ultimately, how spatiotemporal assessment of climate variability in this area. these changes will affect lake and water supplies. To rem- These data can be integrated into further studies to analyze edy this, we have used 158 multi-spectral satellite images inter-annual glacial and lake-area changes and assess hydro- spanning almost 4 decades, from 1975 to 2012, to ob- logic dependence and consequences for downstream popula- tain glacial- and lake-area outlines for the understudied tions. -
Elimination of Plasmodium Falciparum Malaria in Tajikistan Anatoly V
Kondrashin et al. Malar J (2017) 16:226 DOI 10.1186/s12936-017-1861-5 Malaria Journal CASE STUDY Open Access Elimination of Plasmodium falciparum malaria in Tajikistan Anatoly V. Kondrashin1*, Azizullo S. Sharipov2, Dilshod S. Kadamov2, Saifuddin S. Karimov2, Elkhan Gasimov3, Alla M. Baranova1, Lola F. Morozova1, Ekaterina V. Stepanova1, Natalia A. Turbabina1, Maria S. Maksimova1 and Evgeny N. Morozov1,4 Abstract Malaria was eliminated in Tajikistan by the beginning of the 1960s. However, sporadic introduced cases of malaria occurred subsequently probably as a result of transmission from infected mosquito Anopheles fying over river the Punj from the border areas of Afghanistan. During the 1970s and 1980s local outbreaks of malaria were reported in the southern districts bordering Afghanistan. The malaria situation dramatically changed during the 1990s follow- ing armed confict and civil unrest in the newly independent Tajikistan, which paralyzed health services including the malaria control activities and a large-scale malaria epidemic occurred with more than 400,000 malaria cases. The malaria epidemic was contained by 1999 as a result of considerable fnancial input from the Government and the international community. Although Plasmodium falciparum constituted only about 5% of total malaria cases, reduc- tion of its incidence was slower than that of Plasmodium vivax. To prevent increase in P. falciparum malaria both in terms of incidence and territory, a P. falciparum elimination programme in the Republic was launched in 200, jointly supported by the Government and the Global Fund for control of AIDS, tuberculosis and malaria. The main activities included the use of pyrethroids for the IRS with determined periodicity, deployment of mosquito nets, impregnated with insecticides, use of larvivorous fshes as a biological larvicide, implementation of small-scale environmental man- agement, and use of personal protection methods by population under malaria risk.