Global Warming and Its Impacts in Pakistan
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Cyclone Contigency Plan for Karachi City 2008
Cyclone Contingency Plan for Karachi City 2008 National Disaster Management Authority Government of Pakistan July 2008 ii Contents Acronyms………………………………………………………………………………………………………………..iii Executive Summary…………………………………………………………………………………………………....iv General…………………………………………………………………………………………………………………..1 Aim………………………………………………………………………………………………………………………..2 Scope…………………………………………………………………………………………………………………….2 Tropical Cyclone………………………………………………………………………………………..……………….2 Case Studies Major Cyclones………………………..……………………………………… ……………………….3 Historical Perspective – Cyclone Occurrences in Pakistan…...……………………………………….................6 General Information - Karachi ….………………………………………………………………………………….…7 Existing Disaster Response Structure – Karachi………………………. ……………………….…………….……8 Scenarios for Tropical Cyclone Impact in Karachi City ……………………………………………………….…..11 Scenario 1 ……………………………………………………………………………………………….…..11 Scenario 2. ……………………………………………………………………………………………….….13 Response Scenario -1…………………… ……………………………………………………………………….…..14 Planning Assumptions……………………………………………………………………………………....14 Outline Plan……………………………………………………………………………………………….….15 Pre-response Phase…………………………………………………………………………………….… 16 Mid Term Measures……………………………………………………………………..………..16 Long Term Measures…………………...…………………….…………………………..……...20 Response Phase………… ………………………..………………………………………………..………21 Provision of Early Warning……………………. ......……………………………………..……21 Execution……………………….………………………………..………………..……………....22 Health Response……………….. ……………………………………………..………………..24 Coordination Aspects…………………………………………….………………………...………………25 -
Towards Understanding Variability in Droughts in Response to Extreme Climate Conditions Over the Different Agro-Ecological Zones of Pakistan
sustainability Article Towards Understanding Variability in Droughts in Response to Extreme Climate Conditions over the Different Agro-Ecological Zones of Pakistan Adil Dilawar 1,2, Baozhang Chen 1,2,3,4,* , Arfan Arshad 5 , Lifeng Guo 1,2, Muhammad Irfan Ehsan 6, Yawar Hussain 7, Alphonse Kayiranga 1,2, Simon Measho 1,2 , Huifang Zhang 1,2, Fei Wang 1,2, Xiaohong Sun 8 and Mengyu Ge 3,* 1 State Key Laboratory of Resources and Environment Information System, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China; [email protected] (A.D.); [email protected] (L.G.); [email protected] (A.K.); [email protected] (S.M.); [email protected] (H.Z.); [email protected] (F.W.) 2 University of Chinese Academy of Sciences, Beijing 100049, China 3 School of Remote Sensing and Geomatics Engineering, Nanjing University of Information Science and Technology, Nanjing 210044, China 4 Jiangsu Center for Collaborative Innovation in Geographical Information Resources Development and Application, Nanjing 210023, China 5 Department of Irrigation and Drainage, Faculty of Agricultural Engineering, University of Agriculture Faisalabad, Faisalabad 38000, Pakistan; [email protected] 6 Institute of Geology, University of the Punjab, Lahore 54590, Pakistan; [email protected] 7 Department of Geology, University of Liege, 4032 Liege, Belgium; [email protected] Citation: Dilawar, A.; Chen, B.; 8 Key Laboratory of Water and Sediment Sciences, College of Environmental Science and Engineering, Arshad, A.; Guo, L.; Ehsan, M.I.; Ministry of Education, Peking University, Beijing 100871, China; [email protected] Hussain, Y.; Kayiranga, A.; Measho, * Correspondence: [email protected] (B.C.); [email protected] (M.G.); S.; Zhang, H.; Wang, F.; et al. -
Coastal Sea Level Response to the Tropical Cyclonic Forcing in the North
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Ocean Sci. Discuss., 11, 575–611, 2014 Open Access www.ocean-sci-discuss.net/11/575/2014/ Ocean Science doi:10.5194/osd-11-575-2014 Discussions © Author(s) 2014. CC Attribution 3.0 License. This discussion paper is/has been under review for the journal Ocean Science (OS). Please refer to the corresponding final paper in OS if available. Coastal sea level response to the tropical cyclonic forcing in the north Indian Ocean P. Mehra1, S. Mohan1, P. Vethamony1, K. Vijaykumar1, T. M. Balakrishnan Nair2, Y. Agarvadekar1, K. Jyoti1, K. Sudheesh1, R. Luis1, S. Lobo1, and B. Harmalkar1 1CSIR-National Institute of Oceanography (NIO), Goa, India 2Indian National Centre for Ocean Information Services (INCOIS), Hyderabad, Goa, India Received: 13 December 2013 – Accepted: 27 January 2014 – Published: 20 February 2014 Correspondence to: P. Mehra ([email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 575 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract The study examines the observed storm-generated sea-level variation due to deep depression (Event-E1) in the Arabian Sea from 26 November–1 December 2011 and a cyclonic storm “THANE” (Event-E2) over the Bay of Bengal during 25–31 Decem- 5 ber 2011. The sea-level and surface meteorological measurements collected during these extreme events exhibit strong synoptic disturbances leading to storm surge up to 43 cm on the west coast and 29 cm on the east coast of India due to E1 and E2. E1 generated sea level oscillations at the measuring stations on the west coast (Ratnagiri, Verem and Karwar) and east coast (Mandapam and Tuticorin) of India with significant 10 energy bands centered at periods of 92, 43 and 23 min. -
Pakistan: Cyclone Yemyin/Floods; Appeal No
Appeal no. MDRPK001 PAKISTAN: CYCLONE GLIDE no. FF-2007-000082-PAK and TC-2007-000084-PAK YEMYIN/FLOODS 31 July 2007 The Federation’s mission is to improve the lives of vulnerable people by mobilizing the power of humanity. It is the world’s largest humanitarian organization and its millions of volunteers are active in 185 countries. In Brief Operations update no. 06; Period covered: 23 to 30 July 2007; Appeal target: CHF 21.34 million (USD 17.3 million or EUR 12.9 million); Appeal coverage: 29%; Outstanding needs: CHF 15.15 million (USD 12.3 million or EUR 9.1 million) <Click here to go directly to the attached donor response report and here for the version on the website> Appeal history: • Preliminary Appeal launched on 4 July 2007 for CHF 10.38 million (USD 8.5 million or EUR 6.2 million) to assist 14,000 families for six months. • A Revised Emergency Appeal was launched on 17 July 2007 for CHF 21.34 million (USD 17.3 million or EUR 12.9 million) to assist 51,500 families for six months. • Disaster Relief Emergency Funds (DREF) allocated: CHF 250,000 on 2 July 2007. Operational Summary: The Pakistan Red Crescent Society (PRCS) and the Federation continue to assist the most vulnerable floods- affected people in Sindh and Baluchistan provinces. Non-food items have so far been distributed to 2,640 families (18,480 people) while 13,000 food parcels have been distributed by the PRCS/Federation. The PRCS has strategically located six mobile health teams which have now treated approximately 14,000 patients. -
Climate of Pakistan (2012)
Pakistan Meteorological Department 20122012 Snow at Margallas in Jan 2012 Climate of Pakistan (2012) National Drought Monitoring Centre (NDMC) Headquarters Office, Sector H-8/2, Islamabad Tel : + (92-51) 9250598, Fax: + (92-51) 9250368, URL: http://www.pakmet.com.pk, Climate of Pakistan in 2012 Prepared By Ghazala Qaiser (Deputy Director) National Drought Monitoring & Early Warning Centre, Pakistan Meteorological Department, Islamabad S.No. Contents Page No. 1 Temperature 3 2 Rainfall 4 3 Extreme Events 6 4 Other Extreme Events of 2012 8 5 Drought Monitor 15 2 Climate of Pakistan in 2012 Temperature and precipitation are two major elements which determine the climate of any region. Any persistent change in both or one with respect to the long term mean or normal values leads to the climate change of that region. In general, 2012 has witnessed no hazardous events climatically. Highlights of the analysis for the climate of Pakistan in 2012 are listed below. 1. Temperature Average Monthly Temperatures of Pakistan for the year 2012 are compared with Average Monthly Normal Temperatures (1981-2010) in figure 1. Figure 1: Comparison of 2012 mean monthly temperatures with Normal (1981-2010) Pakistan’s monthly mean temperatures of 2012 were above the 1981-2010’s average in July only, while in January, February, March, September, October, November and December were below it. April, Jun, and August temperatures were equal to normal and of May were near normal (Fig. 1). Figure 3: Mean Annual Temperatures (2012) Figure 2: Spatial Distribution of Mean 3 Annual Temperatures of Pakistan for 2012 Difference from Normal (1981-2010) Annual Mean Temperatures (actual) for 2012 remained on higher side in most of the country (Fig. -
Spatio-Temporal Variability of Summer Monsoon Onset Over Pakistan
Asia-Pacific Journal of Atmospheric Sciences Online ISSN 1976-7951 https://doi.org/10.1007/s13143-019-00130-z Print ISSN 1976-7633 ORIGINAL ARTICLE Spatio-Temporal Variability of Summer Monsoon Onset over Pakistan Shaukat Ali1,2 & Bushra Khalid2,3,4 & Rida Sehar Kiani4 & Romaisa Babar4 & Sana Nasir4 & Nadia Rehman1 & Muhammad Adnan1 & Muhammad Arif Goheer1 Received: 5 December 2018 /Revised: 29 April 2019 /Accepted: 2 May 2019 # The Author(s) 2019 Abstract Pakistan receives huge amount of rainfall during summer monsoon season that provides water replenishment for transition periods, helps in maintaining natural and anthropogenic ecosystems, and increased crop productivity. In this changing world, shifts in summer monsoon onset in Pakistan have been observed that seems to affect the society in general. Therefore, it is vital to address these summer monsoon onset shifts to help policy makings and implementation. The study was carried out to analyse the spatio-temporal variability in summer monsoon onset in four objectively defined regions covering all Pakistan. A total of 35 meteorological stations spreading over four regions (i.e., northern, central east, central west, and southern) were taken in to account and shifts in summer monsoon onset have been calculated for the period of 1971–2010. The analysis is based on the observational data of daily precipitation from 20th Jun-20th July for 40 years. The onset for each year and mean onset for each decade has been calculated for all stations. The data was analysed for homogeneity, spatial and temporal variability of monsoon rainfall has been calculated for all four regions, and station wise monsoon onset has been discussed in detail. -
Multiscale Analysis of Three Consecutive Years of Anomalous Flooding in Pakistan
Multiscale analysis of three consecutive years of anomalous flooding in Pakistan By K. L. Rasmussen1+, A. J. Hill*, V. E. Toma#, M. D. Zuluaga+, P. J. Webster#, and R. A. Houze, Jr.+ +Department of Atmospheric Sciences University of Washington Seattle, WA *Atmospheric Science Group Department of Geosciences Texas Tech University Lubbock, TX #School of Earth and Atmospheric Sciences Georgia Institute of Technology Atlanta, GA Submitted to the Quarterly Journal of the Royal Meteorological Society January 2014 Revised April 2014 Revised June 2014 1 Corresponding author: Kristen Lani Rasmussen, Department of Atmospheric Sciences, University of Washington, Box 351640, Seattle, WA 98195 E-mail address: [email protected] ABSTRACT A multiscale investigation into three years of anomalous floods in Pakistan provides insight into their formation, unifying meteorological characteristics, mesoscale storm structures, and predictability. Striking similarities between all three floods existed from planetary and large- scale synoptic conditions down to the mesoscale storm structures, and these patterns were generally well-captured with the ECMWF EPS forecast system. Atmospheric blocking events associated with high geopotential heights and surface temperatures over Eastern Europe were present during all three floods. Quasi-stationary synoptic conditions over the Tibetan plateau allowed for the formation of anomalous easterly midlevel flow across central India into Pakistan that advected deep tropospheric moisture from the Bay of Bengal into Pakistan, enabling flooding in the region. The TRMM Precipitation Radar observations show that the flood- producing storms exhibited climatologically unusual structures during all three floods in Pakistan. These departures from the climatology consisted of westward propagating precipitating systems with embedded wide convective cores, rarely seen in this region, that likely occurred when convection was organized upscale by the easterly midlevel jet across the subcontinent. -
Rainfall Trends in Different Climate Zones of Pakistan Salma, S.1, S
Pakistan Journal of Meteorology Vol. 9, Issue 17: Jul 2012 Rainfall Trends in Different Climate Zones of Pakistan Salma, S.1, S. Rehman1, M. A. Shah2 Abstract In this paper, the study was conducted across the country to assess the rainfall trend in different climate zones of Pakistan over the past three decades. For this purpose dataset comprising 30 years for the period 1976 to 2005 were acquired from 30 meteorological observatories from different parts of the country. The whole data was analyzed through Analysis Of Variations (ANOVA) along Dunnett T3 test. The result has shown a decreasing trend (-1.18mm/decade) all over the country, which may be attributed to the presence of drought period during 1998- 2001. Stations located in different zones of the country mainly from North, North West, West and Coastal areas respectively show overall significant decreasing trend whereas plain areas and South West of the country have been observed with no significant trend. Adverse consequences of the rainfall have already been observed in Pakistan in the form of droughts and super floods which have badly affected human settlements, water management and agriculture sectors. Keywords: Rainfall trend, Climate zones, ANOVA test along Dunnett T3 test. Introduction The issue of climate change has emerged very strongly during the last two decades on global scale in view of its projected implications on the environment of vulnerable states. Steadily rising temperature and its impacts on the cryosphere and rainfall are evident in many regions around the world. There are indications that Pakistan has had its share of the large climatic variations that are known to have taken place in northwest India in the past. -
Disaster Risk Management Plan District Gwadar Government of Balochistan
Disaster Risk Management Plan District Gwadar Government of Balochistan November, 2008 District Disaster Management Authority Gwadar Telephone: 0864-210027 Fax: 0864-211362 Copyright © Provincial Disaster Management Authority, Balochistan Material in this publication may be freely quoted, but acknowledgement is requested. Technical Assistance: National Disaster Management Authority (NDMA) United Nations Development Programme (UNDP) Conceptualized by: Mr. Zubair Murshed Developed by: Mr Shalim Kamran Dost The Plan is available from: a. District Disaster Management Authority DCO Office Gwadar Phone: 0092 864 210027 Fax: 0092 864 211362 b. Provincial Disaster Management Authority Airport Road, Quetta, Balochistan Phone: 0092 81 9201045 Fax: 0092 81 9201720 c. National Disaster Management Authority Prime Minister's Secretariat Islamabad Phone: 0092 51 9222373 Fax 0092 51 9204197 The Plan can also be downloaded from: http//www.ndma.gov.pk Table of Contents Foreword 5 Message by DCO 6 Distribution of Copies 7 Acknowledgments 8 List of Acronyms 9 Section 1: Overview of the District 11 1.1 Geography 11 1.2 Demography 12 1.3 Economy 13 1.4 Shelter 14 1.5 Society 14 1.6 Political and Administrative System 15 Section 2: Disaster Risks in the District 17 2.1 Tehsil Jiwani 19 2.2 Tehsil Pasni 19 2.3 Tehsil Gwadar 19 2.4 Tehsil Ormara 20 2.5 Past Disasters of Gwadar Disasters of the District 20 2.6 Dynamic Pressures 21 2.7 District Capacity to Manage Disasters 22 Section 3: Structure for Disaster Risk Management 23 3.1 Institutional Mechanism for DDRM -
Rainfall Variability and Maize Production Over the Potohar
Pakistan Journal of Meteorology Vol. 8, Issue 15 Rainfall Variability and Maize Production over the Potohar Plateau of Pakistan Khuram Rashid1, Ghulam Rasul1 Abstract Pakistan is an agricultural country, having diverse climate and almost two third area experiences arid type climate. Maize (Zea Mays L.) is the second most important cereal crop after wheat in Pakistan but its yield per unit area is very low. Climatic Variability has direct and adverse impact on the food production and sustainable development especially in rainfed areas. Along the foot-hills of Himalayas, a vast agriculture plain known as Potohar Plateau is isolated. Among climatic factors, the precipitation has great influence on the production of crops. Potohar Plateau is known for its highly variable precipitation characteristics both in terms of frequency and distribution. In this study, it has been found that during vegetative and reproductive stages, as the rainfall increases from 100 mm to 250 mm and 50 mm to 200 mm respectively, the yield has been improved resulting in to maximum production i.e. 2400 Kg/Ha at certain amount of precipitation. Maize is generally planted in July with the onset of the monsoon (rainy season) and it attains maturity as the monsoon recedes from Pakistan in September. After crossing the peak values 300 mm during the growing season, the yield decreases with the increase in rainfall. Planting season is highly risky. If there is persistent rain, it does not provide gap to the soil suitable for seed sowing. On the other hand, if monsoon is delayed then deficient soil moisture fails to sustain the seed germination process. -
Geotechnical Aspects of Recent Extreme Floods in Pakistan; a Case History
Missouri University of Science and Technology Scholars' Mine International Conference on Case Histories in (2013) - Seventh International Conference on Geotechnical Engineering Case Histories in Geotechnical Engineering 03 May 2013, 10:55 am - 11:10 am Geotechnical Aspects of Recent Extreme Floods in Pakistan; A Case History Sarfraz Ali University of Witwatersrand, South Africa Fawad Akram National University of Sciences & Technology, Pakistan Abdul Qudoos Khan University of Witwatersrand, South Africa Misba-Hafsa National University of Sciences & Technology, Pakistan Follow this and additional works at: https://scholarsmine.mst.edu/icchge Part of the Geotechnical Engineering Commons Recommended Citation Ali, Sarfraz; Akram, Fawad; Khan, Abdul Qudoos; and Misba-Hafsa, "Geotechnical Aspects of Recent Extreme Floods in Pakistan; A Case History" (2013). International Conference on Case Histories in Geotechnical Engineering. 1. https://scholarsmine.mst.edu/icchge/7icchge/session17/1 This work is licensed under a Creative Commons Attribution-Noncommercial-No Derivative Works 4.0 License. This Article - Conference proceedings is brought to you for free and open access by Scholars' Mine. It has been accepted for inclusion in International Conference on Case Histories in Geotechnical Engineering by an authorized administrator of Scholars' Mine. This work is protected by U. S. Copyright Law. Unauthorized use including reproduction for redistribution requires the permission of the copyright holder. For more information, please contact [email protected]. -
Annua D Saster Statistical Review
CREDCRED Annua D saster Statistical Review The Numbers and Trends 2007 The Centre for Research on the Epidemiology of Disasters (CRED) is based at the Catholic University of Louvain (UCL), Brussels. CRED promotes research, training and information dissemination on international disasters, with a special focus on public health, epidemiology and socioeconomic factors. It aims to enhance the effectiveness of developing countries’ responses to, and management of, disasters. It works closely with non-governmental and multilateral agencies and universities throughout the world. © 2008 CRED J-M. Scheuren WHO Collaborating Center for Research on the Epidemiology of Disasters School of Public Health O. le Polain de Waroux Catholic University of Louvain 30.94 Clos Chapelle-aux-Champs R. Below 1200 Brussels Belgium D. Guha-Sapir Printed in Belgium CRED S. Ponserre* Annual Disaster Statistical Review The Numbers and Trends 2007 Authors J-M. Scheuren O. le Polain de Waroux R. Below D. Guha-Sapir S. Ponserre* CRED i About the Authors Jean-Michel Scheuren is a MEng Management specialised in environmental and development issues. As a research analyst at CRED, Mr Scheuren primarily works for the EM-DAT project where he is in charge of the analyses of the disaster figures. Olivier le Polain is a medical doctor and a research fellow at CRED. His research interests include the public health consequences of natural disasters. He is one of the researchers involved in the MICRODIS project, and is currently working on several research projects on the health impacts of natural disasters in Asia. Regina Below has been working at the Centre for Research on the Epidemiology of Disasters (CRED) since 20 years.