CMFRI Bulletin 43
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India Situation
70 June 2, 2021 HIGHLIGHTS WHO Situation Update • Indian Immunologicals Limited to initiate production of drug substance for Covaxin (Link) India • National Environmental Engineering Research Institute (NEERI), Nagpur has 2,81,75,044 Confirmed Cases developed a Gargle RT-PCR Method for testing COVID-19 samples (Link) 3,31,895 Total Deaths • Centre issues advisory to States/UTs to encourage work-from-home for nursing mothers (Link) South East Asia Region • Family pension to be given to dependents of those who lost their lives due to 31,922,904 Confirmed Cases COVID under Employees State Insurance Corporation (Link) 408,423 Total Deaths • Union Minister of State, Development of North Eastern Region, requests all government employees 18 years of age to get vaccinated at the earliest (Link) World • National Commission for Protection of Child Rights (NCPCR) asks States/UTS 170,426,245 Confirmed Cases to upload data of children who have lost their parents to COVID-19, on online 3,548,628 Deaths tracking portal “Bal Swaraj” (Link) INDIA SITUATION • There is a decline of 69% in daily cases during last 25 days after reporting the highest number of cases (4,14,188) on 7th May 2021. COVID-19: STATUS ACROSS STATES • In the past week, as compared to previous week, 30 states/UTs have shown a decrease in cases. Higher decline has been reported from Haryana (-63%), Delhi (-61%), Uttar Pradesh (-60%) and Rajasthan (-60%). 70 June 2, 2021 • In Punjab, District authorities have been directed to allow issue of oxygen cylinders to patients who require oxygen -
Lakshadweep Action Plan on Climate Change 2012 2012 333333333333333333333333
Lakshadweep Action Plan on Climate Change 2012 2012 333333333333333333333333 LAKSHADWEEP ACTION PLAN ON CLIMATE CHANGE (LAPCC) UNION TERRITORY OF LAKSHADWEEP i SUPPORTED BY UNDP Lakshadweep Action Plan on Climate Change 2012 LAKSHADWEEP ACTION PLAN ON CLIMATE CHANGE (LAPCC) Department of Environment and Forestry Union Territory of Lakshadweep Supported by UNDP ii Lakshadweep Action Plan on Climate Change 2012 Foreword 2012 Climate Change (LAPCC) iii Lakshadweep Action Plan on Lakshadweep Action Plan on Climate Change 2012 Acknowledgements 2012 Climate Change (LAPCC) iv Lakshadweep Action Plan on Lakshadweep Action Plan on Climate Change 2012 CONTENTS FOREWORD .......................................................................................................................................... III ACKNOWLEDGEMENTS .................................................................................................................... IV EXECUTIVE SUMMARY .................................................................................................................. XIII PART A: CLIMATE PROFILE .............................................................................................................. 1 1 LAKSHADWEEP - AN OVERVIEW ............................................................................................. 2 1.1 Development Issues and Priorities .............................................................................................................................. 3 1.2 Baseline Scenario of Lakshadweep ............................................................................................................................ -
Smart Border Management: Indian Coastal and Maritime Security
Contents Foreword p2/ Preface p3/ Overview p4/ Current initiatives p12/ Challenges and way forward p25/ International examples p28/Sources p32/ Glossary p36/ FICCI Security Department p38 Smart border management: Indian coastal and maritime security September 2017 www.pwc.in Dr Sanjaya Baru Secretary General Foreword 1 FICCI India’s long coastline presents a variety of security challenges including illegal landing of arms and explosives at isolated spots on the coast, infiltration/ex-filtration of anti-national elements, use of the sea and off shore islands for criminal activities, and smuggling of consumer and intermediate goods through sea routes. Absence of physical barriers on the coast and presence of vital industrial and defence installations near the coast also enhance the vulnerability of the coasts to illegal cross-border activities. In addition, the Indian Ocean Region is of strategic importance to India’s security. A substantial part of India’s external trade and energy supplies pass through this region. The security of India’s island territories, in particular, the Andaman and Nicobar Islands, remains an important priority. Drug trafficking, sea-piracy and other clandestine activities such as gun running are emerging as new challenges to security management in the Indian Ocean region. FICCI believes that industry has the technological capability to implement border management solutions. The government could consider exploring integrated solutions provided by industry for strengthening coastal security of the country. The FICCI-PwC report on ‘Smart border management: Indian coastal and maritime security’ highlights the initiatives being taken by the Central and state governments to strengthen coastal security measures in the country. -
CHAP 9 Sri Lanka
79o 00' 79o 30' 80o 00' 80o 30' 81o 00' 81o 30' 82o 00' Kankesanturai Point Pedro A I Karaitivu I. Jana D Peninsula N Kayts Jana SRI LANKA I Palk Strait National capital Ja na Elephant Pass Punkudutivu I. Lag Provincial capital oon Devipattinam Delft I. Town, village Palk Bay Kilinochchi Provincial boundary - Puthukkudiyiruppu Nanthi Kadal Main road Rameswaram Iranaitivu Is. Mullaittivu Secondary road Pamban I. Ferry Vellankulam Dhanushkodi Talaimannar Manjulam Nayaru Lagoon Railroad A da m' Airport s Bridge NORTHERN Nedunkeni 9o 00' Kokkilai Lagoon Mannar I. Mannar Puliyankulam Pulmoddai Madhu Road Bay of Bengal Gulf of Mannar Silavatturai Vavuniya Nilaveli Pankulam Kebitigollewa Trincomalee Horuwupotana r Bay Medawachchiya diya A d o o o 8 30' ru 8 30' v K i A Karaitivu I. ru Hamillewa n a Mutur Y Pomparippu Anuradhapura Kantalai n o NORTH CENTRAL Kalpitiya o g Maragahewa a Kathiraveli L Kal m a Oy a a l a t t Puttalam Kekirawa Habarane u 8o 00' P Galgamuwa 8o 00' NORTH Polonnaruwa Dambula Valachchenai Anamaduwa a y O Mundal Maho a Chenkaladi Lake r u WESTERN d Batticaloa Naula a M uru ed D Ganewatta a EASTERN g n Madura Oya a G Reservoir Chilaw i l Maha Oya o Kurunegala e o 7 30' w 7 30' Matale a Paddiruppu h Kuliyapitiya a CENTRAL M Kehelula Kalmunai Pannala Kandy Mahiyangana Uhana Randenigale ya Amparai a O a Mah Reservoir y Negombo Kegalla O Gal Tirrukkovil Negombo Victoria Falls Reservoir Bibile Senanayake Lagoon Gampaha Samudra Ja-Ela o a Nuwara Badulla o 7 00' ng 7 00' Kelan a Avissawella Eliya Colombo i G Sri Jayewardenepura -
Arabian Sea and the Gulf of Oman by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO
An Atlas of Oceanic Internal Solitary Waves (February 2004) Arabian Sea and the Gulf of Oman by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Arabian Sea and the Gulf of Oman Overview The Arabian Sea is located in the northwest Indian Ocean. It is bounded by India (to the east), Iran (to the north) and the Arabian Peninsula (in the west)(Figure 1). The Gulf of Oman is located in the northwest corner of the Arabian Sea. The continental shelf in the region is widest off the northwest coast of India, which also experiences wind-induced upwelling. [LME, 2004]. The circulation in the Arabian Sea is affected by the Northeast (March-April) and Southwest (September -October) Monsoon seasons [Tomczak et al. 2003]. Figure 1. Bathymetry of Arabian Sea [Smith and Sandwell, 1997]. 501 An Atlas of Oceanic Internal Solitary Waves (February 2004) Arabian Sea and the Gulf of Oman by Global Ocean Associates Prepared for Office of Naval Research – Code 322 PO Observations There has been some scientific study of internal waves in the Arabian Sea and Gulf of Oman through the use of satellite imagery [Zheng et al., 1998; Small and Martin, 2002]. The imagery shows evidence of fine scale internal wave signatures along the continental shelf around the entire region. Table 1 shows the months of the year when internal wave observations have been made. Table 1 - Months when internal waves have been observed in the Arabian Sea and Gulf of Oman (Numbers indicate unique dates in that month when waves have been noted) Jan Feb Mar Apr May Jun Jul Aug Sept Oct Nov Dec 2 552 1251 Small and Martin [2002] reported on internal wave signatures observed in ERS SAR images of the Gulf of Oman. -
Agatti Island, UT of Lakshadweep
Socioeconomic Monitoring for Coastal Managers of South Asia: Field Trials and Baseline Surveys Agatti Island, UT of Lakshadweep Project completion Report: NA10NOS4630055 Project Supervisor : Vineeta Hoon Site Coordinators: Idrees Babu and Noushad Mohammed Agatti team: Amina.K, Abida.FM, Bushra M.I, Busthanudheen P.K, Hajarabeebi MC, Hassan K, Kadeeshoma C.P, Koyamon K.G, Namsir Babu.MS, Noorul Ameen T.K, Mohammed Abdul Raheem D A, Shahnas beegam.k, Shahnas.K.P, Sikandar Hussain, Zakeer Husain, C.K, March 2012 This volume contains the results of the Socioeconomic Assessment and monitoring project supported by IUCN/ NOAA Prepared by: 1. The Centre for Action Research on Environment Science and Society, Chennai 600 094 2. Lakshadweep Marine Research and Conservation Centre, Kavaratti island, U.T of Lakshadweep. Citation: Vineeta Hoon and Idrees Babu, 2012, Socioeconomic Monitoring and Assessment for Coral Reef Management at Agatti Island, UT of Lakshadweep, CARESS/ LMRCC, India Cover Photo: A reef fisherman selling his catch Photo credit: Idrees Babu 2 Table of Contents Executive Summary 7 Acknowledgements 8 Glossary of Native Terms 9 List of Acronyms 10 1. Introduction 11 1.1 Settlement History 11 1.2 Dependence on Marine Resources 13 1.3 Project Goals 15 1.4 Report Chapters 15 2. Methodology of Project Execution 17 2.1 SocMon Workshop 17 2.2 Data Collection 18 2.3 Data Validation 20 3. Site Description and Island Infrastructure 21 3.1 Site description 23 3.2. Community Infrastructure 25 4. Community Level Demographics 29 4.1 Socio cultural status 29 4.2 Land Ownership 29 4.3 Demographic characteristics 30 4.4 Household size 30 4.5. -
It Is Well Known That the Upwelling Along the West Coast of India Is
Results (modifications) It is well known that the upwelling along the west coast of India is influenced by local winds as well as remotely forcing (Yu et al., 1991; McCreary et al., 1993; Shankar and Shetye, 1997; Shankar et al., 2002). A modelling study by Suresh et al. (2016) has shown that winds near Sri Lanka drive 60% of seasonal sea level of Indian west coast where as the contribution from Bay of Bengal wind forcing is only 20%. They also pointed out that sea level signals forced by the winds near Sri Lanka extend westward into the eastern Arabian Sea with more than 50% contribution in the Lakshadweep high/low region. Negative seasonal sea level anomaly and associated thermocline shoaling in the southeastern Arabian Sea (Lakshdweep low region) during the summer monsoon brings nutrients near the surface causes phytoplankton bloom, and thus influences the food chain with a direct impact on the local fisheries (Madhupratap et al., 2001). A recent study by Suresh et al. (2018) showed that during positive IOD events downwelling Kelvin waves induce a positive sea level anomaly and a deep thermocline along the west coast of India very quickly (within days) during fall. Also, the equatorial easterlies force upwelling Kelvin waves that travel through the Bay of Bengal coastal waveguide to the west coast of India very slowly finally resulting in negative sea level anomaly in winter. The sea level anomaly along the west coast thus shifts from positive in fall to negative in winter during positive IOD events. Our results have shown that chlorophyll concentration is low along the south west coast of India during positive IOD years when compared to neutral and negative IOD years (Fig. -
Northern Arabian Sea Circulation-Autonomous Research (Nascar): a Research Initiative Based on Autonomous Sensors
OceTHE OFFICIALa MAGAZINEn ogOF THE OCEANOGRAPHYra SOCIETYphy CITATION Centurioni, L.R., V. Hormann, L.D. Talley, I. Arzeno, L. Beal, M. Caruso, P. Conry, R. Echols, H.J.S. Fernando, S.N. Giddings, A. Gordon, H. Graber, R.R. Harcourt, S.R. Jayne, T.G. Jensen, C.M. Lee, P.F.J. Lermusiaux, P. L’Hegaret, A.J. Lucas, A. Mahadevan, J.L. McClean, G. Pawlak, L. Rainville, S.C. Riser, H. Seo, A.Y. Shcherbina, E. Skyllingstad, J. Sprintall, B. Subrahmanyam, E. Terrill, R.E. Todd, C. Trott, H.N. Ulloa, and H. Wang. 2017. Northern Arabian Sea Circulation-Autonomous Research (NASCar): A research initiative based on autonomous sensors. Oceanography 30(2):74–87, https://doi.org/10.5670/oceanog.2017.224. DOI https://doi.org/10.5670/oceanog.2017.224 COPYRIGHT This article has been published in Oceanography, Volume 30, Number 2, a quarterly journal of The Oceanography Society. Copyright 2017 by The Oceanography Society. All rights reserved. USAGE Permission is granted to copy this article for use in teaching and research. Republication, systematic reproduction, or collective redistribution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The Oceanography Society. Send all correspondence to: [email protected] or The Oceanography Society, PO Box 1931, Rockville, MD 20849-1931, USA. DOWNLOADED FROM HTTP://TOS.ORG/OCEANOGRAPHY SPECIAL ISSUE ON AUTONOMOUS AND LAGRANGIAN PLATFORMS AND SENSORS (ALPS) Northern Arabian Sea Circulation- Autonomous Research (NASCar) A RESEARCH INITIATIVE BASED ON AUTONOMOUS SENSORS By Luca R. Centurioni, Verena Hormann, Lynne D. -
National Institute of Oceanography Goa-India
NATIONAL INSTITUTE OF OCEANOGRAPHY GOA-INDIA 1978 ANNUAL REPORT 14 1978 NATIONAL INSTITUTE OF OCEANOGRAPHY ( Council of Scientific &. Industrial Research ) DONA PAULA - 403 004 GOA, INDIA CONTENTS Page No 1. General Introduction 1 2. Research Activities 2.0 Oceanographic Cruises of R.V. Gaveshani 2 2..1 Physical Oceanography 8 2.2 Chemical Oceanography 15 2.3 Geological Oceanography 22 2.4 Biological Oceanography 26 2.5 Ocean Engineering 36 2.6 Oceanographic Instrumentation 38 2.7 Planning, Publications, Information and Data 41 2.8 Interdisciplinary Task Forces 45 2.9 Sponsored Projects 50 2.10 International Projects 56 3. Technical Services 57 4. Administrative Set-up 4.1 Cruise Planning and Programme Priorities Committee for R.V. Gaveshani 60 4.2 Executive Committee 62 4.3 Scientific Advisory Committee 62 4.4 Budget 64 4.5 Scientific and Technical Staff 64 5. Awards, honours and membership of various committees 73 6. Deputations 76 7. Meetings, exhibitions, seminars, symposia, talks and special lectures 77 8. Colloquia 80 9. Radio talks 82 10. Distinguished visitors 10.1 Visit of the Prime Minister of India 10.2 Visit of the Minister of Shipping and Transport 83 10.3 Visit of other VIP's and Scientists 11. Publications 11.1 Publications of the Institute 87 11.2 Papers published 87 11..3 Popular articles and books published 93 11.4 Reports published 94 1 General Introduction In 1978, emphasis on the utilization of technology available at the Institute by the user community was continued. The Institute's research and development programmes included 23 projects, of which 6 were star- ted during this year. -
Technical Report on Design and Execution of Desalination Plants in Minicoy and Agatti, UT Lakshadweep
Technical Report on Design and Execution of Desalination Plants in Minicoy and Agatti, UT Lakshadweep Sea water desalination is attaining increasing attention of present day policy makers, especially with the growing demands that urbanization, population explosion, irregular rainfall and ground water contamination on the fragile natural resources. ‘Low Temperature Thermal Desalination’ (LTTD) is one process that uses the availability of a temperature gradient between two water bodies, such as the Ocean Thermal Gradient that describes temperature variation across the depth of the oceans, to obtain fresh water. The available thermal gradient between warmer surface water and colder deep seawater is utilized by flash evaporating the warm water at low temperatures and condensing the resultant vapour with cold water. Earth System Science Organization, Ministry of Earth Sciences, Government of India, Through National Institute of Ocean Technology (ESSO-NIOT), India, has successfully demonstrated the 100 m3/day capacity land based desalination plant in the remote islands of Agatti and Minicoy of UT Lakshadweep in 2011 following the initial success of similar capacity plant at Kavaratti island. Temperature (oC) 0 10 20 30 40 0 -50 -100 -150 -200 -250 Depth (m) Depth -300 -350 -400 -450 Fig. 1 Schematic Diagram of LTTD working principle (left) and the Ocean Thermal Gradient in coastal waters (NIO, Goa, 2000) The bathymetry around the islands allows availability of 350-380m water depth within 400- 1000m from the shore, for drawing water at 10-12oC. The temperature gradient of 16oC between the deep sea cold water at 12oC and the warm surface sea water at about 28oC is utilized in the LTTD process as shown Fig. -
Other Processes Regulating Ecosystem Productivity and Fish Production in the Western Indian Ocean Andrew Bakun, Claude Ray, and Salvador Lluch-Cota
CoaStalUpwellinO' and Other Processes Regulating Ecosystem Productivity and Fish Production in the Western Indian Ocean Andrew Bakun, Claude Ray, and Salvador Lluch-Cota Abstract /1 Theseasonal intensity of wind-induced coastal upwelling in the western Indian Ocean is investigated. The upwelling off Northeast Somalia stands out as the dominant upwelling feature in the region, producing by far the strongest seasonal upwelling pulse that exists as a; regular feature in any ocean on our planet. It is surmised that the productive pelagic fish habitat off Southwest India may owe its particularly favorable attributes to coastal trapped wave propagation originating in a region of very strong wind-driven offshore trans port near the southern extremity of the Indian Subcontinent. Effects of relatively mild austral summer upwelling that occurs in certain coastal ecosystems of the southern hemi sphere may be suppressed by the effects of intense onshore transport impacting these areas during the opposite (SW Monsoon) period. An explanation for the extreme paucity of fish landings, as well as for the unusually high production of oceanic (tuna) fisheries relative to coastal fisheries, is sought in the extremely dissipative nature of the physical systems of the region. In this respect, it appears that the Gulf of Aden and some areas within the Mozambique Channel could act as important retention areas and sources of i "see6stock" for maintenance of the function and dillersitv of the lamer reoional biolooical , !I ecosystems. 103 104 large Marine EcosySlIlms ofthe Indian Ocean - . Introduction The western Indian Ocean is the site ofsome of the most dynamically varying-. large marine ecosystems (LMEs) that exist on our planet. -
Arabian Peninsula from Wikipedia, the Free Encyclopedia Jump to Navigationjump to Search "Arabia" and "Arabian" Redirect Here
Arabian Peninsula From Wikipedia, the free encyclopedia Jump to navigationJump to search "Arabia" and "Arabian" redirect here. For other uses, see Arabia (disambiguation) and Arabian (disambiguation). Arabian Peninsula Area 3.2 million km2 (1.25 million mi²) Population 77,983,936 Demonym Arabian Countries Saudi Arabia Yemen Oman United Arab Emirates Kuwait Qatar Bahrain -shibhu l-jazīrati l ِش ْبهُ ا ْل َج ِزي َرةِ ا ْلعَ َربِيَّة :The Arabian Peninsula, or simply Arabia[1] (/əˈreɪbiə/; Arabic jazīratu l-ʿarab, 'Island of the Arabs'),[2] is َج ِزي َرةُ ا ْلعَ َرب ʿarabiyyah, 'Arabian peninsula' or a peninsula of Western Asia situated northeast of Africa on the Arabian plate. From a geographical perspective, it is considered a subcontinent of Asia.[3] It is the largest peninsula in the world, at 3,237,500 km2 (1,250,000 sq mi).[4][5][6][7][8] The peninsula consists of the countries Yemen, Oman, Qatar, Bahrain, Kuwait, Saudi Arabia and the United Arab Emirates.[9] The peninsula formed as a result of the rifting of the Red Sea between 56 and 23 million years ago, and is bordered by the Red Sea to the west and southwest, the Persian Gulf to the northeast, the Levant to the north and the Indian Ocean to the southeast. The peninsula plays a critical geopolitical role in the Arab world due to its vast reserves of oil and natural gas. The most populous cities on the Arabian Peninsula are Riyadh, Dubai, Jeddah, Abu Dhabi, Doha, Kuwait City, Sanaʽa, and Mecca. Before the modern era, it was divided into four distinct regions: Red Sea Coast (Tihamah), Central Plateau (Al-Yamama), Indian Ocean Coast (Hadhramaut) and Persian Gulf Coast (Al-Bahrain).