National Institute of Oceanography Goa-India
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Kutch Basin Forms the North-Western Part of the Western Continental
Basin Introduction :. Kutch basin forms the north-western part of the western continental margin of India and is situated at the southern edge of the Indus shelf at right angles to the southern Indus fossil rift (Zaigham and Mallick, 2000). It is bounded by the Nagar- Parkar fault in the North, Radhanpur-Barmer arch in the east and North Kathiawar fault towards the south. The basin extents between Latitude 22° 30' and 24° 30' N and Longitudes 68° and 72° E covering entire Kutch district and western part of Banaskantha (Santalpur Taluka) districts of Gujarat state. It is an east-west oriented pericratonic embayment opening and deepening towards the sea in the west towards the Arabian Sea. The total area of the basin is about 71,000 sq. km of which onland area is 43,000 sq.km and offshore area is 28,000 sq.km. upto 200 bathymetry. The basin is filled up with 1550 to 2500m of Mesozoic sediments and 550m of Tertiary sediments in onland region and upto 4500m of Tertiary sediments in offshore region (Well GKH-1). The sediment fill thickens from less than 500m in the north to over 4500m in the south and from 200m in the east to over 14,000m in the deep sea region towards western part of the basin indicating a palaeo-slope in the south-west. The western continental shelf of India, with average shelf break at about 200 m depth, is about 300 km wide off Mumbai coast and gradually narrows down to 160 km off Kutch in the north. -
Herein After Termed As Gulf) Occupying an Area of 7300 Km2 Is Biologically One of the Most Productive and Diversified Habitats Along the West Coast of India
6. SUMMARY Gulf of Katchchh (herein after termed as Gulf) occupying an area of 7300 Km2 is biologically one of the most productive and diversified habitats along the west coast of India. The southern shore has numerous Islands and inlets which harbour vast areas of mangroves and coral reefs with living corals. The northern shore with numerous shoals and creeks also sustains large stretches of mangroves. A variety of marine wealth existing in the Gulf includes algae, mangroves, corals, sponges, molluscs, prawns, fishes, reptiles, birds and mammals. Industrial and other developments along the Gulf have accelerated in recent years and many industries make use of the Gulf either directly or indirectly. Hence, it is necessary that the existing and proposed developments are planned in an ecofriendly manner to maintain the high productivity and biodiversity of the Gulf region. In this context, Department of Ocean Development, Government of India is planning a strategy for management of the Gulf adopting the framework of Integrated Coastal and Marine Area Management (ICMAM) which is the most appropriate way to achieve the balance between the environment and development. The work has been awarded to National Institute of Oceanography (NIO), Goa. NIO engaged Vijayalakshmi R. Nair as a Consultant to compile and submit a report on the status of flora and fauna of the Gulf based on secondary data. The objective of this compilation is to (a) evolve baseline for marine flora and fauna of the Gulf based on secondary data (b) establish the prevailing biological characteristics for different segments of the Gulf at macrolevel and (c) assess the present biotic status of the Gulf. -
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 -
Meeting Report-V2.0 V1.0Report
10th OceanSITES Steering Committee Meeting Report-V2.0 V1.0Report 10th OceanSITES Steering Team meeting Date: 03-05 November 2014 Location: Hotel Armação, Porto de Galinhas Beach, Pernambuco, Brazil Authors: Uwe Send (Scripps Institution of Oceanography) Champika Gallage (JCOMMOPS Project Office) Meeting information: http://www.jcomm.info/oceansites2014 1 10th OceanSITES Steering Committee Meeting Report-V2.0 V1.0Report Revision Information Date Prepared by Reviewed by Version 03 Dec 2014 C Gallage U. Send V1.0 01 May 2015 Steering team V2.0 2 10th OceanSITES Steering Committee Meeting Report-V2.0 V1.0Report Table of Contents 10TH OCEANSITES STEERING TEAM MEETING ......................................................................... 1 REVISION INFORMATION ............................................................................................................. 2 TABLE OF CONTENTS ................................................................................................................................3 1. INTRODUCTION ................................................................................................................. 4 2. SCOPE OF THE MEETING................................................................................................. 6 3. OCEANSITES MISSION ..................................................................................................... 7 4. OCEANSITES CHARTER ................................................................................................... 7 5. HOW TO BECOME AN OCEANSITE -
Sr. No. Active Zones
Nashik Municipal Corporation Total Micro Containment Zones 899 Sr. Active Zones 266 No. 1 541, Jadhav Sankul, Satpur, Nashik Active 2 Near Date Dairy, Jadhav Sankul Room no.102 Active 3 Divyasakar, Ramdas Colony, Behind Ramdas Garden, Nashik Active 4 Room No.74, Lane No,3, police Head Quarter, Gangapurroad, Nashik Active 5 Saubhagya Ngr, Vihitgaon, Nashik Road, Nashik Active 6 Bhujar Galli, Devlali gaon, Nashikroad Active 7 Talathi office, Deolaligaon, Nashik Road, Nashik Active 8 Safalya Banglow, Saubhagya ngr, Vihitgaon, Nashik Road Active 9 Bagul Nagar, Vihitgaon, Nashik Road, Nashik Active 10 Jain Colony, Deolaligaon, Nashik Road Active 11 Madhuram Soc., Pethroad, Nashik Active 12 Rutuja Row House, Pawar Colony, Makhmalabad, Nashik Active 13 Yashlaxmi Plaza, Datta Ngr, Nashik Active 14 Sukhdev Appt., Pethroa, Nashik Active 15 Pritrang Soc., Datta Ngar, Nashik Active 16 Pavitray Nivas, Behind Sapna Takies, Badde Ngr, Nashik Active 17 Swapnvastu row house, Shubham Park, Cidco, Nashik Active 18 Bajrang Chowk, Savata Ngr, Cidco, Nashik Active 19 Lokmanya Ngr, Cidco, Nashik Active 20 N-31/A1 Mataji Chowk, Vijay Ngr, Cidco, Nashik Active 21 N-52/B/E-1 Near Ganpati Mandir, Sinhasth Ngr, Cidco, Nashik Active 22 Upendra Ngr, Cidco, Nashik Active 23 Bandavane Ngr, Kamatwada Shivar, Nashik Active 24 Akshay Chowk, Pavan Ngr, Cidco, Nashik Active 25 Behind Sadguru Hotel, Trimurti Chowk, Cidco, Nashik Active 26 Behind Hanuman Mandir, Trimurti Chowk, Cidco, Nashik Active 27 Saibaba Mandir, Shivaji Chowk, Cidco, Nashik Active 28 Nehru Chowk, Savta -
The Geographic, Geological and Oceanographic Setting of the Indus River
16 The Geographic, Geological and Oceanographic Setting of the Indus River Asif Inam1, Peter D. Clift2, Liviu Giosan3, Ali Rashid Tabrez1, Muhammad Tahir4, Muhammad Moazam Rabbani1 and Muhammad Danish1 1National Institute of Oceanography, ST. 47 Clifton Block 1, Karachi, Pakistan 2School of Geosciences, University of Aberdeen, Aberdeen AB24 3UE, UK 3Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA 4Fugro Geodetic Limited, 28-B, KDA Scheme #1, Karachi 75350, Pakistan 16.1 INTRODUCTION glaciers (Tarar, 1982). The Indus, Jhelum and Chenab Rivers are the major sources of water for the Indus Basin The 3000 km long Indus is one of the world’s larger rivers Irrigation System (IBIS). that has exerted a long lasting fascination on scholars Seasonal and annual river fl ows both are highly variable since Alexander the Great’s expedition in the region in (Ahmad, 1993; Asianics, 2000). Annual peak fl ow occurs 325 BC. The discovery of an early advanced civilization between June and late September, during the southwest in the Indus Valley (Meadows and Meadows, 1999 and monsoon. The high fl ows of the summer monsoon are references therein) further increased this interest in the augmented by snowmelt in the north that also conveys a history of the river. Its source lies in Tibet, close to sacred large volume of sediment from the mountains. Mount Kailas and part of its upper course runs through The 970 000 km2 drainage basin of the Indus ranks the India, but its channel and drainage basin are mostly in twelfth largest in the world. Its 30 000 km2 delta ranks Pakiistan. -
Sir Creek: the Origin and Development of the Dispute Between Pakistan and India
IPRI Journal 1 SIR CREEK: THE ORIGIN AND DEVELOPMENT OF THE DISPUTE BETWEEN PAKISTAN AND INDIA Dr Rashid Ahmad Khan∗ ir Creek is one of the eight long-standing bilateral disputes between Pakistan and India that the two countries are trying to resolve under S the ongoing composite dialogue process. It is a dispute over a 96 km (60 miles) long strip of water in the Rann of Kutch marshlands of the River Indus, along the border between the Sindh province of southern part of Pakistan and the state of Rajasthan in India. For the last about 40 years, the two countries have been trying to resolve this row through talks. Although, like other bilateral issues between Pakistan and India, the row over Sir Creek, too, awaits a final solution, this is the only area where the two countries have moved much closer to the resolution of the dispute. Following a meeting between the foreign ministers of Pakistan and India on the sidelines of 14th SAARC Summit in New Delhi, an Indian official announced that the two countries had agreed on a common map of Sir Creek, after the completion of joint survey agreed last year. “W e have one common map of the area, from which we will now work and try and see how far we can take this issue to a resolution, hopefully,” declared the Indian Foreign Secretary Shivshankar Menon after Foreign Minister of Pakistan, Mr. Khurshid Mahmud Kasuri, met his Indian counterpart, Mr. Pranab Mukherji in New Delhi on 2 April 2007.1 W hile discussing the prospects of the resolution of this issue in the light of past negotiations between the two countries, this paper aims to examine the implications of the resolution of this issue for the ongoing peace process between Pakistan and India. -
Chapter 2: Ocean Observations
Chapter 2. Ocean observations 2.1 Observational methods With the rapid advancement in technology, the instruments and methods for measuring oceanic circulation and properties have been quickly evolving. Nevertheless, it is useful to understand what types of instruments have been available at different points in oceanographic development and their resolution, precision, and accuracy. The majority of oceanographic measurements so far have been made from research vessels, with auxiliary measurements from merchant ships and coastal stations. Fig. 2.1 Research vessel. Accuracy: The difference between a result obtained and the true value. Precision: Ability to measure consistently within a given data set (variance in the measurement itself due to instrument noise). Generally the precision of oceanographic measurements is better than the accuracy. 2.1.1 Measurements of depth. Each oceanographic variable, such as temperature (T), salinity (S), density , and current , is a function of space and time, and therefore a function of depth. In order to determine to which depth an instrument has been deployed, we need to measure ``depth''. Depth measurements are often made with the measurements of other properties, such as temperature, salinity and current. Meter wheel. The wire is passed over a meter wheel, which is simply a pulley of known circumference with a counter attached to the pulley to count the number of turns, thus giving the depth the instrument is lowered. This method is accurate when the sea is calm with negligible currents. In reality, research vessels are moving and currents might be strong, and thus the wire is not straight. The real depth is shorter than the distance the wire paid out. -
GK Digest November 2016
GK Digest November 2016 International Affairs Pakistan postpones SAARC summit Pakistan has officially postponed the 19th SAARC Summit to be held in November in Islamabad. Pakistan's decision to postpone the SAARC meet has come in the wake of five South Asian countries, including India, expressing their inability to participate in the summit. India, Bangladesh, Bhutan, Afghanistan and Sri Lanka had already pulled out of the SAARC summit indirectly blaming Pakistan for creating an environment which is not right for the successful holding of the meet. Indo-Sri Lanka Joint Military Exercise Mitra Shakti 2016 begins in Ambepussa, Sri Lanka The fourth edition of the India-Sri Lanka Joint Military Exercise ‘MITRA SHAKTI 2016’ is being conducted at Ambepussa, Sri Lanka from 24 October to 06 November 2016. The Indian Contingent is represented by a platoon from the RAJPUTANA RIFLES Regiment and the Sri Lankan Army will be represented by a platoon from the Sinha Regiment. US & Vietnam navies begin 7th annual NEA in Da Nang The US and Vietnamese navies have begun the 7th annual Naval Engagement Activity NEA, Vietnam 2016 at Tien Sa Port in Da Nang. The exercise will focus on non-combatant events and Code for Unplanned Encounters at Sea and search and rescue scenarios. India home to highest number of poors, Naijria second: World Bank A recent World Bank report said that in the 2013, the highest number of people living below poverty line were in India. It was said in a report titled ‘Poverty and share Prosperity’. The report says,’ India is a country where most number of people are living below the international standard of $1.90 per day. -
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. -
Deep-Sea Drilling in the Northern Indian Ocean: India's Science Plans
DDEEEEPP‐‐SSEEAA DDRRIILLLLIINNGG IINN TTHHEE NNOORRTTHHEERRNN IINNDDIIAANN OOCCEEAANN:: IINNDDIIAA’’SS SSCCIIEENNCCEE PPLLAANNSS National Centre for Antarctic and Ocean Research (Ministry of Earth Sciences) Headland Sada, Vasco da Gama, Goa 403804 2 © NATIONAL CENTRE FOR ANTARCTIC AND OCEAN RESEARCH, 2010 IODP Science Plan Draft Version 1/Jan.2010 3 PREFACE Secretary MoES Message Director, NCAOR Message IODP Science Plan 4 OUTLINED Left intentionally blank IODP Science Plan Draft Version 1/Jan.2010 5 CHAPTER 1: AN OVERVIEW Earth’s evolutionary history through the geologic time has been distinctly recorded in the rocks on its surface as well as at depths. The seafloor sediments and extrusive volcanic rocks represent the most recent snapshot of geological events. Beneath this cover, buried in sedimentary sections and the underlying crust, is a rich history of the waxing and waning of glaciers, the creation and aging of oceanic lithosphere, the evolution and extinction of microorganisms and the building and erosion of continents. The scientific ocean drilling has explored this history in increasing detail for several decades. As a consequence, we have learnt about the complexity of the processes that control crustal formation, earthquake generation, ocean circulation and chemistry, and global climate change. The Ocean Drilling has also elucidated on the deep marine sediments, mid-ocean ridges, hydrothermal circulations and many more significant regimes where microbes thrive and natural resources accumulate. The Integrated Ocean Drilling Program (IODP) began in 2003, envisaged as an ambitious expansion of exploration beneath the oceans. The IODP is an international marine research endeavor that explores Earth's structure and history recorded in oceanic sediments and rocks and monitors sub-sea floor environments.