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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. -
Diversity of Malacofauna from the Paleru and Moosy Backwaters Of
Journal of Entomology and Zoology Studies 2017; 5(4): 881-887 E-ISSN: 2320-7078 P-ISSN: 2349-6800 JEZS 2017; 5(4): 881-887 Diversity of Malacofauna from the Paleru and © 2017 JEZS Moosy backwaters of Prakasam district, Received: 22-05-2017 Accepted: 23-06-2017 Andhra Pradesh, India Darwin Ch. Department of Zoology and Aquaculture, Acharya Darwin Ch. and P Padmavathi Nagarjuna University Nagarjuna Nagar, Abstract Andhra Pradesh, India Among the various groups represented in the macrobenthic fauna of the Bay of Bengal at Prakasam P Padmavathi district, Andhra Pradesh, India, molluscs were the dominant group. Molluscs were exploited for Department of Zoology and industrial, edible and ornamental purposes and their extensive use has been reported way back from time Aquaculture, Acharya immemorial. Hence the present study was focused to investigate the diversity of Molluscan fauna along Nagarjuna University the Paleru and Moosy backwaters of Prakasam district during 2016-17 as these backwaters are not so far Nagarjuna Nagar, explored for malacofauna. A total of 23 species of molluscs (16 species of gastropods belonging to 12 Andhra Pradesh, India families and 7 species of bivalves representing 5 families) have been reported in the present study. Among these, gastropods such as Umbonium vestiarium, Telescopium telescopium and Pirenella cingulata, and bivalves like Crassostrea madrasensis and Meretrix meretrix are found to be the most dominant species in these backwaters. Keywords: Malacofauna, diversity, gastropods, bivalves, backwaters 1. Introduction Molluscans are the second largest phylum next to Arthropoda with estimates of 80,000- 100,000 described species [1]. These animals are soft bodied and are extremely diversified in shape and colour. -
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. -
The Natural Choice for Wildlife Holidays Welcome
HOLIDAYS WITH 100% FINANCIAL PROTECTION The natural choice for wildlife holidays Welcome After spending considerable time and effort reflecting, questioning what we do and how we do it, and scrutinising the processes within our office and the systems we use for support, I am delighted to say that we are imbued with a new vigour, undiminished enthusiasm, and greater optimism than ever. My own determination to continue building on the solid foundation of twenty years of experience in wildlife tourism, since we started from very humble beginnings – to offer what is simply the finest selection of high quality, good value, tailor-made wildlife holidays – remains undaunted, and is very much at the core of all we do. A physical move to high-tech office premises in the attractive city of Winchester leaves us much better connected to, and more closely integrated with, the outside world, and thus better able to receive visitors. Our team is leaner, tighter, more widely travelled and more knowledgeable than ever before, allowing us to focus on terrestrial, marine and – along with Dive Worldwide – submarine life without distraction. In planning this brochure we deliberately set out to whet the appetite, and make no mention of either dates or prices. As the vast majority of trips are tailored to our clients’ exact requirements – whether in terms of itinerary, duration, standard of accommodation or price – the itineraries herein serve merely as indications of what is possible. Thereafter, you can refine these suggestions in discussion with one of our experienced consultants to pin down your precise needs and wants, so we can together create the wildlife holiday of your dreams. -
Comparative Analysis of Sea Surface Temperature Pattern in the Eastern and Western Gulfs of Arabian Sea and the Red Sea in Recent Past Using Satellite Data
Hindawi Publishing Corporation International Journal of Oceanography Volume 2013, Article ID 501602, 16 pages http://dx.doi.org/10.1155/2013/501602 Research Article Comparative Analysis of Sea Surface Temperature Pattern in the Eastern and Western Gulfs of Arabian Sea and the Red Sea in Recent Past Using Satellite Data Neha Nandkeolyar,1 Mini Raman,2 G. Sandhya Kiran,1 and Ajai2 1 Department of Botany, Faculty of Science, M.S. University, Baroda, Vadodara 390002, India 2 Marine Optics Division, Marine and Planetary Sciences Group, Space Application Centre, Ahmedabad 380015, India Correspondence should be addressed to Neha Nandkeolyar; [email protected] Received 1 January 2013; Revised 15 March 2013; Accepted 7 May 2013 Academic Editor: Swadhin Behera Copyright © 2013 Neha Nandkeolyar et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. With unprecedented rate of development in the countries surrounding the gulfs of the Arabian Sea, there has been a rapid warming of these gulfs. In this regard, using Advanced Very High Resolution Radiometer (AVHRR) data from 1985 to 2009, a climatological study of Sea Surface Temperature (SST) and its inter annual variability in the Persian Gulf (PG), Gulf of Oman (GO), Gulf of Aden (GA), Gulf of Kutch (KTCH), Gulf of Khambhat (KMBT), and Red Sea (RS) was carried out using the normalized SST anomaly index. KTCH, KMBT, and GA pursued the typical Arabian Sea basin bimodal SST pattern, whereas PG, GO, and RS followed unimodal SST curve. -
Program and Abstracts
The Atlantic Geoscience Society (AGS) La Société Géoscientifique de l’Atlantique 45th Colloquium and Annual Meeting Special Sessions: • Special Session: In Memory of Dr. Trevor MacHattie (1974 - 2018) • Paleontology and Sedimentology in Atlantic Canada: In Memory of Dr. Ron Pickerill (1947 – 2018) • Current Research in Carboniferous Geology in the Atlantic Provinces • Minerals, metals, melts, and fluids associated with granitoid rocks: new insights from fundamental studies into the genesis, melt fertility, and ore-forming processes • Earth Science Outreach in the Maritime Provinces • Geohazards: Recent and Historical General Sessions: Current Research in the Atlantic Provinces February 7-9, 2019 Fredericton Inn, Fredericton, New Brunswick PROGRAM WITH ABSTRACTS We gratefully acknowledge sponsorship from the following companies and organizations: Department of Energy and Resource Development Geological Surveys Branch Department of Energy and Mines Department of Energy and Mines Geological Surveys Division Petroleum Resources Division Welcome to the 45th Colloquium and Annual Meeting of the Atlantic Geoscience Society in Fredericton, New Brunswick. This is a familiar place for AGS, having been a host several times over the years. We hope you will find something to interest you and generate discussion with old friends and new. AGS members are clearly pushing the boundaries of geoscience in all its branches! Be sure to take in the science on the posters and the displays from sponsors, and don’t miss the after-banquet jam and open mike on Saturday night. For social media types, please consider sharing updates on Facebook and Twitter (details in the program). We hope you will be able to use the weekend to renew old acquaintances, make new ones, and further the aims of your Atlantic Geoscience Society. -
Perennial and Non-Perennial River- River Originating from Mountains, They Get Water Throughout the Year, That River Consider As Perennial River
Perennial and Non-Perennial river- River originating from mountains, they get water throughout the year, that river consider as Perennial river. on the other hand river originating from plateau region called Non-Perennial river. these river do not have enough water for the whole year. Peninsular river- They have a large seasonal fluctuation in volume as they are solely fed from rainfall. These river flow in valley with steep gradients. the river which end in the Bay of Bengal are called 'East flowing' river, If the river empties into the Arabian sea, it is called ' West flowing' river. Inland drainage river- The river which does not empty itself into any sea, and end with any lake or any other water body is known as Inland Drainage river. Classification Indus River Originated from Bokharchu Glacier , near Mansarover. Rivers in India Total length of about 2897 km, it fall into the Arabian sea. Enter in India through Ladakh, flow only in J&K. Ganga River It flow between the Ladakh range and the Zaskar range at Leh. Brahmaputra River Originates as the Bhagirathi from the Gangotri glacier. Originates from Mansaravar Lake. Alaknanda unites with Bhagirathi at Devprayag, Uttarakhand, henceafter know as Ganga. Total length of about 3848 km. It fall into Bay of Bengal. At Bangladesh, Ganga merge with Brahmaputra, mixture known as Padma river. Enter India in Arunachal Pradesh. most of its course lies outside India. Total length of about 2510 km, It fall into the Bay of Bengal. It flow parallel to the Himalayas in the eastward direction. Originate from the Yamunotri glacier, at the Bandarpoonch peak in Uttarakhand. -
Ecological Studies of Mangroves Species in Gulf of Khambhat, Gujarat
ISSN (E): 2349 – 1183 ISSN (P): 2349 – 9265 3(3): 536–542, 2016 DOI: 10.22271/tpr.2016. v3.i3. 070 Research article Ecological studies of mangroves species in Gulf of Khambhat, Gujarat Vandna Devi and Bhawana Pathak* School of Environment and Sustainable Development, Central University of Gujarat, Gandhinagar, India *Corresponding Author: [email protected] [Accepted: 28 September 2016] Abstract: Mangrove forests are of utmost importance due to their role in preventing extreme weather events like tsunamis and cyclones etc. The present study aimed to observe the mangrove plant diversity and edaphic characteristics from Gulf of Khambhat, Gujarat. Ecological parameters and edaphic characteristics were studied for different sites i.e. Navsari, Surat and Bhavnagar. Avicennia marina was found as dominant species at all study sites. Plant species diversity shows increasing tendency with the decrease in plant density. Important Value Index, Shannon-Weaver diversity index and Simpson index of dominance of the mangrove species across the study area were also determined. The present study provides the baseline data of mangrove species and concludes the need of detail study for mangrove species in Gulf of Khambhat, Gujarat for conservation and management strategies. Keywords: Mangrove plants - Avicennia marina - IVI - Plant density - Conservation. [Cite as: Devi V & Pathak B (2016) Ecological studies of mangroves species in Gulf of Khambhat, Gujarat. Tropical Plant Research 3(3): 536–542] INTRODUCTION Mangrove forest ecosystems are significant for the biodiversity, protection of coastal area from erosion and provision of protected nursery breading areas for marine fauna. Ecological study of any area or habitat helps to understand the inter-relationship of all biotic (plants, microbes, other organisms) and abiotic (temperature, moisture and soil etc.) components of environment. -
9TH CLASS India Size and Location SOCIAL
CPP INDIA SIZE AND LOCATION IX CLASS ` KKP / MYP CENTRE 1. Match the following: State Neighbouring Country A. Uttaranchal i. Myanmar B. Rajasthan ii. Pakistan C. Meghalaya iii. China D. Nagaland iv. Bangladesh (A) A - iv, B - iii, C - ii, D - i (B) A - iii, B - ii, C - iv, D – i (C) A - i, B - iii, C - ii, D – iv (D) A - ii, B - iv, C - i, D – iii 2. A major latitude dividing Indian mainland into two equal halves is (A) Arctic circle (B) Equator (C) Tropic of Capricorn (D) Tropic of Cancer 3. India shares longest international boundary with (A) China (B) Nepal (C) Pakistan (D) Bangladesh 4. Maldive Islands are situated to the south of the (A) Port Blair (B) Ross Island (C) Nicobar Island (D) Lakshadweep Island 5. India is separated from Sri Lanka by (A) Arabian Sea (B) Gulf of Kutchh (C) Indian ocean (D) Palk Strait 6. India's mainland extension lies between: (A) 8° 4 N-37° 6 N latitudes 68° 7 E- 97° 25 E longitude (B) 8° 3 N-38° 5 N latitudes 65° 5 E- 97° 21 E longitude (C) 7° 9 N-37° 5 N latitudes 65° 5 E- 97° 21 E longitude (D) 8° 4 N-37° 6 N latitudes 69° 7 E- 97° 24 E longitude 7. The total number of union territories on Western and Eastern coast are : (A) 2 (B) 3 (C) 1 (D) 7 8. An example of Union Territory is (A) Haryana (B) Punjab (C) Chandigarh (D) Kerala 9. Suez Canal has reduced India's distance from Europe by (A) 6,000 km (B) 7,000 km (C) 8,000 km (D) 9,000 km 10. -
Gujarat State Action Plan on Climate Change
Gujarat SAPCC: Draft Report GUJARAT Solar STATE ACTION PLAN ON CLIMATE CHANGE GOVERNMENT OF GUJARAT CLIMATE CHANGE DEPARTMENT Supported by The Energy and Resources Institute New Delhi & GIZ 2014 1 Gujarat SAPCC: Draft Report Contents Section 1 Introduction .......................................................................................................................... 1 1.0 Introduction to Gujarat State Action Plan on Climate Change ............................................................. 3 1.1 Background ................................................................................................................................. 3 1.2 The State Action Plan on Climate Change .................................................................................... 5 2.0 Gujarat – An Overview ........................................................................................................................ 7 2.1Physiography and Climate ............................................................................................................ 7 2.2 Demography ................................................................................................................................ 8 2.3 Economic Growth and Development ........................................................................................... 9 2.4 Policies and Measures ............................................................................................................... 13 2.5 Institutions and Governance .................................................................................................... -
Review of Maritime Transport 2012
UNITED NATIONS CONFERENCE ON TRADE AND DEVELOPMENT OF MARITIME TRANSPORT 2012 UNITED NATIONS CONFERENCE ON TRADE AND DEVELOPMENT OF MARITIME TRANSPORT 2012 New York and Geneva, 2012 ii REVIEW OF MARITIME TRANSPORT 2012 NOTE The Review of Maritime Transport is a recurrent publication prepared by the UNCTAD secretariat since 1968 with the aim of fostering the transparency of maritime markets and analysing relevant developments. Any factual or editorial corrections that may prove QHFHVVDU\EDVHGRQFRPPHQWVPDGHE\*RYHUQPHQWVZLOOEHUHƅHFWHGLQDFRUULJHQGXPWREHLVVXHGVXEVHTXHQWO\ * * * 6\PEROVRI8QLWHG1DWLRQVGRFXPHQWVDUHFRPSRVHGRIFDSLWDOOHWWHUVFRPELQHGZLWKƄJXUHV8VHRIVXFKDV\PEROLQGLFDWHVD reference to a United Nations document. * * * The designations employed and the presentation of the material in this publication do not imply the expression of any opinion whatsoever on the part of the Secretariat of the United Nations concerning the legal status of any country, territory, city or area, or of its authorities, or concerning the delimitation of its frontiers or boundaries. * * * 0DWHULDOLQWKLVSXEOLFDWLRQPD\EHIUHHO\TXRWHGRUUHSULQWHGEXWDFNQRZOHGJHPHQWLVUHTXHVWHGZLWKUHIHUHQFHWRWKHGRFXPHQW QXPEHU VHHEHORZ $FRS\RIWKHSXEOLFDWLRQFRQWDLQLQJWKHTXRWDWLRQRUUHSULQWVKRXOGEHVHQWWRWKH81&7$'VHFUHWDULDWDWWKH following address: Palais des Nations, CH-1211 Geneva 10, Switzerland. UNCTAD/RMT/2012 UNITED NATIONS PUBLICATION Sales no. E.12.II.D.17 ISBN 978-92-1-112860-4 e-ISBN 978-92-1-055950-8 ISSN 0566-7682 ACKNOWLEDGEMENTS iii ACKNOWLEDGEMENTS The Review of Maritime Transport -
Land Feature Extraction-Identification and Descrimincation Using Geospatial Techniques Case Study Along Sabarmati-Tapi Coastal Belt
Kalpa Publications in Civil Engineering Volume 1, 2017, Pages 248{258 ICRISET2017. International Conference on Re- search and Innovations in Science, Engineering &Technology. Selected papers in Civil Engineering Land Feature Extraction-Identification and Descrimincation Using Geospatial Techniques Case study along Sabarmati-Tapi Coastal belt Modi D S1, S N Bhandari2 and L. B. Zala1 1 Civil Engineering Dept.,BVM Engineering College,V V Nagar, Dist: Anand, Gujarat, India 2 Dept. of Earth and Env. Science (DEES), KSKV (Kutch) University,Kutch, Bhuj, Gujarat, India [email protected], [email protected], [email protected] Abstract The Gulf of Cambay/Khambhat, (GoC), the study area is highly influenced by the tidal currents other than geological and structural set up of the region. In Gulf of Cambay, a large tidal range during high and low tides give rise to strong tidal currents and develops a mechanism of sediment transportation. Interestingly the inverted funnel shape of GoC has large contribution for the sediment deposition in this region. During high tide the tide currents move into the Gulf and encroaches the river mouth whereas during low tide, they move out. This regular phenomena since long period on geological time scale has modified the geomorphological features in this region. Along the major estuaries of Sabarmati, Mahi, Narmada and Tapi, the sediment budget is controlled by seasonal variation and also by tide and ebb phenomena. Using remote sensing images of different time scale and topographical map one can study the changes in geomorphological features. Satellite remote sensing technique has proven to be the paramount tool for studying surficial land features, especially for the inaccessible area or where time variable studies and regional scale studies are carried out.