Expansion of the Mangrove Species Rhizophora Mucronata in The
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Fronts in the World Ocean's Large Marine Ecosystems. ICES CM 2007
- 1 - This paper can be freely cited without prior reference to the authors International Council ICES CM 2007/D:21 for the Exploration Theme Session D: Comparative Marine Ecosystem of the Sea (ICES) Structure and Function: Descriptors and Characteristics Fronts in the World Ocean’s Large Marine Ecosystems Igor M. Belkin and Peter C. Cornillon Abstract. Oceanic fronts shape marine ecosystems; therefore front mapping and characterization is one of the most important aspects of physical oceanography. Here we report on the first effort to map and describe all major fronts in the World Ocean’s Large Marine Ecosystems (LMEs). Apart from a geographical review, these fronts are classified according to their origin and physical mechanisms that maintain them. This first-ever zero-order pattern of the LME fronts is based on a unique global frontal data base assembled at the University of Rhode Island. Thermal fronts were automatically derived from 12 years (1985-1996) of twice-daily satellite 9-km resolution global AVHRR SST fields with the Cayula-Cornillon front detection algorithm. These frontal maps serve as guidance in using hydrographic data to explore subsurface thermohaline fronts, whose surface thermal signatures have been mapped from space. Our most recent study of chlorophyll fronts in the Northwest Atlantic from high-resolution 1-km data (Belkin and O’Reilly, 2007) revealed a close spatial association between chlorophyll fronts and SST fronts, suggesting causative links between these two types of fronts. Keywords: Fronts; Large Marine Ecosystems; World Ocean; sea surface temperature. Igor M. Belkin: Graduate School of Oceanography, University of Rhode Island, 215 South Ferry Road, Narragansett, Rhode Island 02882, USA [tel.: +1 401 874 6533, fax: +1 874 6728, email: [email protected]]. -
Basin-Wide Seasonal Evolution of the Indian Ocean's Phytoplankton Blooms
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 112, C12014, doi:10.1029/2007JC004090, 2007 Click Here for Full Article Basin-wide seasonal evolution of the Indian Ocean’s phytoplankton blooms M. Le´vy,1,2 D. Shankar,2 J.-M. Andre´,1,2 S. S. C. Shenoi,2 F. Durand,2,3 and C. de Boyer Monte´gut4 Received 5 January 2007; revised 2 August 2007; accepted 5 September 2007; published 21 December 2007. [1] A climatology of Sea-viewing Wide Field-of-View Sensor (SeaWiFS) chlorophyll data over the Indian Ocean is used to examine the bloom variability patterns, identifying spatio-temporal contrasts in bloom appearance and intensity and relating them to the variability of the physical environment. The near-surface ocean dynamics is assessed using an ocean general circulation model (OGCM). It is found that over a large part of the basin, the seasonal cycle of phytoplankton is characterized by two consecutive blooms, one during the summer monsoon, and the other during the winter monsoon. Each bloom is described by means of two parameters, the timing of the bloom onset and the cumulated increase in chlorophyll during the bloom. This yields a regional image of the influence of the two monsoons on phytoplankton, with distinct regions emerging in summer and in winter. By comparing the bloom patterns with dynamical features derived from the OGCM (horizontal and vertical velocities and mixed-layer depth), it is shown that the regional structure of the blooms is intimately linked with the horizontal and vertical circulations forced by the monsoons. Moreover, this comparison permits the assessment of some of the physical mechanisms that drive the bloom patterns, and points out the regions where these mechanisms need to be further investigated. -
Deep‐Water Dunes on Drowned Isolated Carbonate Terraces
1 Sedimentology Article In Press Archimer https://archimer.ifremer.fr Acceptation date : 2018 https://doi.org/10.1111/sed.12572 https://archimer.ifremer.fr/doc/00472/58418/ Deep-water dunes on drowned isolated carbonate terraces (Mozambique Channel, south-west Indian Ocean) Miramontes Elda 1, *, Jorry Stephan 2, Jouet Gwenael 2, Counts John 3, Courgeon Simon 4, Roy Philippe 1, Guerin Charline 2, Hernández-Molina F. Javier 5 1 UMR6538; CNRS-UBO; IUEM; Laboratoire Géosciences Océan; 29280 Plouzané, France 2 IFREMER; Géosciences Marines; 29280 Plouzané ,France 3 School of Earth Sciences; University College Dublin; Belfield, Dublin 4 ,Ireland 4 University of Geneva; Department of Earth Sciences; 1205 Geneva, Switzerland 5 Department of Earth Sciences; Royal Holloway; University of London; Egham Surrey TW20 0EX, United Kingdom * Corresponding author : Elda Miramontes, email address : [email protected] Abstract : Subaqueous sand dunes are common bedforms on continental shelves dominated by tidal and geostrophic currents. However, much less is known about sand dunes in deep‐marine settings that are affected by strong bottom currents. In this study, dune fields were identified on drowned isolated carbonate platforms in the Mozambique Channel (south‐west Indian Ocean). The acquired data include multibeam bathymetry, multi‐channel high‐resolution seismic reflection data, sea floor imagery, a sediment sample and current measurements from a moored current meter and hull‐mounted acoustic Doppler current profiler. The dunes are located at water depths ranging from 200 to 600 m on the slope terraces of a modern atoll (Bassas da India Atoll) and within small depressions formed during tectonic deformation of drowned carbonate platforms (Sakalaves Seamount and Jaguar Bank). -
Mozambique Weekly Report Is Currently Being Distributed to Over 30 Embassies, 45 Non-Governmental Organisations and 677 Businesses and Individuals in Mozambique
WEEKLY MEDIA REVIEW: 22 JANUARY TO 29 JANUARY 2016 www.rhula.net Managing Editor: Nigel Morgan Mozambique’s LNG projects are located in a remote area and could be a target for attackers (see page 45 for more). Rhula Intelligent Solutions is a Private Risk Management Company servicing multinational companies, non-governmental organisations and private clients operating in Mozambique. The Rhula Mozambique Weekly Report is currently being distributed to over 30 embassies, 45 non-governmental organisations and 677 businesses and individuals in Mozambique. For additional information or services please contact: Joe van der Walt David Barske Operations Director Operational Coordinator Mobile (SA): +27 79 516 8710 Mobile (SA): +27 76 691 8934 Mobile (Moz): +258 826 780 038 Mobile (Moz): +258 84 689 5140 Email: [email protected] Email: [email protected] Disclaimer: The information contained in this report is intended to provide general information on a particular subject or subjects. While all reasonable steps are taken to ensure the accuracy and the integrity of information and date transmitted electronically and to preserve the confidentiality thereof, no liability or responsibility whatsoever is accepted by us should information or date for whatever reason or cause be corrupted or fail to reach its intended destination. It is not an exhaustive document on such subject(s), nor does it create a business or professional services relationship. The information contained herein is not intended to constitute professional advice or services. The material discussed is meant to provide general information, and should not be acted on without obtaining professional advice appropriately tailored to your individual needs. -
Mozambique Channel, South-West Indian Ocean) E
Deep-water dunes on drowned isolated carbonate terraces (Mozambique Channel, south-west Indian Ocean) E. Miramontes, S.J. Jorry, G. Jouet, J.W. Counts, S. Courgeon, P. Le Roy, C. Guerin, F.J. Hernández-Molina To cite this version: E. Miramontes, S.J. Jorry, G. Jouet, J.W. Counts, S. Courgeon, et al.. Deep-water dunes on drowned isolated carbonate terraces (Mozambique Channel, south-west Indian Ocean). Sedimentology, 2019, 66 (4), pp.1222-1242. 10.1111/sed.12572. hal-02944583 HAL Id: hal-02944583 https://hal.archives-ouvertes.fr/hal-02944583 Submitted on 12 Apr 2021 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. 1 Sedimentology Article In Press Archimer https://archimer.ifremer.fr Acceptation date : 2018 https://doi.org/10.1111/sed.12572 https://archimer.ifremer.fr/doc/00472/58418/ Deep-water dunes on drowned isolated carbonate terraces (Mozambique Channel, south-west Indian Ocean) Miramontes Elda 1, *, Jorry Stephan 2, Jouet Gwenael 2, Counts John 3, Courgeon Simon 4, Roy Philippe 1, Guerin Charline 2, Hernández-Molina F. Javier 5 1 UMR6538; CNRS-UBO; -
Cowry Shell Money and Monsoon Trade: the Maldives in Past Globalizations
Cowry Shell Money and Monsoon Trade: The Maldives in Past Globalizations Mirani Litster Thesis submitted for the degree of Doctor of Philosophy The Australian National University 2016 To the best of my knowledge the research presented in this thesis is my own except where the work of others has been acknowledged. This thesis has not previously been submitted in any form for any other degree at this or any other university. Mirani Litster -CONTENTS- Contents Abstract xv Acknowledgements xvi Chapter One — Introduction and Scope 1 1.1 Introduction 1 1.2 An Early Global Commodity: Cowry Shell Money 4 1.2.1 Extraction in the Maldives 6 1.2.2 China 8 1.2.3 India 9 1.2.4 Mainland Southeast Asia 9 1.2.5 West and East Africa 10 1.3 Previous Perspectives and Frameworks: The Indian Ocean 11 and Early Globalization 1.4 Research Aims 13 1.5 Research Background and Methodology 15 1.6 Thesis Structure 16 Chapter Two — Past Globalizations: Defining Concepts and 18 Theories 2.1 Introduction 18 2.2 Defining Globalization 19 2.3 Theories of Globalization 21 2.3.1 World Systems Theory 21 2.3.2 Theories of Global Capitalism 24 2.3.3 The Network Society 25 2.3.4 Transnationality and Transnationalism 26 2.3.5 Cultural Theories of Globalization 26 2.4 Past Globalizations and Archaeology 27 2.4.1 Globalization in the Past: Varied Approaches 28 i -CONTENTS- 2.4.2 Identifying Past Globalizations in the Archaeological 30 Record 2.5 Summary 32 Chapter Three — Periods of Indian Ocean Interaction 33 3.1 Introduction 33 3.2 Defining the Physical Parameters 34 3.2.1 -
Global Ocean Surface Velocities from Drifters: Mean, Variance, El Nino–Southern~ Oscillation Response, and Seasonal Cycle Rick Lumpkin1 and Gregory C
JOURNAL OF GEOPHYSICAL RESEARCH: OCEANS, VOL. 118, 2992–3006, doi:10.1002/jgrc.20210, 2013 Global ocean surface velocities from drifters: Mean, variance, El Nino–Southern~ Oscillation response, and seasonal cycle Rick Lumpkin1 and Gregory C. Johnson2 Received 24 September 2012; revised 18 April 2013; accepted 19 April 2013; published 14 June 2013. [1] Global near-surface currents are calculated from satellite-tracked drogued drifter velocities on a 0.5 Â 0.5 latitude-longitude grid using a new methodology. Data used at each grid point lie within a centered bin of set area with a shape defined by the variance ellipse of current fluctuations within that bin. The time-mean current, its annual harmonic, semiannual harmonic, correlation with the Southern Oscillation Index (SOI), spatial gradients, and residuals are estimated along with formal error bars for each component. The time-mean field resolves the major surface current systems of the world. The magnitude of the variance reveals enhanced eddy kinetic energy in the western boundary current systems, in equatorial regions, and along the Antarctic Circumpolar Current, as well as three large ‘‘eddy deserts,’’ two in the Pacific and one in the Atlantic. The SOI component is largest in the western and central tropical Pacific, but can also be seen in the Indian Ocean. Seasonal variations reveal details such as the gyre-scale shifts in the convergence centers of the subtropical gyres, and the seasonal evolution of tropical currents and eddies in the western tropical Pacific Ocean. The results of this study are available as a monthly climatology. Citation: Lumpkin, R., and G. -
Circulation, Renewal, and Modification of Antarctic Mode And
APRIL 2001 SLOYAN AND RINTOUL 1005 Circulation, Renewal, and Modi®cation of Antarctic Mode and Intermediate Water* BERNADETTE M. SLOYAN1 Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany STEPHEN R. RINTOUL Antarctic CRC, University of Tasmania, and CSIRO Division of Marine Research, Hobart, Australia (Manuscript received 18 October 1999, in ®nal form 10 July 2000) ABSTRACT Nine hydrographic sections are combined in an inverse box model of the Southern Ocean south of ;128S. The inverse model has two novel features: the inclusion of independent diapycnal ¯ux unknowns for each property and the explicit inclusion of air±sea ¯uxes (heat, freshwater, and momentum) and the water mass transformation they drive. Transformation of 34 3 106 m3 s21 of Antarctic Surface Water by air±sea buoyancy ¯uxes, and cooling and freshening where Subantarctic Mode Water outcrops, renews cold, fresh Antarctic Intermediate Water of the southeast Paci®c and southwest Atlantic. Relatively cold, fresh mode and intermediate water enter the subtropical gyres, are modi®ed by air±sea ¯uxes and interior mixing, and return poleward as warmer, saltier mode and intermediate water. While the zonally integrated meridional transport in these layers is small, the gross exchange is approximately 80 3 106 m3 s21. The air±sea transformation of Antarctic surface water to intermediate water is compensated in the Southern Ocean by an interior diapycnal ¯ux of 32 3 106 m3 s21 of intermediate water to upper deep water. The small property differences between slightly warmer, saltier intermediate water and cold, fresh Antarctic Surface Water results in a poleward transfer of heat and salt across the Polar Front zone. -
Physical and Biogeochemical Processes Associated with Upwelling in the Indian Ocean Puthenveettil Narayan
https://doi.org/10.5194/bg-2020-486 Preprint. Discussion started: 9 February 2021 c Author(s) 2021. CC BY 4.0 License. 1 Reviews and syntheses: Physical and biogeochemical processes associated with upwelling in the 2 Indian Ocean 1* 2 3 4 3 Puthenveettil Narayana Menon Vinayachandran , Yukio Masumoto , Mike Roberts , Jenny Hugget , 5 6 7 8 9 4 Issufo Halo , Abhisek Chatterjee , Prakash Amol , Garuda V. M. Gupta , Arvind Singh , Arnab 10 6 11 12 13 5 Mukherjee , Satya Prakash , Lynnath E. Beckley , Eric Jorden Raes , Raleigh Hood 6 7 1Centre for Atmospheric and Oceanic Sciences, Indian Institute of Science, Bengaluru, 560012, India 8 9 2 Graduate School of Science, University of Tokyo, Tokyo, Japan 10 11 3 Nelson Mandela University, Port Elizabeth, South Africa 12 13 4Oceans and Coasts Research, Department of Environment, Forestry and Fisheries, Private Bag X4390, Cape Town 8000, 14 South Africa 15 16 5Department of Conservation and Marine Sciences, Cape Peninsula University of Technology, PO Box 652, Cape Town 17 8000, South Africa 18 6Indian National Centre for Indian Ocean Services, Ministry of Earth Sciences, Hyderabad, India 19 20 7CSIR-National Institute of Oceanography, Regional Centre, Visakhapatnam, 530017, India 21 22 8Centre for Marine Living Resources and Ecology, Ministry of Earth Sciences, Kochi, India 23 24 9Physical Research Laboratory, Ahmedabad, 380009, India 25 26 10 National Centre for Polar and Ocean Research, Ministry of Earth Sciences, Goa, India 27 28 11 Environmental and Conservation Sciences, Murdoch University, Perth, Western Australia 6150, Australia 29 30 12 CSIRO Oceans and Atmosphere, GPO Box 1538, Hobart, TAS, 7001 Australia 31 32 13 University of Maryland Center for Environmental Science, Cambridge, MD, USA 33 34 *Correspondence to: P. -
Chapter 11 the Indian Ocean We Now Turn to the Indian Ocean, Which Is
Chapter 11 The Indian Ocean We now turn to the Indian Ocean, which is in several respects very different from the Pacific Ocean. The most striking difference is the seasonal reversal of the monsoon winds and its effects on the ocean currents in the northern hemisphere. The abs ence of a temperate and polar region north of the equator is another peculiarity with far-reaching consequences for the circulation and hydrology. None of the leading oceanographic research nations shares its coastlines with the Indian Ocean. Few research vessels entered it, fewer still spent much time in it. The Indian Ocean is the only ocean where due to lack of data the truly magnificent textbook of Sverdrup et al. (1942) missed a major water mass - the Australasian Mediterranean Water - completely. The situation did not change until only thirty years ago, when over 40 research vessels from 25 nations participated in the International Indian Ocean Expedition (IIOE) during 1962 - 1965. Its data were compiled and interpreted in an atlas (Wyrtki, 1971, reprinted 1988) which remains the major reference for Indian Ocean research. Nevertheless, important ideas did not exist or were not clearly expressed when the atlas was prepared, and the hydrography of the Indian Ocean still requires much study before a clear picture will emerge. Long-term current meter moorings were not deployed until two decades ago, notably during the INDEX campaign of 1976 - 1979; until then, the study of Indian Ocean dynamics was restricted to the analysis of ship drift data and did not reach below the surface layer. Bottom topography The Indian Ocean is the smallest of all oceans (including the Southern Ocean). -
In Situ Measured Current Structures of the Eddy Field in the Mozambique Channel
See discussions, stats, and author profiles for this publication at: https://www.researchgate.net/publication/259138771 In situ measured current structures of the eddy field in the Mozambique Channel Article in Deep Sea Research Part II Topical Studies in Oceanography · January 2013 DOI: 10.1016/j.dsr2.2013.10.013 CITATIONS READS 19 53 5 authors, including: Jean-François Ternon Michael Roberts Institute of Research for Development Nelson Mandela Metropolitan University 31 PUBLICATIONS 557 CITATIONS 74 PUBLICATIONS 1,312 CITATIONS SEE PROFILE SEE PROFILE L. Hancke B. C. Backeberg 4 PUBLICATIONS 99 CITATIONS Council for Scientific and Industrial Research… 25 PUBLICATIONS 203 CITATIONS SEE PROFILE SEE PROFILE Some of the authors of this publication are also working on these related projects: Ocean data assimilation in support of marine research and operational oceanography in South Africa View project Western Indian Ocean Upwelling Research Initiative (WIOURI), part of the Second International Indian Ocean Expedition (IIO2) View project All content following this page was uploaded by Michael Roberts on 20 May 2015. The user has requested enhancement of the downloaded file. All in-text references underlined in blue are added to the original document and are linked to publications on ResearchGate, letting you access and read them immediately. Deep-Sea Research II 100 (2014) 10–26 Contents lists available at ScienceDirect Deep-Sea Research II journal homepage: www.elsevier.com/locate/dsr2 In situ measured current structures of the eddy field -
Coral Reef Degradation in the Indian Ocean
CORAL REEF DEGRADATION IN THE INDIAN OCEAN Status reports and project presentations 1999 – 1 – CORAL REEF DEGRADATION IN THE INDIAN OCEAN Status reports and project presentations 1999 Published by CORDIO SAREC Marine Science Program Department of Zoology Stockholm University 106 91 Stockholm Sweden ISBN 91-630-8329-9 Maps by Jeanette Bergman Weihed, Tellurit Datorgrafik Produced by Niki Sporrong Enkla Ord, Uppsala Layout by Tryckfaktorn AB, Hans Melcherson Printed by Erlanders Gotab, 1999 – 2 – Foreword Corals as organisms and coral reefs as structures and threaten these peoples livelihoods and endanger a large ecosystems have fascinated scientists for centuries. proportion of the world’s coral reefs, especially those Charles Darwin became well-known among natural adjacent to human populations. In addition, thermal scientists long before the publication of The Origin of pollution from power plants and the chemical industry Species, partly because of his studies of coral reefs and has contributed to coral damage in some industrialised coral islands. Undoubtedly, this fascination for coral areas. reefs is a direct result of the tremendous diversity of When corals become stressed, a typical response is species, exemplified by the overwhelming number of “bleaching” and it occurs when the symbiotic algae are fish of all shapes and colours, that inhabit the world’s lost from the tissue of the coral polyp. For short periods, richest marine ecosystem. the polyp can survive without the algae, but unless the Fundamental to the existence of coral reefs is the situation that caused the bleaching improves and new symbiosis between the reef-building coral polyp and the algae are incorporated into the tissue, the coral will die.