SA Ocean Currents.Pdf
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
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]]. -
Abnormal Waves on the South East Coast of South Africa
ABNORMAL WAVES ON THE SOUTH EAST COAST OF SOUTH AFRICA by J. K. M allo ry Master M ariner, Captain, S. A. Navy (Rtd.), Professor of Oceanography, University of Cape Town Much has been said and written recently about the abnormal waves which have been experienced over the years along the eastern seaboard of South Africa. Many theories have been put forward as to the probable causes of these waves which have incurred considerable damage to vessels when steaming in a southwesterly direction down the east coast between Durnford Point and Great Fish Point. It would therefore be of interest to examine the details concerning the individual occurrences as far as they are known. Unfortunately it is not always possible to obtain full details after a period of time has elapsed since the wave was reported, hence in some instances the case histories are incomplete. It is safe to say that many other ships must have experienced abnormal waves off the South African coast between Durnford Point and Cape Recife, but because the speed of the vessel at the time had been suitably reduced, the ship sustained no damage and hence there was no specific reason for reporting such an occurrence other than as a matter of interest. This is unfortunate because so much more could have been learnt about these phenomena if more specific reports were available, especially if they were to include details on wind and waves, meteorological data, soundings, ship’s course and speed. A list of eleven known cases of vessels either having reported encountering abnormal wave conditions or having foundered as a result of storm waves is given in Appendix A. -
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. -
Cape-Agulhas-WC033 2020 IDP Amendment
REVIEW AND AMENDMENTS TO THE INTEGRATED DEVELOPMENT PLAN 2020/21 CAPE AGULHAS MUNICIPALITY REVIEW AND AMENDMENTS TO THE INTEGRATED DEVELOPMENT PLAN 2020/21 29 My 2020 Together for excellence Saam vir uitnemendheid Sisonke siyagqwesa 1 | P a g e REVIEW AND AMENDMENTS TO THE INTEGRATED DEVELOPMENT PLAN 2020/21 SECTIONS THAT ARE AMENDED AND UPDATED FOREWORD BY THE EXECUTIVE MAYOR (UPDATED)............................................................................ 4 FOREWORD BY THE MUNICIPAL MANAGER (UPDATED) ..................................................................... 5 1 INTRODUCTION ............................................................................................................................... 7 1.1 INTRODUCTION TO CAPE AGULHAS MUNICIPALITY (UPDATED) ......................................... 7 1.2 THE INTEGRATED DEVELOPMENT PLAN AND PROCESS ......................................................... 8 1.2.4 PROCESS PLAN AND SCHEDULE OF KEY DEADLINES (AMENDMENT) ........................... 8 1.3 PUBLIC PARTICIPATION STRUCTURES, PROCESSES AND OUTCOMES .................................. 9 1.3.3 MANAGEMENT STRATEGIC WORKSHOP (UPDATED) .................................................... 10 2. LEGAL FRAMEWORK AND INTERGOVERNMENTAL STRATEGY ALIGNMENT ................................. 11 2.2.2 WESTERN CAPE PROVINCIAL PERSPECTIVE (AMENDED) ............................................. 11 3 SITUATIONAL ANALYSIS............................................................................................................... -
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; -
Physiological Response to Short-Term Starvation in an Abundant Krill
Physiological response to short-term starvation in an abundant krill species of the Northern Benguela Current, Euphausia hanseni Lara Kim Hünerlage, Isabella Kandjii (MME, Namibia),Thorsten Werner and Friedrich Buchholz Alfred-Wegener-Institut für Polar- und Meeresforschung AWI, Bremerhaven, Germany Introduction Krill occupy a central role in oceanic food webs as consumers as well as producers. They are a major source of nutrition to fish, birds, seals, and whales. A change in a krill population may thus have dramatic impacts on ecosystems. Within the zooplankton community, Euphausia hanseni belongs to one of the most abundant krill species of the Northern Benguela Current (Olivar and Barange 1990; Map 1: Hydrographic situation off the coast of Namibia at 20 m depth. Image is based on CTD data and was created by Barange et al. 1991). GENUS-subproject “Physical Oceanography” (Mohrholz et al. 2011). The aim of this study was to investigate specific adaptations within the life strategy of E. hanseni. The Experimental Design animals rely on upwelling pulses that lead to rich plankton patches as a food source. The Benguela Current system is a nutritionally poly-pulsed and stratified environment. During late austral summer, the region is typically characterized by minimum upwelling A (Hagen et al. 2001) which goes along with short periods of food deprivation. The following questions shall be answered: How does E. hanseni metabolically adjust during a period of starvation, i.e. between upwelling pulses? C B Map 2: Stations sampled in austral summer 30.01- 7.08.2011 during Are there metabolic differences in krill influenced A) Maintenance of krill during starvation experiment (n=48) research cruise of Maria S. -
St Helena Bay
The variability of retention in St Helena Bay Anathi Manyakanyaka MNYANA002 Supervisors: Dr Jenifer Jackson-Veitch (SAEON) and A/Prof Mathieu Rouault (UCT) A minor dissertation submitted in partial fulfilment of the requirements for the degree of Master of Science in Applied Ocean Sciences of the University of Cape Town University of Cape Town Department of Oceanography Faculty of Science Submitted February 2020 The copyright of this thesis vests in the author. No quotation from it or information derived from it is to be published without full acknowledgement of the source. The thesis is to be used for private study or non- commercial research purposes only. Published by the University of Cape Town (UCT) in terms of the non-exclusive license granted to UCT by the author. University of Cape Town Declaration I know that plagiarism is wrong. Plagiarism is to use another’s work and pretend that it is one’s own. I have used the Harvard Style referencing convention for citation and referencing. Each contribution to, and quotation in, this thesis from the work(s) of other people has been attributed and has been cited and referenced. This thesis is my own work. I have not allowed, and will not allow, anyone to copy my work with the intention of passing it off as his or her own work. Signature ______________________________ Date 06 February 2020 _________________ 1 | Page Abstract The circulation in St Helena Bay and the variability of the retention of the Bay are investigated using seasonal climatologies of the Regional Ocean Modelling System (ROMS). While retention has been studied biologically, the seasonality of the hydrodynamics contributing to the retention have received less attention. -
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 -
Characteristics of Intermediate Water Flow in the Benguela Current As
Deep-Sea Research II 50 (2003) 87–118 Characteristics of intermediate water flow in the Benguela current as measured with RAFOS floats P.L. Richardsona,*, S.L. Garzolib a Department of Physical Oceanography, Woods Hole Oceanographic Institution, 360 Woods Hole Road, Woods Hole, MA 02543, 3 Water Street, P.O. Box 721, USA b Atlantic Oceanographic and Meteorological Laboratory, NOAA, 4301 Rickenbacker Causeway, Miami, FL 33149, USA Received 28 September 2001; accepted 26 July 2002 Abstract Seven floats (not launched in rings) crossed over the mid-Atlantic Ridge in the Benguela extension with a mean westward velocity of around 2 cm=s between 22S and 35S. Two Agulhas rings crossed over the mid-Atlantic Ridge with a mean velocity of 5:7cm=s toward 2851: This implies they translated at around 3:8cm=s through the background velocity field near 750 m: The boundaries of the Benguela Current extension were clearly defined from the observations. At 750 m the Benguela extension was bounded on the south by 35S and the north by an eastward current located between 18S and 21S. Other recent float measurements suggest that this eastward current originates near the Trindade Ridge close to the western boundary and extends across most of the South Atlantic, limiting the Benguela extension from flowing north of around 20S. The westward transport of the Benguela extension was estimated to be 15 Sv by integrating the mean westward velocities from 22S to 35S and multiplying by the 500 m estimated thickness of intermediate water. Roughly 1.5 Sv of this are transported by the B3 Agulhas rings that cross the mid-Atlantic Ridge each year (as observed with altimetry). -
Conservation Management in Agulhas National Park: Challenges & Successes a PLACE of CONTINENTAL SIGNIFICANCE…
Conservation Management in Agulhas National Park: Challenges & Successes A PLACE OF CONTINENTAL SIGNIFICANCE… 20⁰00’E 34⁰ 50’ S to be celebrated, a showcase of all we are and all we can achieve SOUTHERNMOST TIP OF AFRICA S34˚49’59” E20˚00’12” ↑ On 14 September 1998 SANParks acquired a 4 ha portion of land at the southernmost tip of the African continent to establish a national park. Reason for establishment Declared in 1999 (GN 1135 in GG 20476) dated 23 September 1999. The key intention of founding the park was to protect the following 4 aspects: Lowland fynbos with A wide variety of wet- Geographic location Rich cultural heritage four vegetation units lands(freshwater of the Southernmost (From Stone-age, San, Khoi with high conservation springs,rivers,estuaries Tip of Africa herders, Shipwrecks, status: ,floodplains,lakes, vleis (To conserve and European settlement, Fishermen, agriculture, Central rûens shale and pans) The ecological maintain the spirit of flower farming, salt mining renoster-veld (critically functioning of the wetlands and place of the endangered); other fresh water systems on southernmost tip of until today) Elim ferricrete fynbos the Agulhas plain is critically Africa and develop its (endangered) dependent on water quality and tourism potential) Agulhas sand fynbos quantity of interlinked pans, wetlands, seasonal streams, (vulnerable) flow and interchanges that Cape inland salt pans occur under natural conditions. (vulnerable The ANP started out with the following huge establishment challenges: • Staff capacity insufficient -
Lecture 4: OCEANS (Outline)
LectureLecture 44 :: OCEANSOCEANS (Outline)(Outline) Basic Structures and Dynamics Ekman transport Geostrophic currents Surface Ocean Circulation Subtropicl gyre Boundary current Deep Ocean Circulation Thermohaline conveyor belt ESS200A Prof. Jin -Yi Yu BasicBasic OceanOcean StructuresStructures Warm up by sunlight! Upper Ocean (~100 m) Shallow, warm upper layer where light is abundant and where most marine life can be found. Deep Ocean Cold, dark, deep ocean where plenty supplies of nutrients and carbon exist. ESS200A No sunlight! Prof. Jin -Yi Yu BasicBasic OceanOcean CurrentCurrent SystemsSystems Upper Ocean surface circulation Deep Ocean deep ocean circulation ESS200A (from “Is The Temperature Rising?”) Prof. Jin -Yi Yu TheThe StateState ofof OceansOceans Temperature warm on the upper ocean, cold in the deeper ocean. Salinity variations determined by evaporation, precipitation, sea-ice formation and melt, and river runoff. Density small in the upper ocean, large in the deeper ocean. ESS200A Prof. Jin -Yi Yu PotentialPotential TemperatureTemperature Potential temperature is very close to temperature in the ocean. The average temperature of the world ocean is about 3.6°C. ESS200A (from Global Physical Climatology ) Prof. Jin -Yi Yu SalinitySalinity E < P Sea-ice formation and melting E > P Salinity is the mass of dissolved salts in a kilogram of seawater. Unit: ‰ (part per thousand; per mil). The average salinity of the world ocean is 34.7‰. Four major factors that affect salinity: evaporation, precipitation, inflow of river water, and sea-ice formation and melting. (from Global Physical Climatology ) ESS200A Prof. Jin -Yi Yu Low density due to absorption of solar energy near the surface. DensityDensity Seawater is almost incompressible, so the density of seawater is always very close to 1000 kg/m 3.