DOCSLIB.ORG

References 241

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
References 241 References 241 References 1. Tchernia, P. (1980). Descriptive Regional Oceanogra- 14. Lutjeharms, J.R.E., W.P.M. de Ruijter and R.G. phy. Pergamon Press, Oxford, 253 pp. Peterson (1992). Interbasin exchange and the Agulhas 2. Lutjeharms, J.R.E. (1972). A Guide to Research Done retroflection; the development of some oceanographic Concerning Ocean Currents and Water Masses in the concepts. Deep-Sea Research, 39(10): 1791–1807. South West Indian Ocean. University of Cape Town, 15. Thomson, C.W. and J. Murray (editors) (1881–1895). Cape Town, 577 pp. Report on the scientific results of the voyage of H.M.S. 3. Lutjeharms, J.R.E. (1980). Fisiese Oseanologie van die Challenger during the years 1873–1876. His Majesty’s Suidwes Indiese Oseaan: ’n bronnelys en oorsig van Stationery Office, London, 50 volumes. 1970 tot 1980. WNNR Verslag, T/SEA 8016, 82 pp. 16. Von Schleinitz, B. (1889–1890). Die Forschungsreise 4. Lutjeharms, J.R.E. (1987). The Physical Oceanology of S.M.S. “Gazelle” in den Jahren 1874 bis 1876 unter the South West Indian Ocean; a bibliography for 1980 Kommando des Kapitän zur Zee Freiherrn von to 1985. WNNR-verslag, T/SEA 8712, 131 pp. Schleinitz. Hydrographische Amt, Reichs-Marine- 5. Lutjeharms, J.R.E. (1992). The Physical Oceanology of Ampts, Berlin, Bände I–V. the South West Indian Ocean; a bibliography from 17. Hydrographic Department (1896). List of oceanic 1986 to 1990. CSIR Research Report, 707, 95 pp. depths and serial temperature observations during the 6. Basto, A. de M. (1945). Diario da viagem de Vasco da years 1895. Great Britain, Hydrographic Department, Gama. Vol. 1. Editora, Porto, 150 pp. London. 7. Rennell, J. (1832). An investigation of the currents of 18. Chun, C. (et al.) (1902–1940). Wissenschaftliche the Atlantic Ocean and of those which prevail between Ergebnisse der Deutschen Tiefsee-Expedition auf dem the Indian Ocean and the Atlantic. J.G. and F. Dampfer Valdivia, 1898–1899. Gustaf Fischer, Jena, 24 Rivington, London, 3xx pp. volumes. 8. Deacon, M. (1971). Scientists and the Sea 1650–1900; 19. Chun, C. (1900). Aus den Tiefen des Weltmeeres. a study of marine science. Academic Press, London, Schilderungen von der Deutschen Tiefsee-Expedition. 445 pp. Gustav Fisher, Jena, 549 pp. 9. Kortum, G. (1990). An unpublished manuscript of 20. Von Drygalski, E. (editor) (1908–1952). Ergebnisse Alexander von Humboldt on the Gulf Stream. In Ocean der Deutschen Südpolar-Expedition 1901–1903. Sciences. Their history and relation to man, editors W. Reichsamtes des Innern, Berlin, Bände I–XX. Lenz and M. Deacon. Deutsche Hydrographische 21. Reichs-marine Ampt (1909). Forschungsreise S.M.S. Zeitschrift, B(22): 122–129. “Planet” 1906–1907. Reichs-marine Ampt, Berlin, 10. Koninklijk Nederlandsch Meteorologisch Instituut Bände I–V. (1857). De Agulhas stroom, afgeleid uit de temperatuur 22. Brennecke, W. (1915). Oceanographische Arbeiten van het zeewater aan de oppervlakte; en de invloed dien S.M.S. Möwe im westlichen Indischen Ozean 1913. deze op de atmosfeer uitoefent. In Uitkomsten van Annalen der Hydrographie und Maritimen Meteo- Wetenschap en Ervaring, aangaande winden en zee- rologie, 43(8): 337–343. stromingen in sommige gedeelten van den oceaan, 23. Anonymous (1970). Agulhas. In Standard Encyclopae- Koninklijk Nederlandsch Meteorologisch Instituut, dia of Southern Africa, editors D.J. Potgieter and P.C. L.E. Bosch en Zoon, Utrecht, pp. 40–50. du Plessis, Vol.1, Nasou, Cape Town, p. 254. 11. Van Gogh, J. (1858). De stormen nabij de Kaap de 24. Kerhallet, M.C.P. de (1852). Considérations générales Goede Hoop in verband beschouwd met de temperatuur sur l’océan Atlantique. Annales Hydrographiques, 1er der zee. Verhandelingen en Mededelingen der Konink- Sem. pp. 33–143. lijke Akademie, afdeling Natuurkunde, 8, 23 pp. 25. Zimmermann, W.F.A. (1865). Der Erdball und Seine 12. Brundrit, G.B. and L.V. Shannon (1989). Cape storms Naturwunder. Gustav Hempel, Berlin, 544 pp. (as and the Agulhas Current: a glimpse of the future? South shown in Peterson et al., 199626). African Journal of Science, 85(10): 619–620. 26. Peterson, R.G., L. Stramma and G. Kortum (1996). 13. Jury, M.R. (1994). A thermal front within the marine Early concepts and charts of ocean circulation. atmospheric boundary layer over the Agulhas Current Progress in Oceanography, 37(1): 1–115. south of Africa: Composite aircraft observations. Jour- 27. Rennell, J. (1778). Chart of the Bank of Lagullus and nal of Geophysical Research, 99(C2): 3297–3304. southern Coast of Africa, London. 242 References 28. Maury, M.F. (1855). The Physical Geography of the lichungen des Instituts für Meereskunde an der Univer- Sea. Harper & Brothers, New York, 274 pp., 12 plates. sität Berlin, n.f. A(16): 39 pp. 29. Findlay, A.G. (1866). A directory for the navigation of 46. Möller, L. (1933). Zur Frage der Tiefenzirkulation im the Indian Ocean. Richard Holmes Laurie, London, Indischen Ozean. Annalen des Hydrographie Berlin, 113 pp. 61(8,9): 233–236. 30. Krümmel, O. (1882). Bemerkungen über die Meere- 47. Thomsen, H. (1935). Entstehung und Verbreitung strömungen und Temperaturen in der Falklandsee. Aus einiger charakteristischer Wassermassen in dem den Archiv der Deutschen Seewarte, V, 2, 25 pp. (as Indischen und südlichen Pazifischen Ozean. Annalen shown by Peterson et al., 199626). der Hydrographie und Maritimen Meteorologie, 63(8): 31. Krümmel, O. (1911). Handbuch der Ozeanographie. 293–305. Band II. Die Bewegungsformen des Meeres. von J. 48. Thomsen, H. (1933). The circulation in the depths of Engelhorns Nachf., Stuttgart, 766 pp. the Indian Ocean. Journal Conseil, 8(1): 73–79. 32. Merz, A. (1925). Die Deutsche Atlantische Expedition 49. Schott, G. (1935). Geographie des Indischen und auf dem Vermessungs- und Forschungsschiff “Meteor”. Stillen Ozeans. C. Boysen, 413 pp., 37 plates. Sitzungsberichten der Physikalish-Matematischen 50. Sverdrup, H.U., H.W. Johnson and R.H. Flemming Klasse der Preussischen Akademie der Wissenschaften, (1942). The oceans; their physics, chemistry and gen- 31, pp. 562–586. eral biology. Prentice-Hall, Englewood Cliffs, 1087 pp. 33. Defant, A. (1932–1960). Wissenschaftlichen Ergeb- 51. Brown, A.C. (1997). John D.F. Gilchrist and the early nisse der Deutschen Atlantischen Expedition auf dem years of marine science in South Africa. In A Century Forschung- und Vermessungschiff “Meteor” 1925– of Marine Science in South Africa, editors A.I.L. Payne 1927. Bände I–XVI, Berlin. and J.R.E. Lutjeharms, Sea Fisheries Research Institute, 34. Discovery Committee (1929). Discovery Investigations Royal Society of South Africa, pp. 2–16 and Transac- Station List, 1925–1927. Discovery Reports, 1: 3–138. tions of the Royal Society of South Africa, 52(1): 2–16. 35. B[arlow], E.W. (1932). Major James Rennell. Marine 52. Summers, R.F.H. (1975). A History of the South Afri- Observer, 9(101): 94–98. 496. can Museum, 1825–1975. A. A. Balkema, Cape Town, 36. Pollard, R. and G. Griffiths (1993). James Rennell, the 245 pp. father of oceanography. Ocean Challenge, 4(1/2): 24– 53. Gilchrist, J.D.F. (1923). The South African seas. South 25. African Journal of Science, 20(1): 1–27. 37. Bravo, M. (1993). James Rennell: antiquarian of ocean 54. Gilchrist, J.D.F. (1902). Observations on the tempera- currents. Ocean Challenge, 4(1/2): 41–50. ture and salinity of the sea around the Cape Peninsula. 38. Gould, J. (1993). James Rennell’s view of the Atlantic Marine Investigations in South Africa, 1: 181–216 + 10 circulation: a comparison with our present knowledge. plates + p. 238. Ocean Challenge, 4(1/2): 26–32. 55. Gilchrist, J.D.F. (1904). Currents on the South African 39. Markham, C.R. (1901). Major James Rennell and the coast, as indicated by the course of drift bottles. Marine rise of modern English geography. Cassell and Com- Investigations in South Africa, 2: 101–113. pany, London, 232 pp. 56. Lutjeharms, J.R.E. and L.V. Shannon (1997). A century 40. Dietrich, G. (1935). Aufbau und Dynamik des süd- of physical oceanography in South Africa; in search of lichen Agulhasstromgebietes. Veröffentlichungen des the legacy of John D. Gilchrist. In A Century of Marine Institut für Meereskunde an der Universität Berlin, n.f. Science in South Africa, editors A.I.L. Payne and J.R.E. A(27): 79 pp. Lutjeharms, Sea Fisheries Research Institute, Royal 41. Dietrich, G. (1936). Aufbau und Bewegung von Golf- Society of South Africa, pp. 17–30 and Transactions of strom und Agulhasstrom, eine vergleichende Betrach- the Royal Society of South Africa, 52(1): 17–30. tung. Naturwissenschaften, 24(15): 225–230. 57. Gilchrist, J.D.F. (1925). II. Report of Director of Sur- 42. Dietrich, G. (1935). Zur Dynamik des Atlantischen vey. In Report of the Fisheries and Marine Biological Zweiges des Agulhasstromes. Annalen der Hydro- Survey, Union of South Africa, June, 1923–June, 1925. graphie und Maritimen Meteorologie, 63: 383–387. 4. Cape Town; Government Printers: xix–lx. 43. Möller, L. (1929). Die Zirkulation des Indischen Ozeans; 58. Gilchrist, J.D.F. (1905). The South African marine auf Grund von Temperatur- und Salzgehaltstiefen- fauna and its environment. In Science in South Africa, messungen und Oberflächenstrombeobachtungen. editors W. Flint and J.D.F. Gilchrist, Maskew Miller, Veröffentlichungen des Instituts für Meereskunde an Cape Town, pp. 182–197. der Universität Berlin, n.f. A21: 48 pp. 59. Harris, T.F.W., R. Legeckis and D. van Forest [sic] 44. Michaelis, G. (1923). Die Wasserbewegung an der (1978). Satellite infra-red images in the Agulhas Cur- Oberfläche des Indischen Ozeans im Januar und Juli. rent system. Deep-Sea Research, 25(6): 543–548. Veröffentlichungen des Instituts für Meereskunde an 60. Lutjeharms, J.R.E. (1981). Features of the southern der Universität Berlin, n.f. A8(16): 32 pp.
Load more

Recommended publications
  • Diversity Visa Program, DV 2019-2021: Number of Entries During Each Online Registration Period by Region and Country of Chargeability
    Diversity Visa Program, DV 2019-2021: Number of Entries During Each Online Registration Period by Region and Country of Chargeability The totals below DO NOT represent the number of diversity visas issued nor the number of selected entrants Countries marked with a "0" indicate that there were no entrants from that country or area. Countries marked with "N/A" were typically not eligible for that program year. FY 2019 FY 2020 FY 2021 Region Foreign State of Chargeabiliy Entrants Derivatives Total Entrants Derivatives Total Entrants Derivatives Total Africa Algeria 227,019 123,716 350,735 252,684 140,422 393,106 221,212 129,004 350,216 Africa Angola 17,707 25,543 43,250 14,866 20,037 34,903 14,676 18,086 32,762 Africa Benin 128,911 27,579 156,490 150,386 26,627 177,013 92,847 13,149 105,996 Africa Botswana 518 462 980 552 406 958 237 177 414 Africa Burkina Faso 37,065 7,374 44,439 30,102 5,877 35,979 6,318 2,591 8,909 Africa Burundi 20,680 16,295 36,975 22,049 19,168 41,217 12,287 11,023 23,310 Africa Cabo Verde 1,377 1,272 2,649 894 778 1,672 420 312 732 Africa Cameroon 310,373 147,979 458,352 310,802 165,676 476,478 150,970 93,151 244,121 Africa Central African Republic 1,359 893 2,252 1,242 636 1,878 906 424 1,330 Africa Chad 5,003 1,978 6,981 8,940 3,159 12,099 7,177 2,220 9,397 Africa Comoros 296 224 520 293 128 421 264 111 375 Africa Congo-Brazzaville 21,793 15,175 36,968 25,592 19,430 45,022 21,958 16,659 38,617 Africa Congo-Kinshasa 617,573 385,505 1,003,078 924,918 415,166 1,340,084 593,917 153,856 747,773 Africa Cote d'Ivoire 160,790
    [Show full text]
  • Management of Demersal Fisheries Resources of the Southern Indian Ocean
    FAO Fisheries Circular No. 1020 FIRM/C1020 (En) ISSN 0429-9329 MANAGEMENT OF DEMERSAL FISHERIES RESOURCES OF THE SOUTHERN INDIAN OCEAN Cover photographs courtesy of Mr Hannes du Preez, Pioneer Fishing, Heerengracht, South Africa. Juvenile of Oreosoma atlanticum (Oreosomatidae). This fish was caught at 39° 15’ S, 45° 00’ E, late in 2005 at around 650 m while mid-water trawling for alfonsinos. This genus is remarkable for the large conical tubercles that cover the dorsal surface of the younger fish. Illustration by Ms Emanuela D’Antoni, Marine Resources Service, FAO Fisheries Department. Copies of FAO publications can be requested from: Sales and Marketing Group Information Division FAO Viale delle Terme di Caracalla 00153 Rome, Italy E-mail: [email protected] Fax: (+39) 06 57053360 FAO Fisheries Circular No. 1020 FIRM/C1020 (En) MANAGEMENT OF DEMERSAL FISHERIES RESOURCES OF THE SOUTHERN INDIAN OCEAN Report of the fourth and fifth Ad Hoc Meetings on Potential Management Initiatives of Deepwater Fisheries Operators in the Southern Indian Ocean (Kameeldrift East, South Africa, 12–19 February 2006 and Albion, Petite Rivière, Mauritius, 26–28 April 2006) including specification of benthic protected areas and a 2006 programme of fisheries research. compiled by Ross Shotton FAO Fisheries Department FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2006 The mention or omission of specific companies, their products or brand names does not imply any endorsement or judgement by the Food and Agriculture Organization of the United Nations. The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries.
    [Show full text]
  • Automatic Exchange of Information: Status of Commitments
    As of 27 September 2021 AUTOMATIC EXCHANGE OF INFORMATION (AEOI): STATUS OF COMMITMENTS1 JURISDICTIONS UNDERTAKING FIRST EXCHANGES IN 2017 (49) Anguilla, Argentina, Belgium, Bermuda, British Virgin Islands, Bulgaria, Cayman Islands, Colombia, Croatia, Cyprus2, Czech Republic, Denmark, Estonia, Faroe Islands, Finland, France, Germany, Gibraltar, Greece, Guernsey, Hungary, Iceland, India, Ireland, Isle of Man, Italy, Jersey, Korea, Latvia, Liechtenstein, Lithuania, Luxembourg, Malta, Mexico, Montserrat, Netherlands, Norway, Poland, Portugal, Romania, San Marino, Seychelles, Slovak Republic, Slovenia, South Africa, Spain, Sweden, Turks and Caicos Islands, United Kingdom JURISDICTIONS UNDERTAKING FIRST EXCHANGES BY 2018 (51) Andorra, Antigua and Barbuda, Aruba, Australia, Austria, Azerbaijan3, The Bahamas, Bahrain, Barbados, Belize, Brazil, Brunei Darussalam, Canada, Chile, China, Cook Islands, Costa Rica, Curacao, Dominica4, Greenland, Grenada, Hong Kong (China), Indonesia, Israel, Japan, Lebanon, Macau (China), Malaysia, Marshall Islands, Mauritius, Monaco, Nauru, New Zealand, Niue4, Pakistan3, Panama, Qatar, Russia, Saint Kitts and Nevis, Saint Lucia, Saint Vincent and the Grenadines, Samoa, Saudi Arabia, Singapore, Sint Maarten4, Switzerland, Trinidad and Tobago4, Turkey, United Arab Emirates, Uruguay, Vanuatu JURISDICTIONS UNDERTAKING FIRST EXCHANGES BY 2019 (2) Ghana3, Kuwait5 JURISDICTIONS UNDERTAKING FIRST EXCHANGES BY 2020 (3) Nigeria3, Oman5, Peru3 JURISDICTIONS UNDERTAKING FIRST EXCHANGES BY 2021 (3) Albania3, 7, Ecuador3, Kazakhstan6
    [Show full text]
  • The Structure and Transport of the Agulhas Return Current
    The Structure and Transport of the Agulhas Return Current Isabelle Jane Ansorge Submitted in fulfillment of the requirements of the Master of Science degree Department of Oceanography University of Cape Town 1996 University of Cape Town 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 I ABSTRACT The Agulhas Current flows along the eastern coast of southern Africa as one of the largest western boundary currents in the world's ocean. On overshooting the southern tip of Africa at approximately 20°E, a retroflection loop is formed that causes the current to double back on itself and to fonn the easterly flowing Agulhas Return Current. No focussed investigation to establish the hydrography of this imponant component of global ocean circulation has to date been carried out. To trace the Agulhas Return Current's passage eastwards into the South Indian Ocean, data collected from six CTD hydrographic cruises; AJAX, ARC, SCARC, Marathon, Discovery 164 and SUZIL, as well as from three XBT temperature cruises,· Marion 83, Gallieni 72 and FIBEX, have been analysed. It is shown that the Agulhas Return Current initially flows zonally from 20°-25°E at a latitude approximately 39°30'-40°30'S before forming a planetary wave over the Agulhas Plateau between 25°-28°E.
    [Show full text]
  • Connectivity and Population Structure of Albacore Tuna Across Southeast Atlantic and Southwest Indian Oceans Inferred from Multi
    www.nature.com/scientificreports OPEN Connectivity and population structure of albacore tuna across southeast Atlantic and southwest Indian Oceans inferred from multidisciplinary methodology Natacha Nikolic1,2,3,12*, Iratxe Montes4, Maxime Lalire5, Alexis Puech1, Nathalie Bodin6,11,13, Sophie Arnaud‑Haond7, Sven Kerwath8,9, Emmanuel Corse2,14, Philippe Gaspar 5,10, Stéphanie Hollanda11, Jérôme Bourjea1, Wendy West8,15 & Sylvain Bonhommeau 1,15 Albacore tuna (Thunnus alalunga) is an important target of tuna fsheries in the Atlantic and Indian Oceans. The commercial catch of albacore is the highest globally among all temperate tuna species, contributing around 6% in weight to global tuna catches over the last decade. The accurate assessment and management of this heavily exploited resource requires a robust understanding of the species’ biology and of the pattern of connectivity among oceanic regions, yet Indian Ocean albacore population dynamics remain poorly understood and its level of connectivity with the Atlantic Ocean population is uncertain. We analysed morphometrics and genetics of albacore (n = 1,874) in the southwest Indian (SWIO) and southeast Atlantic (SEAO) Oceans to investigate the connectivity and population structure. Furthermore, we examined the species’ dispersal potential by modelling particle drift through major oceanographic features. Males appear larger than females, except in South African waters, yet the length–weight relationship only showed signifcant male–female diference in one region (east of Madagascar and Reunion waters). The present study produced a genetic diferentiation between the southeast Atlantic and southwest Indian Oceans, supporting their demographic independence. The particle drift models suggested dispersal potential of early life stages from SWIO to SEAO and adult or sub-adult migration from SEAO to SWIO.
    [Show full text]
  • Joint Geological Survey/University of Cape Town MARINE GEOSCIENCE UNIT TECHNICAL ^REPORT NO. 13 PROGRESS REPORTS for the YEARS 1
    Joint Geological Survey/University of Cape Town MARINE GEOSCIENCE UNIT TECHNICAL ^REPORT NO. 13 PROGRESS REPORTS FOR THE YEARS 1981-1982 Marine Geoscience Group Department of Geology University of Cape Town December 1982 NGU-Tfc—Kh JOINT GEOLOGICAL SURVEY/UNIVERSITY OF CAPE TOWN MARINE GEOSCIENCE UNIT TECHNICAL REPORT NO. 13 PROGRESS REPORTS FOR THE YEARS 1981-1982 Marine Geoscience Group Department of Geology University of Cape Town December 1982 The Joint Geological Survey/University of Cape Town Marine Geoscience Unit is jointly funded by the two parent organizations to promote marine geoscientific activity in South Africa. The Geological Survey Director, Mr L.N.J. Engelbrecht, and the University Research Committee are thanked for their continued generous financial and technical support for this work. The Unit was established in 1975 by the amalgamation of the Marine Geology Programme (funded by SANCOR until 1972) and the Marine Geophysical Unit. Financial ?nd technical assistance from the South African National Committee for Oceanographic Research, and the National Research Institute for Oceanology (Stellenbosch) are also gratefully acknowledged. It is the policy of the Geological Survey and the University of Cape Town that the data obtained may be presented in the form of theses for higher degrees and that completed projects shall be published without delay in appropriate media. The data and conclusions contained in this report are made available for the information of the international scientific community with tl~e request that they be not published in any manner without written permission. CONTENTS Page INTRODUCTION by R.V.Dingle i PRELIMINARY REPORT ON THE BATHYMETRY OF PART OF 1 THE TRANSKEI BASIN by S.H.
    [Show full text]
  • International Ocean Discovery Program Expedition 361 Preliminary Report South African Climates (Agulhas LGM Density Profile)
    International Ocean Discovery Program Expedition 361 Preliminary Report South African Climates (Agulhas LGM Density Profile) 30 January–31 March 2016 Ian R. Hall, Sidney R. Hemming, Leah J. LeVay, and the Expedition 361 Scientists Publisher’s notes Core samples and the wider set of data from the science program covered in this report are under moratorium and accessible only to Science Party members until 30 September 2017. This publication was prepared by the JOIDES Resolution Science Operator (JRSO) at Texas A&M University (TAMU) as an account of work performed under the International Ocean Discovery Pro- gram (IODP). Funding for IODP is provided by the following international partners: National Science Foundation (NSF), United States Ministry of Education, Culture, Sports, Science and Technology (MEXT), Japan European Consortium for Ocean Research Drilling (ECORD) Ministry of Science and Technology (MOST), People’s Republic of China Korea Institute of Geoscience and Mineral Resources (KIGAM) Australia-New Zealand IODP Consortium (ANZIC) Ministry of Earth Sciences (MoES), India Coordination for Improvement of Higher Education Personnel, Brazil (CAPES) Portions of this work may have been published in whole or in part in other International Ocean Discovery Program documents or publications. Disclaimer Any opinions, findings, and conclusions or recommendations expressed in this publication are those of the author(s) and do not necessarily reflect the views of the participating agencies, TAMU, or Texas A&M Research Foundation. Copyright Except where otherwise noted, this work is licensed under a Creative Commons Attribution License. Unrestricted use, distribution, and reproduction is permitted, provided the original author and source are credited. Citation Hall, I.R., Hemming, S.R., LeVay, L.J., and the Expedition 361 Scientists, 2016.
    [Show full text]
  • JOIDES Resolution Expedition 361 (Southern African Climates) Site
    IODP Expedition 361: Southern African Climates Site U1475 Summary Background and Objectives Site U1475 is located on the southwestern flank of Agulhas Plateau (41°25.61′S, 25°15.64′E), ~450 nmi south of Port Elizabeth, South Africa, in a water depth of 2669 mbsl. The Agulhas Plateau, which was formed during the early stages of the opening of the South Atlantic about 90 Ma (Parsiegla et al., 2008), is a major bathymetric high that is variably coated with sediments (Uenzelmann Neben, 2001). The 230,000 km2 plateau, which ascends up to ~2500 m above the adjacent seafloor, is bounded on the north by the 4700 m deep Agulhas Passage and is flanked by the Agulhas Basin in the west and the Transkei Basin in the northeast. The northern part of the plateau is characterized by rugged topography, while the central and southern part of the plateau exhibits a relatively smooth topography (Allen and Tucholke, 1981) and has greater sediment thickness (Uenzelmann Neben, 2001). A strong water mass transport flows across the Agulhas Plateau region (Macdonald, 1993), which involves the water column from the surface down to Upper Circumpolar Deep Water. The hydrography of the upper ocean is dominated by the Agulhas Return Current, which comprises the component of the Agulhas Current that is not leaked to the South Atlantic Ocean but rather flows eastwards from the retroflection (Lutjeharms and Ansorge, 2001). Antarctic Intermediate Water, below the Agulhas Return Current, also follows the same flow path near South Africa as the Agulhas Current showing a similar retroflection (Lutjeharms, 1996).
    [Show full text]
  • Summary Record
    SC60 summary record CONVENTION ON INTERNATIONAL TRADE IN ENDANGERED SPECIES OF WILD FAUNA AND FLORA ____________________ Sixtieth meeting of the Standing Committee Doha (Qatar), 25 March 2010 SUMMARY RECORD 1. Election of the Chair, Vice-Chair and Alternate Vice-Chair of the Standing Committee The Secretariat, as temporary chair of the meeting, confirmed that, following the elections at CoP15, the current members of the Standing Committee were as follows: Africa: Botswana, the Democratic Republic of the Congo, Egypt and Uganda; Asia: the Islamic Republic of Iran, Japan and Kuwait; Central and South America and the Caribbean: Colombia, Costa Rica and Dominica; Europe: Bulgaria, Norway, Ukraine and the United Kingdom of Great Britain and Northern Ireland; North America: the United States of America; Oceania: Australia; and Non-elected members: Qatar (previous host country), Switzerland (Depositary Government) and Thailand (next host country). Norway was nominated as the new Chair of the Standing Committee. Norway thanked the Committee for the honour but noted that their acceptance of this position would have to be confirmed in the following weeks. Therefore the Committee agreed that Norway would be the new Chair, subject to its confirmation. The Committee elected the United States as its Vice-Chair and Kuwait as its Alternate Vice-Chair. The representative of Norway chaired the rest of the meeting, thanking the members of the Committee for the privilege and for the confidence they had shown in his country. During discussion of this item, interventions were made by the regional representatives of Asia (Kuwait), Europe (Norway) and North America (the United States), and by Chile.
    [Show full text]
  • Member States
    1/10/19 Total: 193 MEMBER STATES Afghanistan Democratic Republic of the Congo Albania Denmark Algeria Djibouti Andorra Dominica Angola Dominican Republic* Antigua and Barbuda Ecuador Argentina* Egypt* Armenia El Salvador Australia* Equatorial Guinea* Austria Eritrea Azerbaijan Estonia Bahamas Eswatini Bahrain Ethiopia Bangladesh Fiji Barbados Finland* Belarus France* Belgium Gabon Belize Gambia Benin Georgia Bhutan Germany* Bolivia (Plurinational State of) Ghana Bosnia and Herzegovina Greece* Botswana Grenada Brazil* Guatemala Brunei Darussalam Guinea Bulgaria Guinea-Bissau Burkina Faso Guyana Burundi Haiti Cabo Verde Honduras Cambodia Hungary Cameroon Iceland Canada* India* Central African Republic Indonesia Chad Iran (Islamic Republic of) Chile Iraq China* Ireland Colombia* Israel Comoros Italy* Congo Jamaica Cook Islands Japan* Costa Rica* Jordan Côte d'Ivoire* Kazakhstan Croatia Kenya Cuba Kiribati Cyprus Kuwait Czechia Kyrgyzstan Democratic People's Republic of Korea Lao People's Democratic Republic *Council Member State Latvia Rwanda Lebanon Saint Kitts and Nevis Lesotho Saint Lucia Liberia Saint Vincent and the Grenadines Libya Samoa Lithuania San Marino Luxembourg Sao Tome and Principe Madagascar Saudi Arabia* Malawi Senegal Malaysia* Serbia Maldives Seychelles Mali Sierra Leone Malta Singapore* Marshall Islands Slovakia Mauritania Slovenia Mauritius Solomon Islands Mexico* Somalia Micronesia (Federated States of) South Africa* Monaco South Sudan Mongolia Spain* Montenegro Sri Lanka Morocco Sudan* Mozambique Suriname Myanmar Sweden
    [Show full text]
  • Tectonic History, Microtopography and Bottom Water Circulation of the Natal Valley and Mozambique Ridge, Southwest Indian Ocean
    Tectonic history, microtopography and bottom water circulation of the Natal Valley and Mozambique Ridge, southwest Indian Ocean. By: Errol Avern Wiles Submitted in fulfilment of the degree Doctor of Philosophy In the Discipline of Geological Sciences School of Agricultural, Earth and Environmental Sciences College of Agriculture, Engineering and Science University of KwaZulu Natal, Durban South Africa 2014 i Preface The experimental work described in this thesis was carried out in the Discipline of Geological Sciences, University of KwaZulu-Natal, Westville, from July 2010 to November 2014, under the supervision of Prof. Watkeys, Dr. Green and Prof. Jokat. These studies represent original work by the author and have not otherwise been submitted in any form for any degree or diploma to any tertiary institution. Where use has been made of the work of others it is duly acknowledged in the text. Signed:_____________________ Name:________________________ Date:_____________ ii Declaration 1 – Plagiarism I, Errol Avern Wiles, declare that: 1. The research reported in this thesis, except where otherwise indicated, is my original research. 2. This thesis has not been submitted for any degree or examination at any other university. 3. This thesis does not contain other persons’ data, graphs or other information, unless specifically acknowledged as being sourced from other persons. 4. This thesis does not contain any other persons writing, unless specifically acknowledged as being sourced from other researchers. Where other written sources have been quoted then: a. Their words have been re-written but the general information attributed to them has been referenced b. Where their exact words have been used, then their writing has been placed in italics and inside quotation marks, and referenced.
    [Show full text]
  • 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
    [Show full text]