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Biennial Review 1969/70 Bedford Institute Dartmouth, Nova Scotia Ocean Science Reviews 1969/70 A
(This page Blank in the original) ii Bedford Institute. ii Biennial Review 1969/70 Bedford Institute Dartmouth, Nova Scotia Ocean Science Reviews 1969/70 A Atlantic Oceanographic Laboratory Marine Sciences Branch Department of Energy, Mines and Resources’ B Marine Ecology Laboratory Fisheries Research Board of Canada C *As of June 11, 1971, Department of Environment (see forward), iii (This page Blank in the original) iv Foreword This Biennial Review continues our established practice of issuing a single document to report upon the work of the Bedford Institute as a whole. A new feature introduced in this edition is a section containing four essays: The HUDSON 70 Expedition by C.R. Mann Earth Sciences Studies in Arctic Marine Waters, 1970 by B.R. Pelletier Analysis of Marine Ecosystems by K.H. Mann Operation Oil by C.S. Mason and Wm. L. Ford They serve as an overview of the focal interests of the past two years in contrast to the body of the Review, which is basically a series of individual progress reports. The search for petroleum on the continental shelves of Eastern Canada and Arctic intensified considerably with several drilling rigs and many geophysical exploration teams in the field. To provide a regional depository for the mandatory core samples required from all drilling, the first stage of a core storage and archival laboratory was completed in 1970. This new addition to the Institute is operated by the Resource Administration Division of the Department of Energy, Mines & Resources. In a related move the Geological Survey of Canada undertook to establish at the Institute a new team whose primary function will be the stratigraphic mapping of the continental shelf. -
Ebb and Flow Tides and Life on Our Once and Future Planet
This article has This been published in or collective redistirbution of any portion of this article by photocopy machine, reposting, or other means is permitted only with the approval of The approval portionthe ofwith any permitted articleonly photocopy by is machine, of this reposting, means or collective or other redistirbution BOOK REVIEWS Ebb and Flow Oceanography Tides and Life on Our Once and Future Planet , V By Tom Koppel, The Dundurn Group, which is the loss of much of the fleet of olume 21, Number 2, a quarterly journal of journal The olume 21, Number 2, a quarterly 2007, 296 pages, ISBN 9781550027266, Alexander the Great due to a tidal bore), Paperback, $26.99 US coastal ecosystems, modern analysis, and extracting energy from tides. Chapter 1 REVIEWED BY JOHN L. LuiCK contains an account of the ancient tidal dockyards at Lothal, India—surely a can- Ebb and Flow: Tides and Life on Our didate for “Engineering Wonders of the Once and Future Planet is well titled. It Ancient World.” The most ambitious and O tells the story of tides, why they matter, original chapter is the final one, whose ceanography Society. Society. ceanography what causes them, and how they have three subheadings are Sea Level Change changed over time. The author, Tom Causes Intertidal Zones to Migrate; Giant all sorts of ammonia and phosphoric Koppel, is not an analyst or theoretician Ancient Tides and Earth’s Rotation; and salts.” Again, tides are shown to play a C of tides but a man of inquisitive mind The Origin, Evolution, and Future of Life crucial role in both the origin and the opyright 2008 by The 2008 by opyright and substantial beachcombing and on Earth. -
The Evolution and Demise of North Brazil Current Rings*
VOLUME 36 JOURNAL OF PHYSICAL OCEANOGRAPHY JULY 2006 The Evolution and Demise of North Brazil Current Rings* DAVID M. FRATANTONI Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts PHILIP L. RICHARDSON Department of Physical Oceanography, Woods Hole Oceeanographic Institution, and Associated Scientists at Woods Hole, Woods Hole, Massachusetts (Manuscript received 27 May 2004, in final form 26 October 2005) ABSTRACT Subsurface float and surface drifter observations illustrate the structure, evolution, and eventual demise of 10 North Brazil Current (NBC) rings as they approached and collided with the Lesser Antilles in the western tropical Atlantic Ocean. Upon encountering the shoaling topography east of the Lesser Antilles, most of the rings were deflected abruptly northward and several were observed to completely engulf the island of Barbados. The near-surface and subthermocline layers of two rings were observed to cleave or separate upon encountering shoaling bathymetry between Tobago and Barbados, with the resulting por- tions each retaining an independent and coherent ringlike vortical circulation. Surface drifters and shallow (250 m) subsurface floats that looped within NBC rings were more likely to enter the Caribbean through the passages of the Lesser Antilles than were deeper (500 or 900 m) floats, indicating that the regional bathymetry preferentially inhibits transport of intermediate-depth ring components. No evidence was found for the wholesale passage of rings through the island chain. 1. Introduction ration from the NBC, anticyclonic rings with azimuthal speeds approaching 100 cm sϪ1 move northwestward a. Background toward the Caribbean Sea on a course parallel to the The North Brazil Current (NBC) is an intense west- South American coastline (Johns et al. -
Lagrangian Measurement of Subsurface Poleward Flow Between 38 Degrees N and 43 Degrees N Along the West Coast of the United States During Summer, 1993
CORE Metadata, citation and similar papers at core.ac.uk Provided by Calhoun, Institutional Archive of the Naval Postgraduate School Calhoun: The NPS Institutional Archive Faculty and Researcher Publications Faculty and Researcher Publications 1996-09-01 Lagrangian Measurement of subsurface poleward Flow between 38 degrees N and 43 degrees N along the West Coast of the United States during Summer, 1993 Collins, Curtis A. Geophysical Research Letters, Vol. 23, No. 18, pp. 2461-2464, September 1, 1996 http://hdl.handle.net/10945/45730 GEOPHYSICAL RESEARCH LETTERS, VOL. 23, NO. 18, PAGES 2461-2464, SEPTEMBER 1, 1996 Lagrangian Measurement of subsurface poleward Flow between 38øN and 43øN along the West Coast of the United States during Summer, 1993 CurtisA. Collins,Newell Garfield, Robert G. Paquette,and Everett Carter 1 Departmentof Oceanography,Naval Postgraduate School, Monterey, California Abstract. SubsurfaceLagrangian measurementsat about Undercurrentalong the coastsof California and Oregon. We 140 m showedthat the pathof the CaliforniaUndercurrent lay are using quasi-isobaric(float depth controlled primarily by next to the continentalslope betweenSan Francisco(37.80N) the pressureeffect on density)RAFOS floats (Rossby et al., and St. GeorgeReef (41.8øN) duringmid-summer 1993. The 1986) to make these measurements. A RAFOS float consists meanspeed along this 500 km pathwas 8 cms-1. Theflow at of a hydrophonemounted in a glasstube that is about2 meters this depth was not disturbedby upwelling centersat Point long. These hydrophonesreceive signals from three sound Reyesor CapeMendocino. Restfits also demonstratethe abil- sources that were moored 400 km offshore between 34.3øN and ity to acousticallytrack floats located well above the sound 40.4øN.The sound sources emit 15 W, 80 s signalsa•t 260 Hz channelaxis along the California coast. -
2019 Weddell Sea Expedition
Initial Environmental Evaluation SA Agulhas II in sea ice. Image: Johan Viljoen 1 Submitted to the Polar Regions Department, Foreign and Commonwealth Office, as part of an application for a permit / approval under the UK Antarctic Act 1994. Submitted by: Mr. Oliver Plunket Director Maritime Archaeology Consultants Switzerland AG c/o: Maritime Archaeology Consultants Switzerland AG Baarerstrasse 8, Zug, 6300, Switzerland Final version submitted: September 2018 IEE Prepared by: Dr. Neil Gilbert Director Constantia Consulting Ltd. Christchurch New Zealand 2 Table of contents Table of contents ________________________________________________________________ 3 List of Figures ___________________________________________________________________ 6 List of Tables ___________________________________________________________________ 8 Non-Technical Summary __________________________________________________________ 9 1. Introduction _________________________________________________________________ 18 2. Environmental Impact Assessment Process ________________________________________ 20 2.1 International Requirements ________________________________________________________ 20 2.2 National Requirements ____________________________________________________________ 21 2.3 Applicable ATCM Measures and Resolutions __________________________________________ 22 2.3.1 Non-governmental activities and general operations in Antarctica _______________________________ 22 2.3.2 Scientific research in Antarctica __________________________________________________________ -
Particle Pathways in the Gulf Stream
Particle Pathways and P-T Shaw2 in the Gulf Stream Abstract East of Cape Hatteras, the Gulf Stream front separates two water masses: Sargasso Sea water to the south and the An experiment is under way to study the kinematics, dynamics, and cold slope waters to its north. The sharpness of the water mass path evolution of the Gulf Stream front between Cape Hatteras and boundary along the current's cyclonic edge and its coincidence 60°W. The Rafos float, which can track the true motion of water with the stream suggests that the front is impermeable to parcels along density surfaces which slope steeply across the Gulf Stream, has recently been developed for this study. These instruments cross-stream exchange of water. (It should be noted that this are launched in the center of the Gulf Stream every 5-15 days for a distinction of separate water masses loses validity below the 30-day mission. Each float provides a trajectory and a continuous midthermocline, where increasing uniformity of water prop- record of temperature and pressure along the trajectory. Our results erties suggests greater cross-stream exchange.) The Gulf so far show that: a) cross-stream motion has a significant vertical -1 Stream is not so isolated from the Sargasso Sea, however. Be- component (ranging to some 0.1 cm • s ) compared to vertical veloc- ities in midocean; b) floats systematically shoal (upwell) as they ap- tween the Florida Straits and Cape Hatteras the transport of proach anticyclonic meanders and deepen (downwell) as they ap- water more than doubles, with nearly all the new water coming proach cyclonic meanders; c) more than half of the floats launched from the Sargasso Sea. -
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). -
Waba Directory 2003
DIAMOND DX CLUB www.ddxc.net WABA DIRECTORY 2003 1 January 2003 DIAMOND DX CLUB WABA DIRECTORY 2003 ARGENTINA LU-01 Alférez de Navió José María Sobral Base (Army)1 Filchner Ice Shelf 81°04 S 40°31 W AN-016 LU-02 Almirante Brown Station (IAA)2 Coughtrey Peninsula, Paradise Harbour, 64°53 S 62°53 W AN-016 Danco Coast, Graham Land (West), Antarctic Peninsula LU-19 Byers Camp (IAA) Byers Peninsula, Livingston Island, South 62°39 S 61°00 W AN-010 Shetland Islands LU-04 Decepción Detachment (Navy)3 Primero de Mayo Bay, Port Foster, 62°59 S 60°43 W AN-010 Deception Island, South Shetland Islands LU-07 Ellsworth Station4 Filchner Ice Shelf 77°38 S 41°08 W AN-016 LU-06 Esperanza Base (Army)5 Seal Point, Hope Bay, Trinity Peninsula 63°24 S 56°59 W AN-016 (Antarctic Peninsula) LU- Francisco de Gurruchaga Refuge (Navy)6 Harmony Cove, Nelson Island, South 62°18 S 59°13 W AN-010 Shetland Islands LU-10 General Manuel Belgrano Base (Army)7 Filchner Ice Shelf 77°46 S 38°11 W AN-016 LU-08 General Manuel Belgrano II Base (Army)8 Bertrab Nunatak, Vahsel Bay, Luitpold 77°52 S 34°37 W AN-016 Coast, Coats Land LU-09 General Manuel Belgrano III Base (Army)9 Berkner Island, Filchner-Ronne Ice 77°34 S 45°59 W AN-014 Shelves LU-11 General San Martín Base (Army)10 Barry Island in Marguerite Bay, along 68°07 S 67°06 W AN-016 Fallières Coast of Graham Land (West), Antarctic Peninsula LU-21 Groussac Refuge (Navy)11 Petermann Island, off Graham Coast of 65°11 S 64°10 W AN-006 Graham Land (West); Antarctic Peninsula LU-05 Melchior Detachment (Navy)12 Isla Observatorio -
Spatial and Interannual Variability in Mesoscale Circulation in the Northern California Current System Julie E
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 113, C04015, doi:10.1029/2007JC004256, 2008 Click Here for Full Article Spatial and interannual variability in mesoscale circulation in the northern California Current System Julie E. Keister1 and P. Ted Strub1 Received 31 March 2007; revised 16 October 2007; accepted 5 December 2007; published 12 April 2008. [1] We used wavelet analyses of sea surface height (SSH) from >13 years of satellite altimeter data to characterize the variability in mesoscale circulation in the northern California Current (35°N–49°N) and explore the mechanisms of variability. We defined ‘‘mesoscale’’ circulation as features, such as eddies and filaments, which have 50- to 300-km length scales and 4- to 18-week temporal scales. Fluctuations in SSH caused by such features were reflected in wavelet analyses as power (energy). Spatial and interannual variation in mesoscale energy was high. Energy was highest at 38°N, decreasing to the north and south. Between 43°N and 48°N, energy was low. Zonally, mesoscale energy was highest between 125°W and 129°W at latitudes south of 44°N; very little power occurred in the deep ocean west of 130°W. Energy peaked during summer/fall in most years. The primary climate signals were suppressed energy during La Nin˜a and cold years and increased energy during El Nin˜o events. Energy was not strongly linked to upwelling winds, but did correspond to climate indices, indicating that basin-scale processes play a role in controlling mesoscale circulation. We hypothesize that climate affects mesoscale energy through changes in both potential and kinetic energy in the form of density gradients and coastal upwelling winds. -
Deep Eddies in the Gulf of Mexico Observed with Floats
NOVEMBER 2018 F U R E Y E T A L . 2703 Deep Eddies in the Gulf of Mexico Observed with Floats HEATHER FUREY AND AMY BOWER Department of Physical Oceanography, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts PAULA PEREZ-BRUNIUS Department of Physical Oceanography, Ensenada Center for Scientific Research and Higher Education (CISESE), Ensenada, Mexico PETER HAMILTON North Carolina State University, Raleigh, North Carolina ROBERT LEBEN Colorado Center for Astrodynamics Research, University of Colorado Boulder, Boulder, Colorado (Manuscript received 20 November 2017, in final form 9 August 2018) ABSTRACT A new set of deep float trajectory data collected in the Gulf of Mexico from 2011 to 2015 at 1500- and 2500-m depths is analyzed to describe mesoscale processes, with particular attention paid to the western Gulf. Wavelet analysis is used to identify coherent eddies in the float trajectories, leading to a census of the basinwide coherent eddy population and statistics of the eddies’ kinematic properties. The eddy census reveals a new formation region for anticyclones off the Campeche Escarpment, located northwest of the Yucatan Peninsula. These eddies appear to form locally, with no apparent direct connection to the upper layer. Once formed, the eddies drift westward along the northern edge of the Sigsbee Abyssal Gyre, located in the southwestern Gulf of Mexico over the abyssal plain. The formation mechanism and upstream sources for the Campeche Escarpment eddies are explored: the observational data suggest that eddy formation may be linked to the collision of a Loop Current eddy with the western boundary of the Gulf. Specifically, the disintegration of a deep dipole traveling under the Loop Current eddy Kraken, caused by the interaction with the northwestern continental slope, may lead to the acceleration of the abyssal gyre and the boundary current in the Bay of Campeche region. -
Antarctica and Isolate It Geographi- East Falkland
©Lonely Planet Publications Pty Ltd S o u t h e r n O c e a n Why Go? Ushuaia............................31 The southern parts of the Atlantic, Indian and Pacific Oceans Falkland Islands .............39 form the fifth ocean of the world, the Southern Ocean. Its Stanley ...........................42 wild waters surround Antarctica and isolate it geographi- East Falkland ..................46 cally, biologically and climatically from the rest of the world. Scattered around these waters are the islands that early ex- West Falkland .................48 plorers and sealers encountered before they actually found South Georgia ................50 Terra Australis Incognita. South Orkney Islands .... 59 Visit the rocky but fecund shores of the Falkland Islands South Shetland and South Georgia, with abundant wildlife and history. Islands .............................61 Most cruises from South America call in at the South Shet- Heard & McDonald land Islands or the South Orkney Islands, where people set Islands ............................69 up their first Antarctic outposts. Travelers from Australia, Macquarie Island ........... 70 New Zealand and South Africa approach the continent from New Zealand’s Sub- the Ross Sea side, with seabird-rich Heard and Macquarie Antarctic Islands .............71 islands. Sailing these waters and sighting these windswept isles Best Places to recreates the journeys of early adventurers. Spot Wildlife Top Resources » North coast of South » South Georgia & South Sandwich official site (www. Georgia (p 50 ) sgisland.gs) Loads of info, including permit requirements. » Livingston Island (p 65 ) » South Georgia Heritage Trust (www.sght.org) History/ » West Falkland (p 48 ) wildlife conservation group. » Deception Island (p 65 ) » Falkland Islands (www.falklandislands.com) Central source on the island group. -
High Frequency Subsurface Lagrangian Measurements in the California Current with RAFOS Floats
Calhoun: The NPS Institutional Archive Theses and Dissertations Thesis Collection 1995-09 High frequency subsurface Lagrangian measurements in the California Current with RAFOS floats Benson, Kirk R. Monterey, California. Naval Postgraduate School http://hdl.handle.net/10945/35108 NAVAL POSTGRADUATE SCHOOL MONTEREY, CALIFORNIA THESIS HIGH FREQUENCY SUBSURFACE LAGRANGIAN MEASUREMENTS IN THE CALIFORNIA CURRENT WITH RAFOS FLOATS by Kirk R. Benson September, 1995 Thesis Advisor: Newell Garfield Second Reader: Robert G. Paquette Approved for public release; distribution is unlimited. 19960402 122 DTic qoMjf&Y mürmam l DISCLAIMS! NOTICE THIS DOCUMENT IS BEST QUALITY AVAILABLE. THE COPY FURNISHED TO DTIC CONTAINED A SIGNIFICANT NUMBER OF PAGES WHICH DO NOT REPRODUCE LEGIBLY. REPORT DOCUMENTATION PAGE Form Approved OMB No. 0704- Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instruction, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing the collection of information. Send comments regarding this burden estimate or an} other aspect of this collection of information, including suggestions for reducing this burden, to Washington Headquarters Services, Directorate for Information Operations and Reports, 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302, and to the Office of Management and Budget, Paperwork Reduction Project (0704-0188) Washington DC 20503. ___^__ 1. AGENCY USE ONLY (Leave REPORT DATE 3.REPORT TYPE AND DATES blank) September 1995 COVERED Master's Thesis 4. TITLE AND SUBTITLE High Frequency Subsurface Lagrangian FUNDING NUMBERS Measurements in the California Current with RAFOS Floats 6. AUTHOR(S) Kirk R. Benson 7.