ESSO–National Centre for Antarctic and Ocean Research
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Technical Report No. 21
Technical Report No. 21 Climatology of the HOPE-G Global Ocean - Sea Ice General Circulation Model Stephanie Legutke, Deutsches Klimarechenzentrum Ernst Maier-Reimer, Max-Planck-Institut für Meteorologie Bundesstraße 55, D-20146 Hamburg Edited by: Modellberatungsgruppe, DKRZ Hamburg, December 1999 ISSN 0940-9327 ABSTRACT The HOPE-G global ocean general circulation model (OGCM) climatology, obtained in a long-term forced integration is described. HOPE-G is a primitive-equation z-level ocean model which contains a dynamic-thermodynamic sea-ice model. It is formulated on a 2.8o grid with increased resolution in low latitudes in order to better resolve equatorial dynamics. The vertical resolution is 20 layers. The purpose of the integration was both to investigate the models ability to reproduce the observed gen- eral circulation of the world ocean and to obtain an initial state for coupled atmosphere - ocean - sea-ice climate simulations. The model was driven with daily mean data of a 15-year integration of the atmo- sphere general circulation model ECHAM4, the atmospheric component in later coupled runs. Thereby, a maximum of the flux variability that is expected to appear in coupled simulations is included already in the ocean spin-up experiment described here. The model was run for more than 2000 years until a quasi-steady state was achieved. It reproduces the major current systems and the main features of the so-called conveyor belt circulation. The observed distribution of water masses is reproduced reasonably well, although with a saline bias in the intermediate water masses and a warm bias in the deep and bottom water of the Atlantic and Indian Oceans. -
Lecture Notes in Physical Oceanography
LECTURE NOTES IN PHYSICAL OCEANOGRAPHY ODD HENRIK SÆLEN EYVIND AAS 1976 2012 CONTENTS FOREWORD INTRODUCTION 1 EXTENT OF THE OCEANS AND THEIR DIVISIONS 1.1 Distribution of Water and Land..........................................................................1 1.2 Depth Measurements............................................................................................3 1.3 General Features of the Ocean Floor..................................................................5 2 CHEMICAL PROPERTIES OF SEAWATER 2.1 Chemical Composition..........................................................................................1 2.2 Gases in Seawater..................................................................................................4 3 PHYSICAL PROPERTIES OF SEAWATER 3.1 Density and Freezing Point...................................................................................1 3.2 Temperature..........................................................................................................3 3.3 Compressibility......................................................................................................5 3.4 Specific and Latent Heats.....................................................................................5 3.5 Light in the Sea......................................................................................................6 3.6 Sound in the Sea..................................................................................................11 4 INFLUENCE OF ATMOSPHERE ON THE SEA 4.1 Major Wind -
The Undiscovered Oil and Gas of Antarctica
DEPARTMENT OF THE INTERIOR U.S. Geological Survey The Undiscovered Oil and Gas of Antarctica by John Kingston^ OPEN-FILE REPORT 91-597 This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards or with the North American Stratigraphic Code. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. ^Santa Barbara, California CONTENTS Page Abstract ....................................................... 1 Introduction ................................................... 2 Size of area .............................................. 2 Premise and problems of petroleum recoverability .......... 2 Previous investigations and petroleum assessments ......... 2 Methods of assessment ..................................... 4 Regional geology and petroleum occurrence ...................... 6 Assessment by play analysis .................................... 13 Rifted continental margin provinces ....................... 13 General; the south Australia rifted margin analog .... 13 Antarctica-Australia rift province ................... 17 Antarctica-India rift province ....................... 20 Antarctica-Africa rift province ...................... 24 Antarctica-Falkland rift province .................... 24 Interior rift provinces ................................... 30 General .............................................. 30 Ross sea interior rift province ...................... 30 Weddell sea interior rift province .................. -
A Characterisation of the Marine Environment of the North-West Marine Region
A Characterisation of the Marine Environment of the North-west Marine Region A summary of an expert workshop convened in Perth, Western Australia, 5-6 September 2007 Prepared by the North-west Marine Bioregional Planning section, Marine and Biodiversity Division, Department of the Environment, Water, Heritage and the Arts © Commonwealth of Australia 2007. This work is copyright. You may download, display, print and reproduce this material in unaltered form only (retaining this notice) for your personal, non- commercial use or use within your organisation. Apart from any use as permitted under the Copyright Act 1968, all other rights are reserved. Requests and inquiries concerning reproduction and rights should be addressed to Commonwealth Copyright Administration, Attorney General’s Department, Robert Garran Offices, National Circuit, Barton ACT 2600 or posted at http://www.ag.gov.au/cca Disclaimer The views and opinions expressed in this publication are those of the authors and do not necessarily reflect those of the Australian Government or the Minister for the Environment, Heritage and the Arts or the Minister for Climate Change and Water. While reasonable efforts have been made to ensure that the contents of this publication are factually correct, the Commonwealth does not accept responsibility for the accuracy or completeness of the contents, and shall not be liable for any loss or damage that may be occasioned directly or indirectly through the use of, or reliance on, the contents of this publication. 2 Background The Department of the Environment, Water, Heritage and the Arts (DEWHA) is developing a North-west Marine Bioregional Plan under the Environment Protection and Biodiversity Conservation Act 1999 (hereafter referred to as the Act). -
Diffuse Spectral Reflectance-Derived Pliocene and Pleistocene Periodicity from Weddell Sea, Antarctica Sediment Cores
Wesleyan University The Honors College Diffuse Spectral Reflectance-derived Pliocene and Pleistocene Periodicity from Weddell Sea, Antarctica Sediment Cores by Tavo Tomás True-Alcalá Class of 2015 A thesis submitted to the faculty of Wesleyan University in partial fulfillment of the requirements for the Degree of Bachelor of Arts with Departmental Honors in Earth and Environmental Sciences Middletown, Connecticut April, 2015 Table of Contents List of Figures------------------------------------------------------------------------------IV Abstract----------------------------------------------------------------------------------------V Acknowledgements-----------------------------------------------------------------------VI 1. Introduction------------------------------------------------------------------------------1 1.1. Project Context-------------------------------------------------------------------------1 1.2. Antarctic Glacial History-------------------------------------------------------------5 1.3. Pliocene--------------------------------------------------------------------------------11 1.4. Pleistocene-----------------------------------------------------------------------------13 1.5. Weddell Sea---------------------------------------------------------------------------14 1.6. Site & Cores---------------------------------------------------------------------------19 1.7. Project Goals-------------------------------------------------------------------------22 2. Methodology----------------------------------------------------------------------------23 -
In Shackleton's Footsteps
In Shackleton’s Footsteps 20 March – 06 April 2019 | Polar Pioneer About Us Aurora Expeditions embodies the spirit of adventure, travelling to some of the most wild and adventure and discovery. Our highly experienced expedition team of naturalists, historians and remote places on our planet. With over 27 years’ experience, our small group voyages allow for destination specialists are passionate and knowledgeable – they are the secret to a fulfilling a truly intimate experience with nature. and successful voyage. Our expeditions push the boundaries with flexible and innovative itineraries, exciting wildlife Whilst we are dedicated to providing a ‘trip of a lifetime’, we are also deeply committed to experiences and fascinating lectures. You’ll share your adventure with a group of like-minded education and preservation of the environment. Our aim is to travel respectfully, creating souls in a relaxed, casual atmosphere while making the most of every opportunity for lifelong ambassadors for the protection of our destinations. DAY 1 | Wednesday 20 March 2019 Ushuaia, Beagle Channel Position: 21:50 hours Course: 84° Wind Speed: 5 knots Barometer: 1007.9 hPa & falling Latitude: 54°55’ S Speed: 9.4 knots Wind Direction: E Air Temp: 11°C Longitude: 67°26’ W Sea Temp: 9°C Finally, we were here, in Ushuaia aboard a sturdy ice-strengthened vessel. At the wharf Gary Our Argentinian pilot climbed aboard and at 1900 we cast off lines and eased away from the and Robyn ticked off names, nabbed our passports and sent us off to Kathrine and Scott for a wharf. What a feeling! The thriving city of Ushuaia receded as we motored eastward down the quick photo before boarding Polar Pioneer. -
New Record of Dust Input and Provenance During Glacial Periods in Western Australia Shelf (IODP Expedition 356, Site U1461) from the Middle to Late Pleistocene
atmosphere Article New Record of Dust Input and Provenance during Glacial Periods in Western Australia Shelf (IODP Expedition 356, Site U1461) from the Middle to Late Pleistocene Margot Courtillat 1,2,* , Maximilian Hallenberger 3 , Maria-Angela Bassetti 1,2, Dominique Aubert 1,2 , Catherine Jeandel 4, Lars Reuning 5 , Chelsea Korpanty 6 , Pierre Moissette 7,8 , Stéphanie Mounic 9 and Mariem Saavedra-Pellitero 10,11 1 Centre de Formation et de Recherche sur les Environnements Méditerranéens, Université de Perpignan Via Domitia, UMR 5110, 52 Avenue Paul Alduy, CEDEX, F-66860 Perpignan, France; [email protected] (M.-A.B.); [email protected] (D.A.) 2 CNRS, Centre de Formation et de Recherche sur les Environnements Méditerranéens, UMR 5110, 52 Avenue Paul Alduy, CEDEX, F-66860 Perpignan, France 3 Energy & Mineral Resources Group, Geological Institute Wüllnerstr. 2, RWTH Aachen University, 52052 Aachen, Germany; [email protected] 4 Observatoire Midi-Pyrénées, LEGOS (Université de Toulouse, CNRS/CNES/IRD/UPS), 14 Avenue Edouard Belin, 31400 Toulouse, France; [email protected] 5 Institute of Geosciences, CAU Kiel, Ludewig-Meyn-Straße 10, 24118 Kiel, Germany; [email protected] 6 MARUM Center for Marine Environmental Sciences, University of Bremen, Leobener Str. 8, 28359 Bremen, Germany; [email protected] 7 Department of Historical Geology & Palaeontology, Faculty of Geology and Geoenvironment, National and Kapodistrian University of Athens, 15784 Athens, Greece; [email protected] -
Oceanography
Oceanography Chapter 7 CIRCULATION PATTERNS AND OCEAN CURRENTS أ . را اي Chapter 7: Circulation Patterns and Ocean Currents Circulation Patterns and Ocean Currents 7.1 Density -Driven Circulation 7.2 Thermohaline Circulation 7.3 The Layered Oceans The Atlantic Ocean The Arctic Ocean The Pacific Ocean The Indian Ocean 7.4 Measuring Water Properties 7.5 Wind -Driven Water Motion 7.6 Current Flow and Gyres 7.7 Ocean Surface Currents The Pacific Ocean The Atlantic Ocean The Arctic Ocean The Indian Ocean 7.8 Open -Ocean Convergence and Divergence 7.9 Coastal Upwelling and Downwelling 7.10 Eddies 7.11 Measuring the Currents 7.12 Energy Sources Thermal Energy Harnessing the Currents Prepared by: Raed M.Khaldi Chapter 7: Circulation Patterns and Ocean Currents Circulation Patterns and Ocean Currents Major Concept (I) The oceans are not a single, homogeneous body of water. They actually consist of a number of distinct water masses characterized by different densities due to variations in temperature, salinity, and pressure. There is relatively little mixing between water masses. Different water masses can be identified in the oceans on the basis of changes in salinity and/or temperature. Changes in salinity, temperature, and pressure cause differences in density, resulting in the layering we see in seawater. The individual characteristics of water masses are determined at the surface by such processes as: a. the gain and loss of heat, Prepared by: Raed M.Khaldi Chapter 7: Circulation Patterns and Ocean Currents b. evaporation and precipitation patterns, of sea ice, and ذون c. the freezing and thawing d. -
Protection for the Weddell Sea Effort Would Continue Momentum, Safeguard Vital Southern Ocean Waters
A map from Oct 2017 Protection for the Weddell Sea Effort would continue momentum, safeguard vital Southern Ocean waters 48.4 48.6 48.2 Maud Rise Astrid Ridge 48.5 Weddell Sea Marine Protected Area Proposal:a General Protection Zone Fisheries Research Zone Special Protection Zone Weddell Sea CCAMLR management area 48.1 CCAMLR subareas Important Bird Areasb Antarctic Seamountsc Peninsula Sponge distributiond Ice shelf Conservation value of area:e <20% 20-40% 40-60% 60-80% 80-100% Sources: aAlfred Wegener Institute, “Weddell Sea: 8 Reasons for a Marine Protected Area” (2016), https://www.awi.de/fileadmin/user_upload/AWI/Ueber_uns/ Service/Presse/2016/4_Quartal/KM_Weddellmeer_MPA/WEB_UK_Factsheet_Weddellmeer.pdf; bC.M. Harris et al., “Important Bird Areas in Antarctica: 2014 Summary,” BirdLife International and Environmental Research & Assessment Ltd.; cChris Yesson et al., “Knolls and Seamounts in the World Ocean: Links to Shape, KML, and Data Files,” PANGAEA (2011), https://doi.org/10.1594/PANGAEA.757563; dUnpublished sponge distribution in Weddell Sea MPA planning area provided by the Alfred Wegener Institute; eK. Teschke et al., “Scientific Background Document in Support of the Development of a CCAMLR MPA in the Weddell Sea (Antarctica)—Part C: Data Analysis and MPA Scenario Development” (2016), http://epic.awi.de/41178; Marxan “summed solution” represents the percentage of times an area was selected for protection Overview The Commission for the Conservation of Antarctic Marine Living Resources (CCAMLR) is considering a proposal that would create a marine reserve in the Weddell Sea covering 700,000 square miles (1.8 million square kilometers). The Weddell Sea is a remote, ice-covered embayment east of the Antarctic Peninsula, and one of the most pristine marine ecosystems in the world. -
Ocean Surface Circulation
Ocean surface circulation Recall from Last Time The three drivers of atmospheric circulation we discussed: • Differential heating • Pressure gradients • Earth’s rotation (Coriolis) Last two show up as direct forcing of ocean surface circulation, the first indirectly (it drives the winds, also transport of heat is an important consequence). Coriolis In northern hemisphere wind or currents deflect to the right. Equator In the Southern hemisphere they deflect to the left. Major surfaceA schematic currents of them anyway Surface salinity A reasonable indicator of the gyres 31.0 30.0 32.0 31.0 31.030.0 33.0 33.0 28.0 28.029.0 29.0 34.0 35.0 33.0 33.0 33.034.035.0 36.0 34.0 35.0 37.0 35.036.0 36.0 34.0 35.0 35.0 35.0 34.0 35.0 37.0 35.0 36.0 36.0 35.0 35.0 35.0 34.0 34.0 34.0 34.0 34.0 34.0 Ocean Gyres Surface currents are shallow (a few hundred meters thick) Driving factors • Wind friction on surface of the ocean • Coriolis effect • Gravity (Pressure gradient force) • Shape of the ocean basins Surface currents Driven by Wind Gyres are beneath and driven by the wind bands . Most of wind energy in Trade wind or Westerlies Again with the rotating Earth: is a major factor in ocean and Coriolisatmospheric circulation. • It is negligible on small scales. • Varies with latitude. Ekman spiral Consider the ocean as a Wind series of thin layers. Friction Direction of Wind friction pushes on motion the top layers. -
Evaluation of Sea-Ice Thickness from Four Reanalyses in the Antarctic Weddell
https://doi.org/10.5194/tc-2020-71 Preprint. Discussion started: 6 April 2020 c Author(s) 2020. CC BY 4.0 License. Evaluation of Sea-Ice Thickness from four reanalyses in the Antarctic Weddell Sea Qian Shi1,2, Qinghua Yang1,2, Longjiang Mu3,2, Jinfei Wang1,2, François Massonnet4, Matthew Mazloff5 1School of Atmospheric Sciences and Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, 5 Sun Yat-sen University, Zhuhai 519082, China 2Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China 3Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Bremerhaven 27570, Germany 4Georges Lemaître Centre for Earth and Climate Research, Earth and Life Institute, Université catholique de Louvain, Louvain‐ la‐Neuve, Belgium 10 5Scripps Institution of Oceanography, University of California, San Diego, CA, USA Correspondence to: [email protected] and [email protected] Abstract. Ocean-sea ice coupled models constrained by varied observations provide different ice thickness estimates in the Antarctic. We evaluate contemporary monthly ice thickness from four reanalyses in the Weddell Sea, the German contribution of the Estimating the Circulation and Climate of the Ocean project, Version 2 (GECCO2), the Southern Ocean State Estimate 15 (SOSE), the Nucleus for European Modelling of the Ocean (NEMO) based ocean-ice model (called NEMO-EnKF), and the Global Ice-Ocean Modeling and Assimilation System (GIOMAS), and with reference observations from ICESat-1, Envisat, upward looking sonars and visual ship-based sea-ice observations. Compared with ICESat-1 altimetry and in situ observations, all reanalyses underestimate ice thickness near the coast of the western Weddell Sea, even though ICESat-1 and visual observations may be biased low. -
Origin, Signature and Palaeoclimatic Influence of the Antarctic Circumpolar Current
Earth-Science Reviews 66 (2004) 143–162 www.elsevier.com/locate/earscirev Origin, signature and palaeoclimatic influence of the Antarctic Circumpolar Current P.F. Barkera,*, E. Thomasb,c a 25 Church St., Great Gransden, Sandy, Beds SG19 3AF, UK b Department of Earth and Environmental Sciences, Wesleyan University, Middletown, CT 06457, USA c Center for the Study of Global Change, Department of Geology and Geophysics, Yale University, New Haven, CT 06520-1809, USA Accepted 27 October 2003 Abstract The Antarctic Circumpolar Current (ACC) is today the strongest current in the world’s ocean, with a significant influence on global climate. Its assumed history and influence on palaeoclimate, while almost certainly equally profound, are here called into question. In this paper, we review 30 years of accumulated data, interpretation and speculation about the ACC, deriving mainly from DSDP and ODP drilling in the Southern Ocean. For most of this time, a conventional view of ACC development, signature and influence has held sway among palaeoceanographers and marine geologists. In this view, the ACC began at about 34 Ma, close to the Eocene–Oligocene boundary, the time of onset of significant Antarctic glaciation and the time of creation of a deep-water gap (Tasmanian Seaway) between Australia and Antarctica as the South Tasman Rise separated from North Victoria Land. This is the ‘‘smoking gun’’ of synchroneity. The Southern Ocean sediment record shows a latest Eocene development and subsequent geographic expansion of a siliceous biofacies, its northern limit taken to indicate the palaeo- position of the ACC axis. In addition, the ACC was considered to have caused Antarctic glaciation by isolating the continent within a cold-water annulus, reducing north–south heat transport.