Calving Cycle of the Brunt Ice Shelf, Antarctica, Driven by Changes in Ice Shelf Geometry
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Species Status Assessment Emperor Penguin (Aptenodytes Fosteri)
SPECIES STATUS ASSESSMENT EMPEROR PENGUIN (APTENODYTES FOSTERI) Emperor penguin chicks being socialized by male parents at Auster Rookery, 2008. Photo Credit: Gary Miller, Australian Antarctic Program. Version 1.0 December 2020 U.S. Fish and Wildlife Service, Ecological Services Program Branch of Delisting and Foreign Species Falls Church, Virginia Acknowledgements: EXECUTIVE SUMMARY Penguins are flightless birds that are highly adapted for the marine environment. The emperor penguin (Aptenodytes forsteri) is the tallest and heaviest of all living penguin species. Emperors are near the top of the Southern Ocean’s food chain and primarily consume Antarctic silverfish, Antarctic krill, and squid. They are excellent swimmers and can dive to great depths. The average life span of emperor penguin in the wild is 15 to 20 years. Emperor penguins currently breed at 61 colonies located around Antarctica, with the largest colonies in the Ross Sea and Weddell Sea. The total population size is estimated at approximately 270,000–280,000 breeding pairs or 625,000–650,000 total birds. Emperor penguin depends upon stable fast ice throughout their 8–9 month breeding season to complete the rearing of its single chick. They are the only warm-blooded Antarctic species that breeds during the austral winter and therefore uniquely adapted to its environment. Breeding colonies mainly occur on fast ice, close to the coast or closely offshore, and amongst closely packed grounded icebergs that prevent ice breaking out during the breeding season and provide shelter from the wind. Sea ice extent in the Southern Ocean has undergone considerable inter-annual variability over the last 40 years, although with much greater inter-annual variability in the five sectors than for the Southern Ocean as a whole. -
Impact of Increasing Antarctic Ice-Shelf Melting on Southern Ocean Hydrography
Journal of Glaciology, Vol. 58, No. 212, 2012 doi: 10.3189/2012JoG12J009 1191 Impact of increasing Antarctic ice-shelf melting on Southern Ocean hydrography Caixin WANG,1,2 Keguang WANG3 1Department of Physics, University of Helsinki, Helsinki, Finland E-mail: [email protected] 2Norwegian Polar Institute, Tromsø, Norway 3Norwegian Meteorological Institute, Tromsø, Norway ABSTRACT. Southern Ocean hydrography has undergone substantial changes in recent decades, concurrent with an increase in the rate of Antarctic ice-shelf melting (AISM). We investigate the impact of increasing AISM on hydrography through a twin numerical experiment, with and without AISM, using a global coupled sea-ice/ocean climate model. The difference between these simulations gives a qualitative understanding of the impact of increasing AISM on hydrography. It is found that increasing AISM tends to freshen the surface water, warm the intermediate and deep waters, and freshen and warm the bottom water in the Southern Ocean. Such effects are consistent with the recent observed trends, suggesting that increasing AISM is likely a significant contributor to the changes in the Southern Ocean. Our analyses indicate potential positive feedback between hydrography and AISM that would amplify the effect on both Southern Ocean hydrography and Antarctic ice-shelf loss caused by external factors such as changing Southern Hemisphere winds. 1. INTRODUCTION ice thermodynamic model following Semtner (1976). The 8 The Southern Ocean has undergone significant changes in model has a mean resolution of 2 in the horizontal, and recent decades (see review by Jacobs, 2006): for example, 31 vertical layers in the ocean model with grid spacing from rising temperature in the upper 3000 m (Levitus and others, 10 m in the top 100 m to 500 m at the bottom, and 1 (for 2000, 2005; Gille, 2002, 2003), and decreasing salinity in dynamics) or 3 (for thermodynamics) vertical layers in the 8 high-latitude waters (Jacobs and others, 2002; Whitworth, sea-ice model. -
Past and Future Dynamics of the Brunt Ice Shelf from Seabed Bathymetry and Ice Shelf Geometry
The Cryosphere, 13, 545–556, 2019 https://doi.org/10.5194/tc-13-545-2019 © Author(s) 2019. This work is distributed under the Creative Commons Attribution 4.0 License. Past and future dynamics of the Brunt Ice Shelf from seabed bathymetry and ice shelf geometry Dominic A. Hodgson1,2, Tom A. Jordan1, Jan De Rydt3, Peter T. Fretwell1, Samuel A. Seddon1,4, David Becker5, Kelly A. Hogan1, Andrew M. Smith1, and David G. Vaughan1 1British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB3 0ET, UK 2Department of Geography, Durham University, Durham, DH1 3LE, UK 3Department of Geography and Environmental Sciences, Faculty of Engineering and Environment, Northumbria University, Newcastle upon Tyne, UK 4Seddon Geophysical Limited, Ipswich, UK 5Physical and Satellite Geodesy, Technische Universitaet Darmstadt, Franziska-Braun-Str. 7, 64287 Darmstadt, Germany Correspondence: Dominic A. Hodgson ([email protected]) Received: 18 September 2018 – Discussion started: 28 September 2018 Revised: 10 January 2019 – Accepted: 25 January 2019 – Published: 14 February 2019 Abstract. The recent rapid growth of rifts in the Brunt Ice expected calving event causes full or partial loss of contact Shelf appears to signal the onset of its largest calving event with the bed and whether the subsequent response causes re- since records began in 1915. The aim of this study is to de- grounding within a predictable period or a loss of structural termine whether this calving event will lead to a new steady integrity resulting from properties inherited at the grounding state in which the Brunt Ice Shelf remains in contact with the line. bed, or an unpinning from the bed, which could predispose it to accelerated flow or possible break-up. -
BAS Science Summaries 2018-2019 Antarctic Field Season
BAS Science Summaries 2018-2019 Antarctic field season BAS Science Summaries 2018-2019 Antarctic field season Introduction This booklet contains the project summaries of field, station and ship-based science that the British Antarctic Survey (BAS) is supporting during the forthcoming 2018/19 Antarctic field season. I think it demonstrates once again the breadth and scale of the science that BAS undertakes and supports. For more detailed information about individual projects please contact the Principal Investigators. There is no doubt that 2018/19 is another challenging field season, and it’s one in which the key focus is on the West Antarctic Ice Sheet (WAIS) and how this has changed in the past, and may change in the future. Three projects, all logistically big in their scale, are BEAMISH, Thwaites and WACSWAIN. They will advance our understanding of the fragility and complexity of the WAIS and how the ice sheets are responding to environmental change, and contributing to global sea-level rise. Please note that only the PIs and field personnel have been listed in this document. PIs appear in capitals and in brackets if they are not present on site, and Field Guides are indicated with an asterisk. Non-BAS personnel are shown in blue. A full list of non-BAS personnel and their affiliated organisations is shown in the Appendix. My thanks to the authors for their contributions, to MAGIC for the field sites map, and to Elaine Fitzcharles and Ali Massey for collating all the material together. Thanks also to members of the Communications Team for the editing and production of this handy summary. -
Ice on Earth – Download
Ice on Earth: & By Sea By Land ce is found on every continent and ocean basin, from the highest peak in Africa to the icy North and South Poles. Almost two-thirds of all fresh water is trapped in ice. Scientists study Earth’s ice Ibecause it can affect the amount of fresh water available in our rivers, lakes, and reservoirs. Earth scientists study two types of ice on the Earth’s surface: land ice and sea ice. Land ice forms when snow piles up year after year, then gets compressed and hardens. Ice sheets and glaciers on Greenland and Antarctica hold much of our planet's land ice. Sea ice forms when sea water freezes and is found in the Arctic Ocean, the Southern Ocean around Antarctica, and other cold regions. Monitoring Ice from Space —clouds Much of Earth’s ice is found in remote and dangerous places. NASA uses sensors on satellites and airplanes to measure ice clouds— in places that are hard to visit. Satellite images also provide scientists with a global view of how ice is changing on our planet. — sea ice sea ice— Greenland Melting Ice (land ice) Light-colored surfaces that reflect more sun- light have a high albedo, IMAGE: Earth Observatory and dark surfaces that absorb more sunlight On July 11, 2011, NASA’s Terra satellite IMAGE: NASA captured this image of the north polar have a lower albedo. Ice region. Natural-color images of ice on reflects a lot of sunlight the Arctic Ocean can be compared with back into space; it has a high albedo. -
Ice Sheet Stability - Istar
Ice Sheet Stability - iSTAR Science Plan 1. Summary Limitations in our understanding of ice sheet dynamics mean that models are currently unable to adequately describe contemporary ice mass loss rates. The result is that they cannot provide confident predictions of future mass loss rates. Such predictions and their resultant impact on sea-level rise estimates are important for both climate modellers and coastal planners. The £7.4M NERC programme on Ice Sheet Stability is a response to the requirement to provide better projections of future ice sheet stability. 2. The Research Programme’s Objective The objective of this programme is to improve understanding of the key ice sheet and ocean processes that affect ice sheet stability, and to enable the incorporation of this understanding into models leading to an improved ability to predict future ice sheet behaviour. The programme will focus on the West Antarctic Ice Sheet, with an emphasis in the Amundsen Sea sector and Pine Island Glacier. 3. Scientific Background The great ice sheets of Antarctica contain major reservoirs of freshwater. Changes in these ice sheets will induce large changes in global sea level and in freshwater flux to the oceans, which in turn can affect ocean circulation and climate. Although many factors contribute to sea level rise, the Fourth Assessment Report of the Intergovernmental Panel on Climate Change identified the cryosphere as the largest source of uncertainty in predictions of future sea level rise over the 50-200 year time horizon. There is evidence from the geological record of rapid changes in sea level that imply dramatic changes in the Antarctic ice sheets. -
Ice Shelf Flubber Activity FAR 2016
How Do Ice Shelves Affect Sea Level Rise?: Using Flubber to Model Ice Shelf/Glacier Interactions Grade Level: 6 - 8 Minutes: 15 - 60 min Subject: earth science, physical science Activity type: model, lab, earth dynamics NGSS Connections: Performance Expectations: - MS-ESS2- Earth’s Systems Science and Engineering Practices: - Developing and Using Models https://upload.wikimedia.org/wikipedia/co mmons/1/10/Map-antarctica-ross-ice- shelf-red-x.png Meet the scientist: Lynn Kaluzienski is a student research scientist with the Climate Change Institute at the University of Maine. Lynn is a glaciologist and will be conducting field research and gathering data to better understand changes occurring in the Ross Ice Shelf, which happens to be the largest ice shelf in Antarctica. Using the data she collects, Lynn will develop a model to make predictions about the future of the Ross Ice Shelf and its effect on sea level rise. Follow her mission through the 4-H Follow a Researcher™ program (https://extension.umaine.edu/4h/youth/follow-a-researcher/)! What’s an ice shelf? Ice shelves are thick slabs of ice floating on water, formed by glaciers and ice sheets that flow from land towards the coastline. Ice shelves are constantly pushed out into the sea by the glaciers behind them, but instead of growing continuously into the ocean as they advance, chunks of ice shelves are broken off to form icebergs in a process called calving. Warm ocean water also causes the underside of an ice shelf to melt. Despite what you might expect, the sea level does not rise when ice shelves melt and break apart since they are already floating on the ocean surface. -
Past Ice Sheet-Seabed Interactions in the Northeastern Weddell Sea Embayment, Antarctica Jan Erik Arndt1,2, Robert D
Past ice sheet-seabed interactions in the northeastern Weddell Sea Embayment, Antarctica Jan Erik Arndt1,2, Robert D. Larter2, Claus-Dieter Hillenbrand2, Simon H. Sørli3, Matthias Forwick3, James A. Smith2, Lukas Wacker4 5 1Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research, Am Handelshafen 12, 27570 Bremerhaven, Germany 2British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, United Kingdom 3Department of Geosciences, UiT The Arctic University of Norway, Postboks 6050 Langnes, N-9037 Tromsø, Norway 4ETH Zürich, Laboratory of Ion Beam Physics, Schafmattstrasse 20, CH-8093 Zurich, Switzerland 10 Correspondence to: Jan Erik Arndt ([email protected]) Abstract. The Antarctic Ice Sheet extent in the Weddell Sea Embayment (WSE) during the Last Glacial Maximum (LGM; ca. 19-25 calibrated kiloyears before present, cal. ka BP) and its subsequent retreat from the shelf are poorly constrained, with two conflicting scenarios being discussed. Today, the modern Brunt Ice Shelf, the last remaining ice shelf in the northeastern WSE, is only pinned at a single location and recent crevasse development may lead to its rapid disintegration in the near future. We 15 investigated the seafloor morphology on the northeastern WSE shelf and discuss its implications, in combination with marine geological records, for reconstructions of the past behaviour of this sector of the East Antarctic Ice Sheet (EAIS), including ice-seafloor interactions. Our data show that an ice stream flowed through Stancomb-Wills Trough and acted as the main conduit for EAIS drainage during the LGM in this sector. Post-LGM ice-stream retreat occurred stepwise, with at least three documented grounding line still stands, and the trough had become free of grounded ice by ~10.5 cal. -
PRESS RELEASE Iceberg A-74 Calves from the Brunt Ice Shelf In
U.S. National Ice Center NOAA Satellite Operations Facility 4231 Suitland Road Suitland, MD 20746 PRESS RELEASE FOR IMMEDIATE RELEASE Contact: LT Falon Essary, NOAA [email protected] 301-817-3934 Iceberg A-74 Calves from the Brunt Ice Shelf in the Weddell Sea 01MAR20201, Suitland, MD — The U.S. National Ice Center (USNIC) has confirmed A-74 has calved from the north facing side of the Brunt Ice Shelf. The much anticipated break was first reported on the 26th of February by GPS equipment, but not confirmed until 27th of February via Sentinel-1A imagery. As of the 28th of February, the new iceberg A-74 was located at 75° 13' South, 25° 41' West and measures 30 nautical miles on its longest axis and 18 nautical miles on its widest axis. The western part of the shelf which was first identified as the next potential large iceberg to calve from Brunt due to several large crevasses running through it remains intact. A-74 was first reported by the British Antarctic Survey, and confirmed by USNIC Ice Analyst Christopher Readinger using the Sentinel-1A image shown below. Iceberg names are derived from the Antarctic quadrant in which they were originally sighted. The quadrants are divided counter-clockwise in the following manner: A = 0-90W (Bellingshausen/Weddell Sea) C = 180-90E (Western Ross Sea/Wilkesland) B = 90W-180 (Amundsen/Eastern Ross Sea) D = 90E-0 (Amery/Eastern Weddell Sea) When first sighted, an iceberg’s point of origin is documented by USNIC. The letter of the quadrant, along with a sequential number, is assigned to the iceberg. -
Draft Comprehensive Environmental Evaluation
Proposed Construction and Operation of a New Chinese Research Station, Victoria Land, Antarctica DRAFT COMPREHENSIVE ENVIRONMENTAL EVALUATION January 2014 Polar Research Institute of China Tongji University Contents CONTACT DETAILS ..................................................................................................................... 1 NON-TECHNICAL SUMMARY .................................................................................................. 2 1. Introduction ............................................................................................................................. 9 1.1 Purpose of a new station in Victoria Land................................................................................................... 9 1.2 History of Chinese Antarctic activities ...................................................................................................... 13 1.3 Scientific programs for the new station ..................................................................................................... 18 1.4 Preparation and submission of the Draft CEE ........................................................................................... 22 1.5 Laws, standards and guidelines ................................................................................................................. 22 1.5.1 International laws, standards and guidelines ................................................................................. 23 1.5.2. Chinese laws, standards and guidelines ...................................................................................... -
The Larsen Ice Shelf System, Antarctica
22–25 Sept. GSA 2019 Annual Meeting & Exposition VOL. 29, NO. 8 | AUGUST 2019 The Larsen Ice Shelf System, Antarctica (LARISSA): Polar Systems Bound Together, Changing Fast The Larsen Ice Shelf System, Antarctica (LARISSA): Polar Systems Bound Together, Changing Fast Julia S. Wellner, University of Houston, Dept. of Earth and Atmospheric Sciences, Science & Research Building 1, 3507 Cullen Blvd., Room 214, Houston, Texas 77204-5008, USA; Ted Scambos, Cooperative Institute for Research in Environmental Sciences, University of Colorado Boulder, Boulder, Colorado 80303, USA; Eugene W. Domack*, College of Marine Science, University of South Florida, 140 7th Avenue South, St. Petersburg, Florida 33701-1567, USA; Maria Vernet, Scripps Institution of Oceanography, University of California San Diego, 8622 Kennel Way, La Jolla, California 92037, USA; Amy Leventer, Colgate University, 421 Ho Science Center, 13 Oak Drive, Hamilton, New York 13346, USA; Greg Balco, Berkeley Geochronology Center, 2455 Ridge Road, Berkeley , California 94709, USA; Stefanie Brachfeld, Montclair State University, 1 Normal Avenue, Montclair, New Jersey 07043, USA; Mattias R. Cape, University of Washington, School of Oceanography, Box 357940, Seattle, Washington 98195, USA; Bruce Huber, Lamont-Doherty Earth Observatory, Columbia University, 61 US-9W, Palisades, New York 10964, USA; Scott Ishman, Southern Illinois University, 1263 Lincoln Drive, Carbondale, Illinois 62901, USA; Michael L. McCormick, Hamilton College, 198 College Hill Road, Clinton, New York 13323, USA; Ellen Mosley-Thompson, Dept. of Geography, Ohio State University, 1036 Derby Hall, 154 North Oval Mall, Columbus, Ohio 43210, USA; Erin C. Pettit#, University of Alaska Fairbanks, Dept. of Geosciences, 900 Yukon Drive, Fairbanks, Alaska 99775, USA; Craig R. -
Submarine Glacial Landform Distribution in the Central Arctic Ocean Shelf–Slope–Basin System
Downloaded from http://mem.lyellcollection.org/ by guest on September 29, 2021 Submarine glacial landform distribution in the central Arctic Ocean shelf–slope–basin system M. JAKOBSSON Department of Geological Sciences, Stockholm University, Svante Arrhenius va¨g 8, 106 91 Stockholm, Sweden (e-mail: [email protected]) The central Arctic Ocean, including its surrounding seas, extends by Batchelor & Dowdeswell (2014). They classified the troughs over an area of c. 9.5 Â 106 km2 of which c. 53% comprises shallow into three types using the characteristics of bathymetric profiles continental shelves (Jakobsson 2002) (Fig. 1a). The surface of along the trough-axis and the presence or otherwise of a bathy- this nearly land-locked polar ocean is at present dominated by a metric bulge linked to glacial sediment deposition. Several of the perennial sea-ice cover with a maximum extent every year in late identified CSTs can be traced back into one or more deep tributary February to March and a minimum in early to mid-September fjords on adjacent landmasses such as Svalbard, Ellesmere Island (Fig. 1a) (Serreze et al. 2007). Outlet glaciers producing ice- and northern Greenland. The three largest CSTs, all extending bergs that drift in the central Arctic Ocean exist on northern Green- more than 500 km in length, are the troughs of St Anna, M’Clure land, Ellesmere Island and on islands in the Barents and Kara Strait and Amundsen Gulf (Batchelor & Dowdeswell 2014) seas (Diemand 2001) (Fig. 1a). Ice shelves, although substantially (Fig. 1a, c, d). By contrast, the shallow and relatively flat continen- smaller than those found in Antarctica, presently exist in some of tal shelves of the Laptev, East Siberian and Chukchi seas lack Greenland’s fjords (Rignot & Kanagaratnam 2006), on Severnaya bathymetrically well-expressed CSTs (Fig.