United States Antarctic Research Program Field Season 1965-1966
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Multi-Decadal Surface Temperature Trends in East
MULTI-DECADAL SURFACE TEMPERATURE TRENDS IN EAST ANTARCTICA INFERRED FROM BOREHOLE FIRN TEMPERATURE MEASUREMENTS AND GEOPHYSICAL INVERSE METHODS by Atsuhiro Muto B.Sc., Chiba University, Japan, 2003 M.Sc., Chiba University, Japan, 2005 A thesis submitted to the Faculty of the Graduate School of the University of Colorado in partial fulfillment of the requirement for the degree of Doctor of Philosophy Department of Geography 2010 This thesis entitled: Multi-decadal surface temperature trends in East Antarctica inferred from borehole firn temperature measurements and geophysical inverse methods written by Atsuhiro Muto has been approved for the Department of Geography by _____________________________________ Konrad Steffen _____________________________________ Theodore A. Scambos Date _______________ The final copy of this thesis has been examined by the signatories, and we find that both the content and the form meet acceptable presentation standards of scholarly work in the above mentioned discipline. Muto, Atsuhiro (Ph.D., Geography) Multi-decadal surface temperature trends in East Antarctica inferred from borehole firn temperature measurements and geophysical inverse methods Thesis directed by Professor Konrad Steffen Abstract The climate trend of the Antarctic interior remains unclear relative to the rest of the globe because of a lack of long-term weather records. Recent studies by other authors utilizing sparse available records, satellite data, and models have estimated a significant warming trend in the near-surface air temperature in West Antarctica and weak and poorly constrained warming trend in East Antarctica for the past 50 years. In this dissertation, firn thermal profiling was used to detect multi-decadal surface temperature trends in the interior of East Antarctica where few previous records of any kind exist. -
Utilisation Des Températures De Surface MODIS Et Du
Using MODIS land surface temperatures and the Crocus snow model to understand the warm bias of ERA- Interim reanalysis at the surface in Antarctica H. Fréville, E. Brun, G. Picard, N. Tatarinova, L. Arnaud, C. Lanconelli, C. Reijmer and M. van den Broeke 7th EARSeL workshop on Land Ice and Snow February 2014 • Introduction • Data and Methods • Evaluation results ▫ LST MODIS evaluation ▫ ERA-Interim and Crocus surface temperature analysis • Conclusions Introduction Use of remote-sensed surface temperature to evaluate the quality of reanalysis and snow model outputs in Antarctica. • Limited use of satellite observations for the evaluation of surface temperature simulations • Ts can be estimated from satellite observations under clear-sky conditions using the thermal emission of the surface in the infrared • Ts is more appropriate than T2m for investigating the energy budget of a snow-covered surface : • Ts : function of the surface energy budget • T2m : diagnosis from the surface temperature and the air temperature at the lowest atmospheric vertical level • Large temperature gradients near the surface Data and method OBSERVATIONS : MODIS surface temperatures Clear-sky satellite observations Hourly data; period : 2000-2011; Resolution ~1km In situ observations 7 stations : Dome C, South Pole, Syowa, Kohnen, Plateau Station B, Pole of Inaccessibility and Princess Elisabeth. MODELS : ERA-Interim surface temperatures ERA-i Ts is derived from the energy balance equation during the forecast step of IFS (Integrated Forecast Model) 3-hourly data; period: 2000-2011; Resolution : 80 km Crocus snow model simulations SURFEX/Crocus ERA-Interim forcing data : T2m, HR2m, U10m, precipitation rate, LWdown, SWdown, Ps, extracted at 0.5° resolution 3H time step. -
Explorer's Gazette
EEXXPPLLOORREERR’’SS GAZETTE GAZETTE Published Quarterly in Pensacola, Florida USA for the Old Antarctic Explorers Association Uniting All OAEs in Perpetuating the History of U.S. Navy Involvement in Antarctica Volume 6, Issue 3 Old Antarctic Explorers Association, Inc Jul-Sep 2006 Coast Guard Cutter Polar Star at McMurdo Ice Pier Polar Star Change of Command Ceremony Compiled by Billy-Ace Baker ince the late 1970s, the 400-foot mammoths of the Coast The “J”-shaped cranes and work areas near the stern and S Guard fleet, based in Seattle, Washington, have been port side of ship give scientists the capability to do at-sea traveling north and south on their primary mission of studies in the fields of geology, vulcanology, oceanography, scientific and logistical support in both Polar Regions. Polar sea-ice physics, and other earth science disciplines. class icebreakers, the Polar Star and the Polar Sea, have a On 10 June 2006 at 10:30 a.m. in Seattle Washington, a variety of missions while operating in Polar Regions. change of command ceremony took place aboard the Coast During Antarctic deployments, their missions include Guard Cutter Polar Star at Pier 36. breaking a channel through the sea ice to McMurdo Station On 30 June, the icebreaker entered caretaker status at its in the Ross Sea. Resupply ships use the channel to bring homeport in Seattle pending a decision whether the ship will food, fuel, and other goods to McMurdo Station. In addition be decommissioned or undergo a major renovation. Polar Star serves as a scientific research platform with five See Polar Star on page 4. -
An Approach to Polar Research
Commentary ANAPPROACH TO POLAR RESEARCH* T. 0. Jones? IKE theattainment of thePoles, the development of aco-ordinated L programfor the scientific exploration of thepolar regions has not occurred overnight. In fact more than a century has passed since Matthew FontaineMaury first proposed an international scientific assaulton the unexplored parts of the earth. His contemporaries did not heed his advice and at times it has required the zeal and courage of such eminent explorers as the late Admiral RichardE. Byrd to keep the sparkof United States polar interest burning. However, only the concerted effortsof many nations could have made possible the massive programsof scientific exploration witnessed during the International Polar Years and the InternationalGeophysical Year. TheNational Science Foundation has supported specific projects in polarresearch since its establishment in 1950, includingthe study of specimens and data collections from earlier expeditions. Not until the IGY, however, did the Foundation engage in substantial financial support for arcticand antarctic research. During this period, its support of polar research was provided through a special appropriation on a project basisto areas of research not otherwise sponsored, but necessary to balance the United States research effort. The conclusion of the IGY confronted United States efforts in Antarctica with a problem. The initial success of IGY Antarctic Program in estab- lishinga sound foundation of observationalresults about the physical features of the continentwould have been impairedif the program hadcome to an abrupt end. To close the stations even for a short time would have jeopardized their value for future use and the long term research projects would have been irretrievably disrupted. -
Antarctica: at the Heart of It All
4/8/2021 Antarctica: At the heart of it all Dr. Dan Morgan Associate Dean – College of Arts & Science Principal Senior Lecturer – Earth & Environmental Sciences Vanderbilt University Osher Lifelong Learning Institute Spring 2021 Webcams for Antarctic Stations III: “Golden Age” of Antarctic Exploration • State of the world • 1910s • 1900s • Shackleton (Nimrod) • Drygalski • Scott (Terra Nova) • Nordenskjold • Amundsen (Fram) • Bruce • Mawson • Charcot • Shackleton (Endurance) • Scott (Discovery) • Shackleton (Quest) 1 4/8/2021 Scurvy • Vitamin C deficiency • Ascorbic Acid • Makes collagen in body • Limits ability to absorb iron in blood • Low hemoglobin • Oxygen deficiency • Some animals can make own ascorbic acid, not higher primates International scientific efforts • International Polar Years • 1882-83 • 1932-33 • 1955-57 • 2007-09 2 4/8/2021 Erich von Drygalski (1865 – 1949) • Geographer and geophysicist • Led expeditions to Greenland 1891 and 1893 German National Antarctic Expedition (1901-04) • Gauss • Explore east Antarctica • Trapped in ice March 1902 – February 1903 • Hydrogen balloon flight • First evidence of larger glaciers • First ice dives to fix boat 3 4/8/2021 Dr. Nils Otto Gustaf Nordenskjold (1869 – 1928) • Geologist, geographer, professor • Patagonia, Alaska expeditions • Antarctic boat Swedish Antarctic Expedition: 1901-04 • Nordenskjold and 5 others to winter on Snow Hill Island, 1902 • Weather and magnetic observations • Antarctic goes north, maps, to return in summer (Dec. 1902 – Feb. 1903) 4 4/8/2021 Attempts to make it to Snow Hill Island: 1 • November and December, 1902 too much ice • December 1902: Three meant put ashore at hope bay, try to sledge across ice • Can’t make it, spend winter in rock hut 5 4/8/2021 Attempts to make it to Snow Hill Island: 2 • Antarctic stuck in ice, January 1903 • Crushed and sinks, Feb. -
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 -
Explorer's Gazette
EEXXPPLLOORREERR’’SS GAZETTE GAZETTE Published Quarterly in Pensacola, Florida USA for the Old Antarctic Explorers Association Uniting All OAEs in Perpetuating the History of U.S. Navy Involvement in Antarctica Volume 7, Issue 2 Old Antarctic Explorers Association, Inc Apr-Jun 2007 San Diego, California Night Launch of USNS Richard E. Byrd USNS Richard E. Byrd, (T-AKE-4) Launching Ceremony Compiled by Billy-Ace Baker Laura Kissel, Byrd Polar Research Center, and OAEA President, John Lamont West, contributed to this article. HE SECOND SHIP TO BE NAMED IN HONOR OF THE region by air in May 1926. He was awarded the Medal of FAMOUS Navy polar explorer was launched on 15 Honor for the flight. Two and a half years later, Byrd began T May 2007 in San Diego, CA at the NASSCO his first expedition to Antarctica. He commanded the first Shipyard. The U.S Navy’s newest re-supply ship, flight over the South Pole on 29 November 1929. Byrd USNS Richard E. Byrd is a dry cargo/ammunition ship completed four more expeditions to the Antarctic continent designed and built by General Dynamics. The mission of the over the next 26 years, including Operation Deep Freeze in ship will be to deliver ammunition, provisions, stores, spare 1955 the IGY expedition that established seven U.S. stations parts, potable water, and petroleum products to strike groups in Antarctica . and other naval forces. Speakers at the launching ceremony included The A 1912 graduate of the U.S. Naval Academy and a Honorable Donald C. Winter, Secretary of the Navy; Naval Aviator, Byrd (1888–1957), explored the North Pole See: Byrd Launching on page 4. -
Mystery of the Third Trip Or Time Pressure Levanevskogo
Mystery of the Third trip or time pressure Levanevskogo The author-composer: Kostarev Evgeny . 2007/2008 Part 1. Start "Flying high above, and the farthest the fastest! " Battle cry of the Soviet government. Shortcut In autumn 1934 the Hero of the Soviet Union, the polar marine pilot Sigismund Alexandrovich Levanevskogo enticed by the idea Flight. He was the first in the Soviet Union, who suggested the idea of non-stop flight across the North Pole. The starting point of the route was Moscow; fit to accomplish the same in the U.S. The Soviet government in this project was received with great interest and supported the idea of non-stop transpolar flight. Of course! From Moscow to San Francisco can be reached in three ways - through the pole across the Atlantic or the Pacific Ocean. In this case, the distance will be 9,605 km, 14,000 km and 18,000 respectively. Sigismund Levanevsky Zygmunt A. Levanevsky - a very controversial figure in the history of Soviet aviation. He was born in 1902 in St. Petersburg. Levanevskogo father, a Polish worker, died when he was only 8 years old. In 1916, after graduating from three classes of the district school, Sigismund gave up teaching and went to work in a factory the company "Spring" in order to feed his family. Revolution scattered Levanevskogo the world - Sigismund in 1919, joined the Red Army, and his family moved from Petrograd. During the Civil War Levanevsky managed to get a fighter requisition, party members, eliminate gangs in Dagestan, and assistant warden 4th aeronautic squad in Petrograd. -
Event-Driven Deposition of Snow on the Antarctic Plateau: Analyzing field Measurements with SNOWPACK
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Open Access Biogeosciences Biogeosciences Discussions Open Access Open Access Climate Climate of the Past of the Past Discussions Open Access Open Access Earth System Earth System Dynamics Dynamics Discussions Open Access Geoscientific Geoscientific Open Access Instrumentation Instrumentation Methods and Methods and Data Systems Data Systems Discussions Open Access Open Access Geoscientific Geoscientific Model Development Model Development Discussions Open Access Open Access Hydrology and Hydrology and Earth System Earth System Sciences Sciences Discussions Open Access Open Access Ocean Science Ocean Science Discussions Open Access Open Access Solid Earth Solid Earth Discussions The Cryosphere, 7, 333–347, 2013 Open Access Open Access www.the-cryosphere.net/7/333/2013/ The Cryosphere doi:10.5194/tc-7-333-2013 The Cryosphere Discussions © Author(s) 2013. CC Attribution 3.0 License. Event-driven deposition of snow on the Antarctic Plateau: analyzing field measurements with SNOWPACK C. D. Groot Zwaaftink1,4, A. Cagnati2, A. Crepaz2, C. Fierz1, G. Macelloni3, M. Valt2, and M. Lehning1,4 1WSL Institute for Snow and Avalanche Research SLF, Davos, Switzerland 2ARPAV CVA, Arabba di Livinallongo, Italy 3Institute of Applied Physics – IFAC-CNR, Florence, Italy 4CRYOS, School of Architecture, Civil and Environmental Engineering, EPFL, Lausanne, Switzerland Correspondence to: C. -
Chamaecyparis Nootkatensis
This file was created by scanning the printed publication Text errors identified by the software have been corrected; however, some errors may remain. Compilers P.E. HENNON is a research plant pathologist, Forestry Sciences Laboratory, Pacific Northwest Research Station and State and Private Forestry, USDA Forest Service, 2770 Sherwood Lane, Suite 2A, Juneau, AK 99801; A.S. HARRIS was a research silviculturist (now retired), 4400 Glacier Highway, Juneau, AK 99801. Annotated Bibliography of Chamaecyparis nootkatensis RE. Hennon A.S. Harris Compilers U S Department of Agriculture Forest Service Pacific Northwest Research Station Portland, Oregon General Technical Report PNW-GTR-413 September 1997 Abstract Hennon, P.E ; Harris, A.S., comps. 1997. Annotated bibliography of Chamaecypans nootkatensis Gen Tech Rep PNW-GTR-413 Portland, OR US Department of Agriculture, Forest Service, Pacific Northwest Research Station 112 p Some 680 citations from literature treating Chamaecypans nootkatensis are listed alphabetically by author in this bibliography Most citations are followed by a short summary A subject index is included Key words Yellow-cedar, Alaska-cedar, Alaska yellow-cedar, bibliography Foreword A considerable amount of material has been published on Chamaecypans nootkatensis (D Don) Spach in the 28 years since the 1969 printing of "Alaska-cedar, a bibliography with abstracts The current bibliography is a revision and expansion of the initial 1969 publication, now out of print The original 301 citations are included here with new ones -
Radiation Climatology at Plateau Station Meteorological
Radiation Climatology at will be added to this battery of instruments in the Plateau Station coming year. It is expected that the total global and shortwave radiation for the midsummer months of December PAUL C. DALRYMPLE and LEANDER A. STROSCHEIN 1966 and January 1967 will reach new highs. On January 10, 1967, Kuhn, using the Kipp normal in- Earth Sciences Laboratory cident pyrheliometer with filters, obtained a series of U.S. Arm y Natick Laboratories readings which resulted in a computed value of 1.76 cal/cm2/min. If this is substantiated after re- The U.S. Army Natick Laboratories (NLABS) calibration of the instrument, it will be the highest conducted a radiation climatology program at Pla- known value ever obtained on Earth for normal in- teau Station throughout the 1966 winter. Mr. Mar- cident radiation. tin Sponholz, of the U.S. Weather Bureau, ESSA, was responsible for the maintenance of the instru- mentation, which Mr. Leander Stroschein of Meteorological Observations at NLABS installed during the 1965-1966 austral Palmer Station, 1965-1966 summer. Continuous measurements were made throughout the year of net and total global radia- ARTHUR S. RUNDLE tion and, throughout days with sunshine, of short- Institute of Polar Studies wave and reflected shortwave radiation. The net Ohio State University and total global radiation were measured with the so-called Funk radiometer, made in Australia, and A program of surface meteorological observations the shortwave and reflected-shortwave radiation has been conducted in conjunction with a glaciologi- were recorded by Kipp solarimeters, made in Hol- cal program at Palmer Station, Anvers Island, since land. -
Representative Surface Snow Density on the East Antarctic Plateau
The Cryosphere, 14, 3663–3685, 2020 https://doi.org/10.5194/tc-14-3663-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. Representative surface snow density on the East Antarctic Plateau Alexander H. Weinhart1, Johannes Freitag1, Maria Hörhold1, Sepp Kipfstuhl1,2, and Olaf Eisen1,3 1Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, Bremerhaven, Germany 2Physics of Ice, Climate and Earth, Niels Bohr Institute, University of Copenhagen, Copenhagen, Denmark 3Fachbereich Geowissenschaften, Universität Bremen, Bremen, Germany Correspondence: Alexander H. Weinhart ([email protected]) Received: 10 January 2020 – Discussion started: 2 March 2020 Revised: 4 September 2020 – Accepted: 21 September 2020 – Published: 5 November 2020 Abstract. Surface mass balances of polar ice sheets are es- snow density parameterizations for regions with low accu- sential to estimate the contribution of ice sheets to sea level mulation and low temperatures like the EAP. rise. Uncertain snow and firn densities lead to significant uncertainties in surface mass balances, especially in the in- terior regions of the ice sheets, such as the East Antarctic Plateau (EAP). Robust field measurements of surface snow 1 Introduction density are sparse and challenging due to local noise. Here, we present a snow density dataset from an overland traverse Various future scenarios of a warming climate as well as cur- in austral summer 2016/17 on the Dronning Maud Land rent observations in ice sheet mass balance indicate a change plateau. The sampling strategy using 1 m carbon fiber tubes in surface mass balance (SMB) of the Greenland and Antarc- covered various spatial scales, as well as a high-resolution tic ice sheets (IPCC, 2019).