Chap. 7: Building Plateau
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Dukes County Intelligencer
Journal of History of Martha’s Vineyard and the Elizabeth Islands THE DUKES COUNTY INTELLIGENCER VOL. 55, NO. 1 WINTER 2013 Left Behind: George Cleveland, George Fred Tilton & the Last Whaler to Hudson Bay Lagoon Heights Remembrances The Big One: Hurricane of ’38 Membership Dues Student ..........................................$25 Individual .....................................$55 (Does not include spouse) Family............................................$75 Sustaining ...................................$125 Patron ..........................................$250 Benefactor...................................$500 President’s Circle ......................$1000 Memberships are tax deductible. For more information on membership levels and benefits, please visit www.mvmuseum.org To Our Readers his issue of the Dukes County Intelligencer is remarkable in its diver- Tsity. Our lead story comes from frequent contributor Chris Baer, who writes a swashbuckling narrative of two of the Vineyard’s most adventur- ous, daring — and quirky — characters, George Cleveland and George Fred Tilton, whose arctic legacies continue to this day. Our second story came about when Florence Obermann Cross suggested to a gathering of old friends that they write down their childhood memories of shared summers on the Lagoon. The result is a collective recollection of cottages without electricity or water; good neighbors; artistic and intellectual inspiration; sailing, swimming and long-gone open views. This is a slice of Oak Bluffs history beyond the more well-known Cottage City and Campground stories. Finally, the Museum’s chief curator, Bonnie Stacy, has reminded us that 75 years ago the ’38 hurricane, the mother of them all, was unannounced and deadly, even here on Martha’s Vineyard. — Susan Wilson, editor THE DUKES COUNTY INTELLIGENCER VOL. 55, NO. 1 © 2013 WINTER 2013 Left Behind: George Cleveland, George Fred Tilton and the Last Whaler to Hudson Bay by Chris Baer ...................................................................................... -
Hands Across History
Hands Across History A joint newsletter for the White Sands Historical Foundation and the White Sands Pioneer Group. Volume III, Letter II May 2007 The Foundation Receives Two Donations The White Sands Historical Foundation received two generous donations recently. The first was a $10,000 check from the Raytheon Company that was presented on April 10 during a special ceremo- ny marking their 50-year assoca- tion with White Sands Missile Range. Pete Franklin, Raytheon’s vice president for Integrated Air and Missile Defense, presented the check to Jon Gibson, Foundation Treasurer during the ceremony. Also, during the ceremony, Jon assisted Dave Hawkins, Raytheon’s local rep, in unveil- ing the Raytheon brick that will anchor the expansion of the Foundation Treasurer Jon Gibson and Dave Hawkins, Director of Raytheon’s Mis- Museum’s Signature Plaza. The sion Capability at White Sands, pose beside the new custom Raytheon brick to be plaza already has hundreds of placed in the Museum Signature Plaza. Raytheon also presented the Foundation bricks in place and needs addition- with a check for $10,000 to assist in building a new Museum building. al room for growth. The addition will extend out into Missile Park along the walkway. In addition to the check and brick, Raytheon created a custom made photo- display for the museum that pictures 50 years of the company’s activity at White Sands. It is now in place in the Museum’s main hall. Raytheon has tested such systems as HAWK, THAAD, Patriot, Stinger and CLAWS at White Sands. On May 9, Jon Gibson accepted a $100 check from Linda Silvernail, Presi- dent of the White Sands Club. -
Fish Terminologies
FISH TERMINOLOGIES Monument Type Thesaurus Report Format: Hierarchical listing - class Notes: Classification of monument type records by function. -
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. -
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 -
Patrick "Rediron" Mccormick Memoir
DEEP FREEZE I AND DEEP FREEZE II, 1955 - 1957 A MEMOIR BY Patrick “Rediron” McCormick INTRODUCTION I am very proud and consider myself privileged to have taken part in Operation Deep Freeze I which occurred nearly a lifetime ago. This memoir is intended to convey my personal observations and involvement in that adventure. I have concentrated on the life and efforts at McMurdo Station and The South Pole Station because I was a Seabee and that’s where I was. McMurdo Station was then known as Williams Air Operating Facility (WilliamsAIROPFAC), The South Pole Station is now known as Amundsen-Scott South Pole Station. Those stations were and are commonly referred to as McMurdo and The Pole. Although I have entitled this my memoir, it really is the memoir of all ninety-three members of the 1956 McMurdo Station winter-over party, the finest group of men I have ever been associated with. This memoir would not be possible without having access to the Narrative Log Williams Air Operating Facility McMurdo Sound, Antarctica as written by LCDR David W. Canham Jr., USNR and Robert L. Chaudoin, YN1, USN and the South Pole Station Daily Narrative commencing October 13,1956, and ending January 20,1957, as written by LTJG Richard A. Bowers, CEC, USN. Both documents are available and can be viewed on The Antarctican Society website. According to proper U. S. Navy protocol all officers below the rank of Commander are addressed as Mister followed by their last name. Mr. Canham, the Officer in Charge at McMurdo Station, and Mr. -
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. -
19 November 1956
RADM DUFEK was feeling considerably better and appeared to have completely regained his health. VX-6Õs R5D was scheduled some five times during the day for departure, but the strong winds and low blowing scud clouds caused cancellation each time. In spite of the strong winds, the temperatures crept above the freezing mark for the first time, reaching an official figure of plus thirty-three. The low as plus nineteen. During the peak of the storm, the damaged C-124 slipped off of its wooden pilings and is once again resting on its nose. Air Force personnel made a routine inspection and did not think that much additional damage had been done. They desire to have it moved into its new position (some hundred feet ahead of where it is now) by November 25th. A message received from Little America indicates that they are not thinking in possible terms of building a substitute BYRD STATION by airdrop if the trail does not work out, a situation which now appears to be quite likely. The BEARDMORE group reported all its items retrieved now from the airdrop and 2700 gallons of AvGas left. The Sno-kitten is running and they have been able to drag the airstrip and state that it has been improved some sixty percent. The Officer-CPO meeting in the evening discussed the coming weekÕs principle items of work which included a camp cleanup, installation of the torque converter engine in the second D-8 and the initial completion of all the runway facilities. Message authority from BuPers was received to have LTJG TUCK report to the Commanding Officer, Mobile Construction Battalion (Special) for duty involving flying as a technical observer, such orders to terminate on June 30, 1957 or earlier. -
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). -
Antarctic Surface Temperatures from in Situ and Satellite Infrared Measurements, J
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | The Cryosphere Discuss., 8, 55–84, 2014 Open Access www.the-cryosphere-discuss.net/8/55/2014/ The Cryosphere TCD doi:10.5194/tcd-8-55-2014 Discussions © Author(s) 2014. CC Attribution 3.0 License. 8, 55–84, 2014 This discussion paper is/has been under review for the journal The Cryosphere (TC). Antarctic surface Please refer to the corresponding final paper in TC if available. temperature Using MODIS land surface temperatures H. Fréville et al. and the Crocus snow model to Title Page understand the warm bias of ERA-Interim Abstract Introduction reanalyses at the surface in Antarctica Conclusions References Tables Figures H. Fréville1, E. Brun1, G. Picard2, N. Tatarinova1, L. Arnaud2, C. Lanconelli4, C. Reijmer3, and M. van den Broeke3 J I 1CNRM-GAME UMR3589, Météo-France and CNRS, Toulouse, France 2University Grenoble Alpes, LGGE UMR5183, 38041 Grenoble, France J I 3 Institute for Marine and Atmospheric Research Utrecht, University of Utrecht, Utrecht, the Back Close Netherlands 4Institute of Atmospheric Sciences and Climate, Bologna, Italy Full Screen / Esc Received: 19 November 2013 – Accepted: 16 December 2013 – Published: 6 January 2014 Printer-friendly Version Correspondence to: H. Fréville ([email protected]) Interactive Discussion Published by Copernicus Publications on behalf of the European Geosciences Union. 55 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract TCD MODIS land surface temperatures in Antarctica were processed in order to produce a gridded data set at 25 km resolution, spanning the period 2000–2011 at an hourly 8, 55–84, 2014 time-step.