Dedicated to YOU* My Dear Reader What Would My Humble Work Be Without YOU?
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Winter Landscapes
JANUARY 2013 Arkansas WINTER Landscapes Thanks from the Big Apple It’s a Family Thing at The Green Store On the shOres Of table rOck lake in sOuthwest MissOuri January through February 2013 FALLS LODGE DOUBLE QUEEN ROOM Double Queen Rooms in Falls Lodge feature a balcony or a patio, a Jacuzzi bath and Sleep Experience bedding. PRIVATE ONE ROOM LOG CABIN OR FALLS LODGE DELUXE KING ROOM Choose from a Private One Room Log Cabin with a wood-burning fireplace, a private deck, and an outdoor grill or a Deluxe King Room on the top floor of Falls Lodge, featuring a gas fireplace and a balcony overlooking the lake. Either accommodation will spoil you with the Sleep Experience bedding and a jetted tub. *VALID SUNDAY THROUGH THURSDAY ONLY. Not valid on current reservations, holidays or Limited groups availability. over 10. BigCedar.com 1.800.225.6343 RA01132 JANUARY 2013 CONTENTS JANUARY 2013 10 PHOTO BY GAR Y B features 32 EAN 10 Arkansas Winter Landscapes in every issue Arkansas wilderness photographer, Tim Ernst, pays homage to this season with some Arkansas winter 4 Editor’s Letter landscapes. 6 Currents 18 Hammerschmidt Receives Sidney S. McMath Public Service 7 Trivia Leadership Award 24 Capitol Buzz 20 Thanks from the Big Apple New Yorker shows 26 Doug Rye Says gratitude to Arkansas linemen 30 Healthy Living 32 Cooking with Joy 36 Reflections 38 Crossword Puzzle on the cover 39 Scenes from the Past Frozen Glory Hole 40 Let’s Eat This formation, built from layer upon layer of ice, took at least a week to develop. -
Quantification of Ikaite in Antarctic Sea
Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | The Cryosphere Discuss., 6, 505–530, 2012 www.the-cryosphere-discuss.net/6/505/2012/ The Cryosphere doi:10.5194/tcd-6-505-2012 Discussions © Author(s) 2012. CC Attribution 3.0 License. This discussion paper is/has been under review for the journal The Cryosphere (TC). Please refer to the corresponding final paper in TC if available. Quantification of ikaite in Antarctic sea ice M. Fischer1,6, D. N. Thomas2,3, A. Krell1, G. Nehrke1, J. Gottlicher¨ 4, L. Norman2, C. Riaux-Gobin5, and G. S. Dieckmann1 1Alfred Wegener Institute for Polar and Marine Reserach, Bremerhaven, Germany 2Ocean Sciences, College of Natural Sciences, Bangor University, Menai Bridge, UK 3Marine Centre, Finnish Environment Institute (SYKE), Helsinki, Finland 4Institute of Synchrotron Radiation (ISS), Synchrotron Radiation Source ANKA, Karlsruhe Institute of Technology, Eggenstein-Leopoldshafen, Germany 5USR3278, CRIOBE, CNRS-EPHE, Perpignan, France 6Faculty of Biology and Chemistry, University of Bremen, Bremen, Germany Received: 18 January 2012 – Accepted: 25 January 2012 – Published: 3 February 2012 Correspondence to: M. Fischer (michael.fi[email protected]) Published by Copernicus Publications on behalf of the European Geosciences Union. 505 Discussion Paper | Discussion Paper | Discussion Paper | Discussion Paper | Abstract Calcium carbonate precipitation in sea ice can increase pCO2 during precipitation in winter and decrease pCO2 during dissolution in spring. CaCO3 precipitation in sea ice is thought to potentially drive significant CO2 uptake by the ocean. However, little is 5 known about the quantitative spatial and temporal distribution of CaCO3 within sea ice. This is the first quantitative study of hydrous calcium carbonate, as ikaite, in sea ice and discusses its potential significance for the carbon cycle in polar oceans. -
Dr John Glen Interviewed by Paul Merchant
NATIONAL LIFE STORIES AN ORAL HISTORY OF BRITISH SCIENCE Dr John Glen Interviewed by Dr Paul Merchant C1379/26 © The British Library Board http://sounds.bl.uk This interview and transcript is accessible via http://sounds.bl.uk . © The British Library Board. Please refer to the Oral History curators at the British Library prior to any publication or broadcast from this document. Oral History The British Library 96 Euston Road London NW1 2DB United Kingdom +44 (0)20 7412 7404 [email protected] Every effort is made to ensure the accuracy of this transcript, however no transcript is an exact translation of the spoken word, and this document is intended to be a guide to the original recording, not replace it. Should you find any errors please inform the Oral History curators. © The British Library Board http://sounds.bl.uk The British Library National Life Stories Interview Summary Sheet Title Page Ref no: C1379/26 Collection title: An Oral History of British Science Interviewee’s surname: Glen Title: Dr Interviewee’s forename: John W Sex: M Occupation: Physicist Date and place of birth: 6/11/1927; Putney, London Mother’s occupation: Father’s occupation: ‘Day Publisher’, Times Newspaper Dates of recording, Compact flash cards used, tracks (from – to): 28/7/10 (track 1-3); 29/7/10 (track 4-10) Location of interview: Interviewee’s home, Birmingham Name of interviewer: Dr Paul Merchant Type of recorder: Marantz PMD661 Recording format : WAV 24 bit 48kHz Total no. of tracks: 10 Stereo Total Duration: 8:12:10 Additional material: Small collection of digitised photographs, referred to in recording. -
Park District News ………..…2 Naturalist Programs ……… 3-4
Park District News ………..…2 What’s Inside Naturalist Programs ……… 3-4 Christmas Tree Recycling …...8 Luminary Walk ……………...5 Asian Longhorned Beetle …..9-10 Thank You …………………..6 Rental Facilities ……………...11 Fall Festival ……………….....7 Park Information ……………12 Luminary Walk page 5 Park District News Chris Clingman, Director At Pattison Park you may have noticed that several large trees have been removed. These are all ash trees that have been infested by the Emerald Ash Borer. Once they infest a tree it takes about 5 years to completely kill the tree. Duke Energy contacted the Park District about several of these trees along power lines that run parallel or through park properties. In order to prevent the trees from dropping branches on the power lines, Duke has started to remove the infested ash trees. This will help prevent power outages in the area. The Park District will use the wood at Pattison Park for our maple syrup programs. Moving the wood to other locations could be very destructive, as it would help speed the spread of this destructive pest. For more information on Emerald Ash Borer visit http://ashalert.osu.edu/ Elsewhere in this newsletter you will find information on the Asian Longhorned Beetle. This pest attacks 13 different genera of trees with maples being its preferred host. The primary infestation is in the village of Bethel and Tate Township, but it has also been found in small areas of Stonelick and Monroe Townships. Both of those infestations can be linked to firewood being moved from the Bethel area to those townships. For more information on the Asian Longhorned Beetle visit www.beetlebusters.info This winter the Chilo Lock 34 Visitor Center and Museum will be closed to help save on staff and utility costs. -
East Antarctic Sea Ice in Spring: Spectral Albedo of Snow, Nilas, Frost Flowers and Slush, and Light-Absorbing Impurities in Snow
Annals of Glaciology 56(69) 2015 doi: 10.3189/2015AoG69A574 53 East Antarctic sea ice in spring: spectral albedo of snow, nilas, frost flowers and slush, and light-absorbing impurities in snow Maria C. ZATKO, Stephen G. WARREN Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA E-mail: [email protected] ABSTRACT. Spectral albedos of open water, nilas, nilas with frost flowers, slush, and first-year ice with both thin and thick snow cover were measured in the East Antarctic sea-ice zone during the Sea Ice Physics and Ecosystems eXperiment II (SIPEX II) from September to November 2012, near 658 S, 1208 E. Albedo was measured across the ultraviolet (UV), visible and near-infrared (nIR) wavelengths, augmenting a dataset from prior Antarctic expeditions with spectral coverage extended to longer wavelengths, and with measurement of slush and frost flowers, which had not been encountered on the prior expeditions. At visible and UV wavelengths, the albedo depends on the thickness of snow or ice; in the nIR the albedo is determined by the specific surface area. The growth of frost flowers causes the nilas albedo to increase by 0.2±0.3 in the UV and visible wavelengths. The spectral albedos are integrated over wavelength to obtain broadband albedos for wavelength bands commonly used in climate models. The albedo spectrum for deep snow on first-year sea ice shows no evidence of light- absorbing particulate impurities (LAI), such as black carbon (BC) or organics, which is consistent with the extremely small quantities of LAI found by filtering snow meltwater. -
Response to Review 1 V3
Dear Referee #1, Thank you very much for reviewing our manuscript and for your constructive and valuable comments and suggestions. In the following text, our response to your comments is given in blue, whereas the corresponding revisions in the main text are highlighted in red. 5 Gao et al present a study of ozone loss near the surface of an outdoor mesocosm sea ice facility in Winnipeg, Canada. The sea ice facility is unique and provides an opportunity to control the formation of the sea ice with complete exposure to the atmosphere, allowing ambient snow accumulation. The comparison of O3 levels during daytime for the UV-transmitting vs UV-blocking tubes is useful. The authors 10 attribute O3 loss at 10 cm above the sea ice surface (observed for the UV- transmitting but not UV-blocking, showing that this is a photochemical process) to reaction with bromine radicals based on their enhancement of seawater Br-, which then migrated into the snow above. My major comment is the lack of discussion of the role of NOx, which is known to be important in O3 and bromine chemistry, and 15 should be particularly important in this urban ambient study (see detailed comments below). This is particularly important because snow photochemical reactions produce NO, which can react with O3, and so disentangling this from reaction with Br is important to consider. Additionally, there is additional published literature, stated below, that is relevant and should be considered in this 20 manuscript. The role of NOx needs to be discussed in this study, as there is currently no mention of NOx in the paper. -
Seasonal Timeline for Snow-Covered Sea Ice Processes in Nunavik's
https://doi.org/10.5194/tc-2019-199 Preprint. Discussion started: 10 September 2019 c Author(s) 2019. CC BY 4.0 License. Seasonal timeline for snow-covered sea ice processes in Nunavik’s Deception Bay from TerraSAR-X and time-lapse photography Sophie Dufour-Beauséjour1,2, Anna Wendleder3, Yves Gauthier1,2, Monique Bernier1,2, Jimmy Poulin1,2, 5 Véronique Gilbert4, Juupi Tuniq5, Amélie Rouleau6, Achim Roth3 1Centre Eau Terre Environnement, Institut national de la recherche scientifique (INRS), Quebec, G1K 9A9, Canada 2Centre d’études nordiques (CEN), Université Laval, Quebec, G1V 0A6, Canada 3German Aerospace Center (DLR), Oberpfaffenhofen, 82234 Weßling, Germany 10 4Kativik Regional Government, Kuujjuaq, J0M 1C0, Canada 5Salluit, J0M 1S0, Canada 6Raglan Mine (a Glencore Company), Laval, H7S 1Z5, Canada Correspondence to: Sophie Dufour-Beauséjour ([email protected]) Abstract. Inuit have reported greater inter-annual variability in seasonal sea ice conditions. For Deception Bay (Nunavik), an area 15 prized for seal and caribou hunting, an increase in solid precipitation and a shorter snow cover period is expected in the near future. In this context, and considering ice-breaking transport in the fjord by mining companies, we monitored sea ice in the area for three seasons of ice between 2015 and 2018. This article presents a case study for the combined use of TerraSAR-X and time-lapse photography time-series in order to monitor snow-covered sea ice seasonal processes. The X-band median backscattering is shown to reproduce the seasonal evolution expected from C-band data. Two different freeze-up and breakup processes are characterized. -
Halogen Species Record Antarctic Sea Ice Extent Over Glacial-Interglacial
Review of paper : Halogen species record Antarctic sea ice extent over glacial‐interglacial periods by Spolaor et al. General Comments: This paper provides the first record ever of iodine and bromide concentrations in a deep ice core, here the recently drilled Talos Dome Antarctic ice core. The paper shows a clear antinomic behaviour between the two species across the glacial‐interglacial cycles, which the authors attribute to a combination of contrasts in sources and transport distances. While bromide is essentially of oceanic abiotic origin (marine aerosols) and often associated to frost flowers formation on thin sea ice, Iodine is produced by sympagic (sea ice hosted) algae. Following the authors, glacials therefore appear as peaks in iodine, because of larger seasonal sea ice extent, and depletions in bromide because of the larger distance of seasonal sea ice to the coast. The reverse is true for interglacials. Signal alterations at the source and during the transport are discussed and a simple model is proposed to simulate bromide depletion from source to deposition. Conclusions are drawn on the past extent of sea ice during LGM and penultimate glacial maximum. The paper is highly innovative and “at the frontier of science”. It potentially provides a promising alternative to continental ice proxies of sea ice extent such as MSA or SO4, the universality of which has been highly debated in the recent decade. The paper is well written and easy to read, even for a larger audience with limited expertise in atmospheric chemistry. Some technical improvements are suggested in the technical table below. At this stage, I have three main concerns with the paper, which I would like to see better addressed: 1. -
Crystallofolia (“Frost Flowers”)1 Through Which the Ice Ribbons Are Extruded
Below is a link to a short video of Hermit while he Crystallofolia (frost flowers) on dittany (Cunila origanoides). was the pride of the neighborhood (the photos in the numbers that we saw during our hike on this, this article were taken from this video). What will the second day of the New Year. Frost flowers are be our next rare visitor? Nature goes on! http://s13.photobucket.com/albums/a298/rockoutgrl1/ normally encountered during the first hard freezes ?action=view¤t=20100109151344.flv of fall when the ground is not yet frozen. Water in the stems of certain plants expands as a result of the freezing air temperatures, causing vertical cracks to form along the length of the stem Crystallofolia (“Frost Flowers”)1 through which the ice ribbons are extruded. The formations are rather ephemeral, usually melting or sublimating away by late morning in fall’s typically By Ted C. MacRae mild daytime temperatures. As fall progresses to winter, water stores in the plant stems become While hiking the middle stretch of the Ozark depleted after several freezes or locked up when Trail’s Wappapello Section, Rich Thoma and I the ground itself freezes, and as a result frost witnessed a bounty of crystallofolia, or “frost flowers are rarely seen later than December in flowers”. These fragile, yet exquisite formations Missouri. However, it has been a wet and mild fall are, of course, not flowers at all, nor are they true and early winter, and after an extended period of frost (which forms directly from water vapor moisture during December, Missouri was finally without first condensing), but rather are thin layers gripped by a severe cold spell with lows in the of ice that form as water is drawn from cracks in single digits and daytime highs remaining down in plant stems and freezes upon contact with cold air. -
Virginia Junior Academy of Science Proceedings
VIRGINIA JUNIOR ACADEMY OF SCIENCE PROCEEDINGS 78TH ANNUAL MEETING & RESEARCH SYMPOSIUM OLD DOMINION UNIVERSITY NORFOLK, VIRGINIA MAY 23, 2019 Animal and Human Sciences Salt Affecting Brine Shrimp Tucker Albaugh and Felix Green, Mary Ellen Henderson Middle School Our experiment tHat we were testing is How does tHe concentration of salt in water affect How many brine shrimp’s eggs Hatch and live for a day. We Had 4 different independent variables. THey were 3.5%, 2%, 5% and 6%. THe purpose of tHis experiment was to find How tHe rising salt levels of tHe ocean will affect brine shrimp and its population. We measured How many brine shrimps survived by taking tHem out of tHe Hatchery and Hand counting. We conducted tHe experiment by weigHing tHe water and tHen weigHing tHe salt to find tHe salinity. In tHe first 3 levels of salt tHe number of Brine Shrimp increased but wHen tHe shrimps were placed in 6% salinity tHey decreased. SometHing tHat we realized from studying our grapHs was tHat our data was not scattered. AnotHer tHing we realized was tHat in trial 4 tHe 5% salinity tHe most amount of shrimp Hatched (witH 69.3% Hatched). We also realized tHat tHe 2% (wHich Had a Hatch rate of 65%) and tHe 3.5% (wHich Had a Hatch rate of 66.4%) tHe number of shrimps tHat Hatched in tHe 4 trials were very similar. Our data supported our HypotHesis was supported until we reached 6% salt (only 61% Hatched). Our experiment can relate to tHe information we already knew because brine Shrimp are exceptionally tolerant to HigH levels of salt in tHe water. -
Micrometeorological and Thermal Control of Frost Flower Growth and Decay on Young Sea Ice Ryan J
ARCTIC VOL. 68, NO. 1 (MARCH 2015) P. 79 – 92 http://dx.doi.org/10.14430/arctic4457 Micrometeorological and Thermal Control of Frost Flower Growth and Decay on Young Sea Ice Ryan J. Galley,1,2 Brent G.T. Else,1 Nicolas-Xavier Geilfus,1,4 Alexander A. Hare,1 David Babb,1 Tim Papakyriakou,1 David G. Barber1 and Søren Rysgaard1,3,4 (Received 22 April 2014; accepted in revised form 20 June 2014) ABSTRACT. Frost flowers are transient crystal structures that form on new and young sea ice surfaces. They have been implicated in a variety of biological, chemical, and physical processes and interactions with the atmosphere at the sea ice surface. We describe the atmospheric and radiative conditions and the physical and thermal properties of the sea ice and atmosphere that form, decay, and destroy frost flowers on young sea ice. Frost flower formation occurred during a high-pressure system that caused air temperatures to drop to −30˚C, with relative humidity of 70% (an undersaturated atmosphere), and very calm wind conditions. The sea ice surface temperature at the time of frost flower initiation was 10˚ – 13˚C warmer than the air temperature. Frost flowers grew on nodules raised above the mean surface height by 5 mm, which were ˚4 – 6˚C colder than the bare, brine-wetted, highly saline sea ice surface that provided the necessary moisture. The cold nodules created potential water vapour supersaturation zones above them with respect to air over the brine skim. Frost flowers formed and grew overnight in the absence of shortwave radiation, while the net longwave radiation was negative and dominated the net all-wave radiation balance at the surface. -
Surface-Based Ku- and Ka-Band Polarimetric Radar for Sea Ice Studies
https://doi.org/10.5194/tc-2020-151 Preprint. Discussion started: 3 August 2020 c Author(s) 2020. CC BY 4.0 License. Surface-Based Ku- and Ka-band Polarimetric Radar for Sea Ice Studies Julienne Stroeve1,2,3, Vishnu Nandan1, Rosemary Willatt2, Rasmus Tonboe4, Stefan Hendricks5, Robert 5 Ricker5, James Mead6, Marcus Huntemann5,7, Polona Itkin8, Martin Schneebeli9, Daniela Krampe5, Gunnar Spreen7, Jeremy Wilkinson10, Ilkka Matero5, Mario Hoppmann5, Robbie Mallett2 and Michel Tsamados2 1University of Manitoba, Centre for Earth Observation Science, 535 Wallace Building, Winnipeg, MB, R3T 2N2, Canada 10 2University College London, Earth Science Department, Gower Street, WC1E 6BT, UK 3National Snow and Ice Data Center, University of Colorado, 1540 30th Street, Boulder, CO 80302, USA 4Danish Meteorological Institute, Lyngbyvej 100, 2100 Copenhagen, Denmark 5Alfred Wegener Institute, Am Handelshafen 12, 27570 Bremerhaven, Germany 6ProSensing, 107 Sunderland Road, Amherst, MA, 01002-1357, USA 15 7Institute of Environmental Physics, University of Bremen, Otto-Hahn-Allee 1, D-28359 Bremen, Germany 8UiT The Arctic University of Norway, Department of Physics and Technology, Tromsø, 9019, Norway 9WSL Institute for Snow and Avalanche Research SLF, Fluelastrasse 11, CH-7260 Davos Dorf, Switzerland 10British Antarctic Survey, High Cross, Madingley Road, Cambridge, CB30ET, UK 20 *Correspondence to: Julienne Stroeve ([email protected]) Abstract. To improve our understanding of how snow properties influence sea ice thickness retrievals from presently operational and upcoming satellite radar altimeter missions, as well as investigating the potential for combining dual frequencies to simultaneously map snow depth and sea ice thickness, a new, surface-based, fully-polarimetric Ku- and Ka- 25 band radar (KuKa radar) was built and deployed during the 2019-2020 year-long MOSAiC International Arctic drift expedition.