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2006 General Election Results on Sugar Island
The next issue of The Sault Tribe News will be the 2005 Annual Report. We will feature reports from every department of the Tribe along with their accomplishments and funding statistics. Please be sure to read the next issue of the news. The deadline for submissions for the following issue is Aug 1. HE AULT RIBE EWS T S Visit us online at www.saulttribe.comT N (O)De'imin Giizis “Strawberry Moon” Win Awenen Nisitotung “One Who Understands” June 30 2006 • Vol. 27, No. 9 News briefs No body contact advisory 2006 General election results on Sugar Island. Close race in Unit II determined by recount As a result of high bacteria levels, specifically E. coli, on the north shore of Sugar Island, the Chippewa County Health Depart- ment has issued a no body con- tact advisory for areas near 55 N. Westshore Dr., Williams Dr., and Village Rd. People should avoid body contact with surface waters of the St. Mary's River in these areas. Chippewa County Health Department will notify the public when the no body contact advisory is lifted. Gravelle hearing rescheduled for July 5 A preliminary hearing re- garding felony drug charges New Unit III Representative Keith Massaway, center, with wife, Re-elected incumbent Dennis McKelvie congratulates new levied last May 31 against Sault Jean, and one of his sons, Andrew. board member DJ Hoffman. PHOTOS BY ALAN KAMUDA Tribe Board of Directors Unit I The Sault Tribe’s governing count was requested by Hank and their oath of office at the Sault UNOFFICIAL RESULTS Representative Todd Gravelle body will welcome three new a hand count of the votes was con- powwow on July 1. -
Forest Economy in the U.S.S.R
STUDIA FORESTALIA SUECICA NR 39 1966 Forest Economy in the U.S.S.R. An Analysis of Soviet Competitive Potentialities Skogsekonomi i Sovjet~rnionen rned en unalys av landets potentiella konkurrenskraft by KARL VIICTOR ALGTTERE SICOGSH~GSICOLAN ROYAL COLLEGE OF FORESTRY STOCKHOLM Lord Keynes on the role of the economist: "He must study the present in the light of the past for the purpose of the future." Printed in Sweden by ESSELTE AB STOCKHOLM Foreword Forest Economy in the U.S.S.R. is a special study of the forestry sector of the Soviet economy. As such it makes a further contribution to the studies undertaken in recent years to elucidate the means and ends in Soviet planning; also it attempts to assess the competitive potentialities of the U.S.S.R. in international trade. Soviet studies now command a very great interest and are being undertaken at some twenty universities and research institutes mainly in the United States, the United Kingdoin and the German Federal Republic. However, it would seem that the study of the development of the forestry sector has riot received the detailed attention given to other fields. In any case, there have not been any analytical studies published to date elucidating fully the connection between forestry and the forest industries and the integration of both in the economy as a whole. Studies of specific sections have appeared from time to time, but I have no knowledge of any previous study which gives a complete picture of the Soviet forest economy and which could faci- litate the marketing policies of the western world, being undertaken at any university or college. -
Basic Structure for 6U Mite Practices
Basic Structure for 6U Mite Practices The 6U Mite group consists of players ranging in age from 4 to 6 years old. USA Hockey recommends players take a basic learn to skate before implementing 6U practice plans. The Learn to Skate foundational program will provide the rudimentary skills needed for the 6U program. In the case of some smaller youth associations it may be necessary to group the Learn to Skate, 6U and the 8U players into practice sessions. This can still be done efficiently with proper planning and be very beneficial to all involved. Skating is a primary skill for ice hockey and although players must continue to master skating technique throughout their career, there must be a special emphasis placed on the ABC elements of skating in the early years of development. Players at the Mite age have a harder time processing technical skills instruction and their bodies lack some of the fine motor control required. At this age large muscle groups and multiple joint movements should be incorporated into the practice sessions. Agility, balance and coordination (ABC’s) on the ice surface are at the foundation of LTAD for 6U Mites. Activity volume plays a significant role in development at the 6U age group. Little kids are doers so keep instruction short and activity high. Practices have a preparatory phase followed by the main body of the practice. The main body of the practice session includes station work so that kids are developing their skills in an efficient manner. The recommended breakdown is with six stations so that there is enough variety to hold the interest of players at this age. -
THE ICE CIRCLE (Draft of 11 December 2013)
THE ICE CIRCLE (Draft of 11 December 2013) The Ice Circle’s Role The Ice Circle is a global collaborative platform encouraging and supporting a multidisciplinary response to the state and impact of rapidly changing snow and ice regimes. As necessary, it will leverage focus and funding on issues relating to ice and snow with a view to generating global awareness, profiling research outcomes and supporting local action that could reduce vulnerability to disasters, mitigate forces causing ice melt, and help peoples and communities to adapt. Impact of the Decline of Ice and Snow In the last two decades, ice and snow regimes around the globe have dramatically declined. Glaciers are disappearing, permafrost is thawing, snow cover is retreating and if the current rate of sea ice losses continues, the Arctic will soon be ice-free in summer for the first time in human history. These and other changes to ice and snow — collectively described as the cryosphere —are of concern to all of humanity by affecting global hydrological systems including oceans. The distribution of snow, ice and water plays a critical role in temperature and moisture in the Earth’s atmosphere, governing major weather patterns, regulating sea level and salinity, and dramatically impacting transportation, urban and rural settlements, commerce and geopolitics. The release of methane as a permafrost thaw will affect the global carbon balance. The retreat of ice and snow represent a particular challenge for Arctic communities and important mountain regions including the Himalayan mountains, the Tibetan plateau, the Alps, the Andes and Rockies, the East African Highlands, and the Pamir Mountains in Central Asia. -
247986.Pdf (1.300Mb)
Clim Dyn DOI 10.1007/s00382-012-1464-3 Verification of model simulated mass balance, flow fields and tabular calving events of the Antarctic ice sheet against remotely sensed observations Diandong Ren • Lance M. Leslie • Mervyn J. Lynch Received: 19 February 2012 / Accepted: 16 July 2012 Ó The Author(s) 2012. This article is published with open access at Springerlink.com Abstract The Antarctic ice sheet (AIS) has the greatest exact timing of calving and of iceberg sizes cannot be potential for global sea level rise. This study simulates AIS simulated accurately at present. A projection of the future ice creeping, sliding, tabular calving, and estimates the total mass change of the AIS is made, with SEGMENT-Ice mass balances, using a recently developed, advanced ice forced by atmospheric conditions from three different dynamics model, known as SEGMENT-Ice. SEGMENT- coupled general circulation models. The entire AIS is esti- Ice is written in a spherical Earth coordinate system. mated to be losing mass steadily at a rate of *120 km3/a at Because the AIS contains the South Pole, a projection present and this rate possibly may double by year 2100. transfer is performed to displace the pole outside of the simulation domain. The AIS also has complex ice-water- Keywords Climate change Á Ice sheet dynamics Á granular material-bedrock configurations, requiring Sea level rise Á Ice shelf calving sophisticated lateral and basal boundary conditions. Because of the prevalence of ice shelves, a ‘girder yield’ type calving scheme is activated. The simulations of present 1 Introduction surface ice flow velocities compare favorably with InSAR measurements, for various ice-water-bedrock configura- At present the Earth’s climate is in an interglacial period. -
Daffodil Society, Inc
AMERICAN DAFFODIL SOCIETY, INC. THE DAFFODIL JOURNAL Volume 31, Number 2 ' December, 1994 The Daffodil Journal ISSN 0011-5290 Quarterly Publication of the American Daffodil Society, Inc. Volume 31 December, 1994 Number 2 OFFICERS OF THE SOCIETY Marilynn Howe, President 11831 Juniette Street, Culver City, CA 90230 • 310-827-3229 Jaydee Atkins Ager, First Vice President 344 Bear Branch Road, Kathleen, GA 31047 • 912-987-9282 Bob Spotts, Second Vice President 409 Hazelnut Drive, Oakley, CA 94561 • 510-625-5526 Phyllis Hess, Secretary 3670 E. Powell Road, Westerville, OH 43081 • 614-882-5720 Joseph Stettinius, Treasurer P.O. Box 17070, Richmond, VA 23726 • 804-285-3935 Executive Director — Mary Lou Gripshover 1686 Grey Fox Trails, Milford, OH 45150 (Tel .513-248-9137) All correspondence regarding memberships, change of address, receipt of publications, supplies, ADS records, and other business matters should be addressed to the Executive Director. THE DAFFODIL JOURNAL (ISSN 0011-5290) is published quarterly (March, June, September and December) by the American Daffodil Society, Inc., 1686 Grey Fox Trails, Milford, OH 45150-1521. Second class postage paid at Milford, OH 45150-1521. POSTMASTER: Send address changes to The Daffodil Journal, 1686 Grey Fox Trails, Milford, OH 45150-1521. Membership in the Society includes a subscription. $16.00 of the dues are designated for the Journal. © 1994 American Daffodil Society, Inc. Chairman of Publications Editor, Daffodil Journal Martha Kitchens Lee Kitchens 351 Buttonwood Lane 351 Buttonwood Lane Cinnaminson, NJ 08077 Cinnaminson, NJ 08077 Tel. 609-829-6557 Tel. 609-829-6557 FAX: 609-786-1314 FAX: 609-786-1314 Articles and photographs (glossy finish for black and white, transparency fo rcolor) on daffodil culture and related subjects are invited from members of the Society. -
Université De Montréal Transformations Rédox Et Spéciation
Université de Montréal Transformations rédox et spéciation du Hg dans la neige et les eaux de surface de l’extrême arctique et de régions tempérées Alexandre Poulain Département de sciences biologiques Faculté des études supérieures Thèse présentée à la faculté des études supérieures en vue de l’obtention du grade de Philosophiae Doctor (Ph.D.) en sciences biologiques Avril 200f © copyright, Alexandre Poulain, 200f. 2zN c7ç 034 2cQ C Vt CQS Université de Montréal Direction des bibliothèques AVIS L’auteur a autorisé l’Université de Montréal à reproduire et diffuser, en totalité ou en partie, pat quelque moyen que ce soit et sut quetque support que ce soit, et exclusivement à des fins non lucratives d’enseignement et de recherche, des copies de ce mémoire ou de cette thèse. L’auteur et les coauteurs le cas échéant conservent la propriété du droit d’auteur et des droits moraux qui protègent ce document. Ni la thèse ou le mémoire, ni des extraits substantiels de ce document, ne doivent être imprimés ou autrement reproduits sans l’autorisation de l’auteur. Afin de se conformer à la Loi canadienne sur la protection des renseignements personnels, quelques formulaires secondaires, coordonnées ou signatures intégrées au texte ont pu être enlevés de ce document. Bien que cela ait pu affecter la pagination, il n’y a aucun contenu manquant. NOTICE The author of this thesis or dissertation has granted a nonexclusive license allowing Université de Montréal to reproduce and publish the document, in part or in whole, and in any format, solely for noncommercial educational and research purposes. -
Observers Guide to Sea
Observers Guide to U. S. Department of Commerce • National Oceanic and Atmospheric Administration NOAA Ocean Service • Office of Response and Restoration National Environmental Satellite, Data, and Information Service • National Ice Center U. S. Department of Commerce National Oceanic and Atmospheric Administration NOAA Ocean Service • Office of Response and Restoration National Environmental Satellite, Data, and Information Service • National Ice Center For additional information contact: NOAA Emergency Response Division 7600 Sand Point Way NE Seattle, WA 98115 response.restoration.noaa.gov This Observers’ Guide to Sea Ice was prepared by Dr. Orson P. Smith, University of Alaska Anchorage, School of Engineering for the National Oceanic and Atmospheric Administration with thanks to Kathleen Cole, Anchorage Forecast Office Ice Forecaster. It is a product of the Cook Inlet and Prince William Sound Navigation Safety and Ef- ficiency project. To order additional copies of this document, fax your request to (206) 526-6329 or e-mail [email protected]. OBSERVERS’ GUIDE TO SEA ICE Table of Contents Introduction 2 Completing an Observation Report 4 Sea Ice Observation Report Form 5 Glacier Ice Observation Report Form 6 Concentration 7 Stages of Development 11 Sea Ice Forms 16 Glacier Ice Forms 23 1 Introduction This booklet is intended for use by volunteers to report aerial, ship- board, or shoreline observations of ice conditions at sea to authorities such as the National Weather Service, National Ice Center, U.S. Coast Guard, pilots’ associations, port authorities, or other maritime interests. Emphasis here is on conditions of concern to mariners with regard to safe passage of ships. Scientific observers may wish to note additional details following guidance of the World Meteorological Organization. -
Downloaded 09/29/21 07:12 PM UTC SEPTEMBER 2012 C a N D L I S H E T a L
1182 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 29 Atmospheric Temperature and Absolute Humidity Profiles over the Beaufort Sea and Amundsen Gulf from a Microwave Radiometer LAUREN M. CANDLISH,RICHARD L. RADDATZ,MATTHEW G. ASPLIN, AND DAVID G. BARBER Centre for Earth Observation Science, University of Manitoba, Winnipeg, Manitoba, Canada (Manuscript received 11 December 2010, in final form 22 February 2012) ABSTRACT A Radiometrics MP-3000A microwave radiometric profiler (MWRP) provided high temporal resolution atmospheric profiles for temperature and absolute humidity up to 10 km, while 113 radiosondes were launched (and 68 were used in the analysis) over sea ice and the open ocean during the 2008 Circumpolar Flaw Lead System Study and the 2009 ArcticNet Cruise in the western Canadian High Arctic. The profiles were categorized by season and by the underlying sea ice concentrations. The MWRP was validated against the radiosonde data, focusing on the lower 2 km, which are generally influenced by the nature of the underlying surface. Root-mean-square (RMS) differences for temperature averaged 1.79 K through the lowest 2 km for the winter season, 1.81 K for spring, 2.51 K for summer, and 2.47 K for fall. Average biases of 10.99, 11.19, 12.13, and 12.08 K, respectively, indicate that the MWRP measurements were colder than the raobs for the lower 2 km. The RMS difference for absolute humidity averaged 0.25 g m23 in the lowest 2 km during the winter season, 0.32 g m23 for spring, 0.74 g m23 for summer, and 0.37 g m23 for fall. -
Investigation of an Ice Circle in NE Utah in Feb 2002
Report on an Ice Circle in NE Utah, February 21, 2002 National Institute for Discovery Science Las Vegas, NV July 2002 Introduction NIDS was contacted at 8:00 AM on the morning of February 21, 2002 regarding an “ice circle” that had mysteriously appeared on a ranch overnight. According to the report, at approx 7:00 AM on the morning of February 21, 2002 the circle—measuring 5 feet 9 inches in diameter—was discovered in an irrigation canal on a ranch in NE Utah. The local NIDS investigator, who is a retired deputy sheriff and an experienced tracker, was on the spot within less than an hour. The investigator immediately proceeded to take photographs (see Photos 2–5). The ice was approximately 3/4 inch thick under the circle. The circle occurred near a spot where ranch cattle frequently drink water (see Photo 2 below). According to the investigator, the nearby cattle were behaving normally when he arrived. Investigation The circle appeared to be approximately 1/4 inch deep in the ice and multiple ice shavings found around the circumference suggested it had been gouged or cut rather than melted. Close examination of the groove showed no evidence of melted ice in or around the circumference. Rather, the groove suggested a sharp instrument had been used to carve the circle. Since the construction seemed to be relatively close to a perfect circle of diameter five feet nine inches, the investigator spent the first hour laboriously studying the center of the circle from multiple angles to determine whether an implement had been used in the center to inscribe the circle. -
Anne Bevan & Jane Downes
Edited by Timo Jokela & Glen Coutts Relate North Culture, Community and Communication Edited by Timo Jokela & Glen Coutts LUP Lapland University Press Rovaniemi 2016 © 2016 Authors and the copyright holders of the images. “The peer-review label is a trademark registered by the Federation of Finnish Learned Societies (TSV). The label will indicate that the peer-review of articles and books has been performed in line with the quality and ethical criteria imposed by the academic community. The trademark owner, TSV will grant user rights to all scholarly publishers committing themselves to the terms and conditions of the label use presented on this web page.” https://www.tsv.fi/en/services/label-for-peer-reviewed-schol- arly-publications/requirements-for-use Layout & Design: Anna-Mari Nukarinen Lapland University Press PO Box 8123 FI-96101 Rovaniemi Tel +358 40 821 4242 [email protected] www.ulapland.fi/lup Rovaniemi 2016 ISBN 978-952-310-959-9 (paperback) ISBN 978-952-310-958-2 (pdf) Contents Timo Jokela & Glen Coutts Preface. 6 Iain Biggs Re-visioning “North” as an ecosophical context for creative practices ................ 12 Annamari Manninen & Mirja Hiltunen Dealing with complexity – Pupils’ representations of place in the era of Arctic Urbanization ..................... 34 Kathryn Burnett Place apart: Scotland’s north as a cultural industry of margins. 60 Irina V. Zemtsova & Valery Sharapov “Tradition that does not exist”: wood painting of Komi-ziryans (ethnographic descriptions and methods of artistic enskillement) ........................ 84 Essi Kuure, Heidi Pietarinen & Hannu Vanhanen Experimenting with Arctic social phenomena A multicultural workshop model ..... 104 Marlene Ivey Designing for Nova Scotia Gaelic cultural revitalization: Collaborating, designing & transmitting cultural meaning. -
Supplement of Geosci
Supplement of Geosci. Model Dev., 11, 1343–1375, 2018 https://doi.org/10.5194/gmd-11-1343-2018-supplement © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Supplement of LPJmL4 – a dynamic global vegetation model with managed land – Part 1: Model description Sibyll Schaphoff et al. Correspondence to: Sibyll Schaphoff ([email protected]) The copyright of individual parts of the supplement might differ from the CC BY 4.0 License. S1 Supplementary informations to the evaluation of the LPJmL4 model The here provided supplementary informations give more details to the evaluations given in Schaphoff et al.(under Revision). All sources and data used are described in detail there. Here we present ad- ditional figures for evaluating the LPJmL4 model on a plot scale for water and carbon fluxes Fig. S1 5 - S16. Here we use the standard input as described by Schaphoff et al.(under Revision, Section 2.1). Furthermore, we evaluate the model performance on eddy flux tower sites by using site specific me- teorological input data provided by http://fluxnet.fluxdata.org/data/la-thuile-dataset/(ORNL DAAC, 2011). Here the long time spin up of 5000 years was made with the input data described in Schaphoff et al.(under Revision), but an additional spin up of 30 years was conducted with the site specific 10 input data followed by the transient run given by the observation period. Comparisons are shown for some illustrative stations for net ecosystem exchange (NEE) in Fig. S17 and for evapotranspira- tion Fig. S18.