River Ice Management in North America
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Benthic Community Response to Iceberg Scouring at an Intensely Disturbed Shallow Water Site at Adelaide Island, Antarctica
Vol. 355: 85–94, 2008 MARINE ECOLOGY PROGRESS SERIES Published February 26 doi: 10.3354/meps07311 Mar Ecol Prog Ser Benthic community response to iceberg scouring at an intensely disturbed shallow water site at Adelaide Island, Antarctica Dan A. Smale*, David K. A. Barnes, Keiron P. P. Fraser, Lloyd S. Peck British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 OET, UK ABSTRACT: Disturbance is a key structuring force influencing shallow water communities at all latitudes. Polar nearshore communities are intensely disturbed by ice, yet little is known about benthic recovery following iceberg groundings. Understanding patterns of recovery following ice scour may be particularly important in the West Antarctic Peninsula region, one of the most rapidly changing marine systems on Earth. Here we present the first observations from within the Antarc- tic Circle of community recovery following iceberg scouring. Three grounded icebergs were marked at a highly disturbed site at Adelaide Island (~67° S) and the resultant scours were sampled at <1, 3, 6, 12, 18 and 30 to 32 mo following formation. Each iceberg impact was catastrophic in that it resulted in a 92 to 96% decrease in abundance compared with reference zones, but all post- scoured communities increased in similarity towards ‘undisturbed’ assemblages over time. Taxa recovered at differing rates, probably due to varying mechanisms of return to scoured areas. By the end of the study, we found no differences in abundance between scoured and reference samples for 6 out of 9 major taxonomic groups. Five pioneer species had consistently elevated abundances in scours compared with reference zones. -
Dispossessing the Algonquins of South- Eastern Ontario of Their Lands
"LAND OF WHICH THE SAVAGES STOOD IN NO PARTICULAR NEED" : DISPOSSESSING THE ALGONQUINS OF SOUTH- EASTERN ONTARIO OF THEIR LANDS, 1760-1930 MARIEE. HUITEMA A thesis submitted to the Department of Geography in conformity with the requirements for the degree of Master of Arts Queen's University Kingston, Ontario, Canada 2000 copyright O Maqke E. Huiterna, 0 11 200 1 Nationai Library 6iblioîMque nationale du Canada Acquisitions and Acquisitions et Bibliographie Senrices services bibliographiques The author has granted a non- L'auteur a accordé une licence non exclusive licence allowing the exclusive permettant à la National Library of Canada to Bibliothèque nationale du Canada de reproduce, loan, distribute or sell reproduire, prêter, distribuer ou copies of this thesis in microform, vendre des copies de cette thèse sous paper or electronic formats. la forme de microfiche/nlm, de reproduction sur papier ou sur format electronique. The author retaias ownership of the L'auteur conserve la propriété du copyright in tbis thesis. Neither the droit d'auteur qui protège cette thèse. thesis nor substantial extracts fiom it Ni la thèse ni des extraits substantiels rnay be printed or othexwise de celle-ci ne doivent être imprimés reproduced without the author's ou autrement reproduits sans son permission. autorisation. ABSTRACT Contemporary thought and current üterature have estabüshed links between unethical colonial appropriation of Native lands and the seemingly unproblematic dispossession of Native people from those lands. The principles of justification utiiized by the colonking powers were condoned by the belief that they were commandeci by God to subdue the earth and had a mandate to conquer the wildemess. -
Sea Ice Growth and Decay a Remote Sensing Perspective Sea Ice Growth & Decay
Sea Ice Growth And Decay A Remote Sensing Perspective Sea Ice Growth & Decay Add snow here Loss of Sea Ice in the Arctic Donald K. Perovich and Jacqueline A. Richter-Menge Annual Review of Marine Science 2009 1:1, 417-441 Sea Ice Remote Sensing Method Physical Property Sensor Type Geophysical Variable Passive Microwave Surface Emissivity Radiometer Sea Ice Concentration ~ 1 – 100 GHz Sea Ice Classification Sea Ice Motion Thin Sea Ice Thickness (Snow Depth) Active Microwave Backscatter SAR Sea Ice Classification Sea Ice Motion Very Thin Sea Ice Thickness Scatterometer Sea Ice Type Altimeter Sea Ice Thickness (Snow Depth) Optical Spectral Albedo Spectrometer Floe Sizes Distribution Melt Pond Coverage Melt Pond Depth Infrared Surface Emissivity Radiometer Sea Ice Surface Temperature Thin Sea Ice Thickness Laser Backscatter Altimeter Sea Ice Thickness What are the main processes of sea ice growth & decay? How do they affect sea ice remote sensing? How to observe these processes independently? Formation Redistribution Snow Surface Melt & Growth Processes Annual Cycle of Sea Ice Sea Ice Extent Area covered at least with 15% sea ice (according to passive microwave data) Long-Term Sea Ice Trends Sea Ice Extent Sea Ice Thickness Passive Microwave Time Series Submarines, Moorings, Airborne Surveys Arctic Antarctic No comparable sea ice thickness data record Sea Ice Age & Type Sea Ice Age Sea Ice Type Model with observed ice drift & concentration Passive & Active Microwave Formation Redistribution Snow Surface Melt & Growth Processes Early Sea Ice -
Frazil-Ice Nucleation by Mass-Exchange Processes at the Air- Water Interface
J ournal oIG/acio logy, V o !. 19, No. 8 1, 197 7 FRAZIL-ICE NUCLEATION BY MASS-EXCHANGE PROCESSES AT THE AIR- WATER INTERFACE By T. E. O ST E RKAMP':' (Geophysical Institute, University of Alaska, Fairbanks, A laska 99701, U .S.A. ) AosTRACT. T he physical requirem ents for proposed frazil-ice nucleati on theori es are reviewed in the light of recent observations on frazil-ice forma tion. It is concluded that sponta neous heterogeneous nucleation in a thin supercooled surface la yer of wa ter is not a via ble mechanism for frazil-ice nucleation. E fforts to observe crys ta l multiplicati on b y b order ice have n o t been successful. The mass-excha nge m echanism proposed by O sterka mp and others ( 1974) has been gen era li zed to include splashing, wind spray, bubble bursting, evapo ra tion, a nd ma teria l tha t originates a t a dista nce from the strea m (e. g. snow, frost, ice pa rticles, cold orga nic m a teria l, a nd cold soil pa rticles). I t is shown that these mass-exchange processes ca n account for frazil-ice nucleation under a wide ra nge of phys ical a nd meteorological conditions. It is suggested that secondary nuclea tion may be responsible for large frazil-ice concentra tions in streams and rivers. R EsuME. JVllcieatioll de la glace dll ''.fra zil'' par des processus d'echallges de masses a I'illlerface air ell eall. O n a rev u les conditions physiques requises pa r les theories p our la nucleation d e la glace du " frazil " a la lumicre de recentes observations sur cette forma ti on. -
Springtime Flood Risk Reduction in Rural Arctic: a Comparative Study of Interior Alaska, United States and Central Yakutia, Russia
geosciences Article Springtime Flood Risk Reduction in Rural Arctic: A Comparative Study of Interior Alaska, United States and Central Yakutia, Russia Yekaterina Y. Kontar 1,* ID , John C. Eichelberger 2, Tuyara N. Gavrilyeva 3,4 ID , Viktoria V.Filippova 5 ID , Antonina N. Savvinova 6 ID , Nikita I. Tananaev 7 ID and Sarah F. Trainor 2 1 Science Diplomacy Center, The Fletcher School of Law and Diplomacy, Tufts University, Medford, MA 02155, USA 2 International Arctic Research Center (IARC), University of Alaska Fairbanks, Fairbanks, AK 99775-7340, USA; [email protected] (J.C.E.); [email protected] (S.F.T.) 3 Institute of Engineering & Technology, North-Eastern Federal University, Yakutsk 677007, Russia; [email protected] 4 Department of Regional Economic and Social Studies, Yakutian Scientific Center of the Russian Academy of Sciences, Yakutsk 677007, Russia 5 The Institute for Humanities Research and Indigenous Studies of the North, Russian Academy of Sciences Siberian Branch, Yakutsk 677000, Russia; fi[email protected] 6 Institute of Natural Sciences, North-Eastern Federal University, Yakutsk 677000, Russia; [email protected] 7 The Melnikov Permafrost Institute, Siberian Branch of the Russian Academy of Sciences, Yakutsk 677010, Russia; [email protected] * Correspondence: [email protected]; Tel.: +1-402-450-2267 Received: 30 November 2017; Accepted: 3 March 2018; Published: 8 March 2018 Abstract: Every spring, riverine communities throughout the Arctic face flood risk. As the river ice begins to thaw and break up, ice jams—accumulation of chunks and sheets of ice in the river channel, force melt water and ice floes to back up for dozens of kilometers and flood vulnerable communities upstream. -
Airplane Icing
Federal Aviation Administration Airplane Icing Accidents That Shaped Our Safety Regulations Presented to: AE598 UW Aerospace Engineering Colloquium By: Don Stimson, Federal Aviation Administration Topics Icing Basics Certification Requirements Ice Protection Systems Some Icing Generalizations Notable Accidents/Resulting Safety Actions Readings – For More Information AE598 UW Aerospace Engineering Colloquium Federal Aviation 2 March 10, 2014 Administration Icing Basics How does icing occur? Cold object (airplane surface) Supercooled water drops Water drops in a liquid state below the freezing point Most often in stratiform and cumuliform clouds The airplane surface provides a place for the supercooled water drops to crystalize and form ice AE598 UW Aerospace Engineering Colloquium Federal Aviation 3 March 10, 2014 Administration Icing Basics Important Parameters Atmosphere Liquid Water Content and Size of Cloud Drop Size and Distribution Temperature Airplane Collection Efficiency Speed/Configuration/Temperature AE598 UW Aerospace Engineering Colloquium Federal Aviation 4 March 10, 2014 Administration Icing Basics Cloud Characteristics Liquid water content is generally a function of temperature and drop size The colder the cloud, the more ice crystals predominate rather than supercooled water Highest water content near 0º C; below -40º C there is negligible water content Larger drops tend to precipitate out, so liquid water content tends to be greater at smaller drop sizes The average liquid water content decreases with horizontal -
Snow and Ice Control Around Structures - George D
COLD REGIONS SCIENCE AND MARINE TECHNOLOGY - Snow and Ice Control Around Structures - George D. Ashton SNOW AND ICE CONTROL AROUND STRUCTURES George D. Ashton Consultant, Lebanon, NH 03766 Keywords: ice jams, ice control, flooding, snow drifting, snow loads, river ice Contents 1. Introduction 2. Nature of ice jams 2.1. Frazil Ice 2.1.1. Hanging Dams 2.1.2. Blockage of Intakes 2.2. Breakup Ice Jams 3. Control of ice jams 3.1. Frazil Ice Jams 3.2. Breakup Ice Jams 3.2.1. Ice Suppression 3.2.2. Dikes 3.2.3. Ice Booms 3.2.4. Ice Control Structures 3.2.5. Ice Removal 3.2.6. Ice Breaking 3.2.7. Ice Weakening 3.2.8. Blasting 4. Other Ice Control Techniques 4.1. Air Bubbler Systems 4.1.1. Requirements 4.1.2. Limitations 4.1.3. Operation 4.2. Other Ice Control Techniques 5. Snow control around structures 5.1. Buildings 5.1.1. Snow UNESCOLoads on Roofs – EOLSS 5.1.2. Blowing Snow 5.2. Roads 5.2.1 Snow Fences 6. Conclusion SAMPLE CHAPTERS Glossary Bibliography Biographical Sketch Summary Two main topics are treated here: control of ice jams including mitigation measures, and control of snow accumulations around structures. The nature of ice jams is described and the difference between jams formed of frazil ice and jams formed of broken ice is ©Encyclopedia of Life Support Systems (EOLSS) COLD REGIONS SCIENCE AND MARINE TECHNOLOGY - Snow and Ice Control Around Structures - George D. Ashton discussed. Also discussed are various ice control techniques used for specific problems. -
Les Fruits Du Sommet
GOÛTER LA VALLÉE Le territoire de la MRC de la Vallée-de-la-Gatineau offre une panoplie de produits agricoles locaux, frais et de qualité. Derrière ces produits se cachent des éleveurs, des maraîchers, des acériculteurs, des fermiers et des artisans passionnés, dont le travail et le savoir-faire ont de quoi nous rendre fiers. En achetant les produits de la Vallée-de- la-Gatineau, vous rendez hommage aux hommes et aux femmes qui les produisent et vous soutenez le dynamisme agricole de notre territoire. Plusieurs options s’offrent donc à vous : • Fréquentez les marchés publics ou les kiosques à la ferme à proximité • Privilégiez (ou demandez) des produits locaux au restaurant et partout où vous achetez des aliments • Mettez de la fraîcheur dans vos assiettes en privilégiant les produits locaux et saisonniers dans vos recettes • Expliquez à votre entourage les retombées de l’achat local • Et surtout, partagez votre enthousiasme pour les producteurs et les aliments d’ici ! Encourageons les producteurs de chez nous, achetons local ! PHOTOS DE LA COUVERTURE : 1) ÉRIC LABONTÉ, MAPAQ. 2) JOCELYN GALIPEAU 3) JONATHAN SAMSON 4) LINDA ROY 1 2 3 4 2 ÉVÉNEMENTS MARCHÉ AGRICOLE LES SAVEURS DE LA VALLÉE 66, rue Saint-Joseph, Gracefield Tous les vendredis de 13h à 18h du 19 juin au 28 août 2020. Courriel : [email protected] Site web : www.lessaveursdelavallee.com Marché/Market Les Saveurs de la Vallée Le Marché Les Saveurs de la Vallée est le rendez-vous hebdomadaire des épicuriens fréquentant la Vallée-de-la-Gatineau. Il a pour mission de mettre en valeur le savoir-faire des producteurs de la région, ainsi que d’offrir la possibilité de déguster des aliments de saison, frais, locaux et de qualité, le tout dans une ambiance exceptionnelle ! The Les Saveurs de la Vallée Farmer’s Market is the weekly gathering of epicureans visiting the Vallée-de-la-Gatineau. -
The Effects of Rotation and Ice Shelf Topography on Frazil-Laden Ice Shelf Water Plumes
The effects of rotation and ice shelf topography on frazil-laden ice shelf water plumes Article Published Version Holland, P. R. and Feltham, D. L. (2006) The effects of rotation and ice shelf topography on frazil-laden ice shelf water plumes. Journal of Physical Oceanography, 36 (12). pp. 2312-2327. ISSN 0022-3670 doi: https://doi.org/10.1175/JPO2970.1 Available at http://centaur.reading.ac.uk/34907/ It is advisable to refer to the publisher’s version if you intend to cite from the work. See Guidance on citing . Published version at: http://dx.doi.org/10.1175/JPO2970.1 To link to this article DOI: http://dx.doi.org/10.1175/JPO2970.1 Publisher: American Meteorological Society All outputs in CentAUR are protected by Intellectual Property Rights law, including copyright law. Copyright and IPR is retained by the creators or other copyright holders. Terms and conditions for use of this material are defined in the End User Agreement . www.reading.ac.uk/centaur CentAUR Central Archive at the University of Reading Reading’s research outputs online 2312 JOURNAL OF PHYSICAL OCEANOGRAPHY VOLUME 36 The Effects of Rotation and Ice Shelf Topography on Frazil-Laden Ice Shelf Water Plumes ϩ PAUL R. HOLLAND* AND DANIEL L. FELTHAM Centre for Polar Observation and Modelling, University College London, London, United Kingdom (Manuscript received 24 June 2005, in final form 20 April 2006) ABSTRACT A model of the dynamics and thermodynamics of a plume of meltwater at the base of an ice shelf is presented. Such ice shelf water plumes may become supercooled and deposit marine ice if they rise (because of the pressure decrease in the in situ freezing temperature), so the model incorporates both melting and freezing at the ice shelf base and a multiple-size-class model of frazil ice dynamics and deposition. -
The Riverwatch Handbook a Field Guide for Ottawa Riverkeeper’S Riverwatchers
The Riverwatch Handbook A field guide for Ottawa Riverkeeper’s Riverwatchers Ottawa Riverkeeper - Published 2015 613.321.1120 • 1-888-9KEEPER www.ottawariverkeeper.ca • @ottriverkeeper www.facebook.com/ottawa.riverkeeper This field guide is designed to help riverwatchers 1) identify aquatic phenomena and environmental concerns, 2) collect the information needed to report their observations, and 3) connect with the proper agencies and organizations with these questions and concerns. Riverwatchers should consider potential sources and causes of observed phenomena. In a river system, causes can come from activities on land (e.g. deforestation, development/construction), areas upstream, and be the result of events that have happened recently (e.g. water releases from dams, heavy rains and wind). 1. Aquatic Phenomena 1.1 Water Colour Brown Tea Colour: dissolved organic matter (i.e. decaying plant matter), algae growth, and minerals such as iron. Just as tea leaves alter the colour of the water in your tea cup, the plant material adds Red: Suspended sediment from run-off, organic matter and color to the water. and minerals such as iron. Ottawa River at Rocher Fendu. Photo: Wilderness Tours Ottawa River at Hudson, QC. Photo: Sue McLennan Brown/Cloudy Colour: Suspended Grey: Suspended sediment from runoff sediment from runoff or erosion. (typically in urban areas from streams and storm drains) Ottawa River at Hawkesbury, ON. Photo: Meaghan Murphy Gatineau River tributary, QC. Photo: Rita Jain Yellow: Some algae or tree pollen. Green/Blue-Green: Algae bloom Private lake in South Ottawa. Photo: Larry Pegg Ottawa River at Lake Timiskaming. Photo: OBVT 1.2 What’s that floating in the water? Foam: The majority of foam that we see is natural. -
2011-2012 Michigan Winter Hazards Awareness
2011-2012 Michigan Winter Hazards Awareness INSIDE THIS PACKET Governor’s Proclamation Committee for Severe Weather Awareness Contacts 2009-2010 Winter Season Review Winter Safety Tips Winter Hazards Frequently Asked Questions (FAQs) Preventing Frozen Pipes Preventing Roof Ice Dams Ice Jams/Flooding Preventing Flood Damage Flood Insurance FAQs Winter Power Outage Tips - Heat Sources Safety Portable Generator Hazards National Weather Service Offices The Michigan Committee for Severe Weather Awareness was formed in 1991 to promote safety awareness and coordinate public information efforts regarding tornadoes, lightning, flooding and winter weather. For more information visit www.mcswa.com November 2011 For more information visit www.mcswa.com November 2011 Michigan Committee for Severe Weather Awareness Rich Pollman, Chair Kevin Thomason National Weather Service State Farm Insurance 9200 White Lake Road P.O. Box 4094 White Lake, MI 48386-1126 Kalamazoo, MI 49003-4094 248/625-3309, Ext. 726 269/384-2580 [email protected] [email protected] Mary Stikeleather-Piorunek, Vice Chair Terry Jungel Lapeer County Emergency Management Michigan Sheriffs’ Association 2332 W. Genesee Street 515 N. Capitol Lapeer, MI 48446 Lansing, MI 48933 810/667-0242 517-485-3135 [email protected] [email protected] Lori Conarton, Secretary Les Thomas Insurance Institute of Michigan Michigan Dept. of Environmental Quality 334 Townsend P.O. Box 30458 525 W. Allegan Lansing, MI 48933 Lansing, MI 48909-7958 517/371-2880 517/335-3448 [email protected] [email protected] Mark Walton Terry DeDoes National Weather Service Consumers Energy 4899 South Complex Drive, S.E. 530 W. Willow Grand Rapids, MI 49512 Lansing, MI 48909-7662 616/949-0643, Ext. -
Overview of Icing Research at NASA Glenn
Overview of Icing Research at NASA Glenn Eric Kreeger NASA Glenn Research Center Icing Branch 25 February, 2013 Glenn Research Center at Lewis Field Outline • The Icing Problem • Types of Ice • Icing Effects on Aircraft Performance • Icing Research Facilities • Icing Codes Glenn Research Center at Lewis Field 2 Aircraft Icing Ground Icing Ice build-up results in significant changes to the aerodynamics of the vehicle This degrades the performance and controllability of the aircraft In-Flight Icing Glenn Research Center at Lewis Field 3 3 Aircraft Icing During an in-flight encounter with icing conditions, ice can build up on all unprotected surfaces. Glenn Research Center at Lewis Field 4 Recent Commercial Aircraft Accidents • ATR-72: Roselawn, IN; October 1994 – 68 fatalities, hull loss – NTSB findings: probable cause of accident was aileron hinge moment reversal due to an ice ridge that formed aft of the protected areas • EMB-120: Monroe, MI; January 1997 – 29 fatalities, hull loss – NTSB findings: probable cause of accident was loss-of-control due to ice contaminated wing stall • EMB-120: West Palm Beach, FL; March 2001 – 0 fatalities, no hull loss, significant damage to wing control surfaces – NTSB findings: probable cause was loss-of-control due to increased stall speeds while operating in icing conditions (8K feet altitude loss prior to recovery) • Bombardier DHC-8-400: Clarence Center, NY; February 2009 – 50 fatalities, hull loss – NTSB findings: probable cause was captain’s inappropriate response to icing condition 5 Glenn Research