2 edition of Beaufort Sea extreme wave studies assessment found in the catalog.
Beaufort Sea extreme wave studies assessment
Environmental Studies Revolving Funds (Canada)
|Statement||Alan Murray, Marc Maes ; scientific advisor, L.R. Muir.|
|Series||Environmental Studies Research Funds (Canada). Report -- 023|
|Contributions||Murray, Alan., Maes, Marc.|
|The Physical Object|
|Pagination||xii, 97 p.|
|Number of Pages||97|
Li Erikson. Li is a research oceanographer and coastal engineer with 20+ years of experience in wave and storm surge physics, nearshore processes, coastal inundation, and shoreline change; she’s been involved in Arctic work since Her academic background includes a in Environmental Engineering, in Ocean Engineering and a Ph.D. in Coastal Engineering. The Beaufort Sea (French: Mer de Beaufort) is a marginal sea of the Arctic Ocean, located north of the Northwest Territories, the Yukon, and Alaska, and west of Canada's Arctic sea is named after Sir Francis Beaufort, a Mackenzie River, the longest in Canada, empties into the Canadian part of the Beaufort Sea west of Tuktoyaktuk, which is one of the few permanent Average depth: m ( ft).
The first assessment of fish species in the Beaufort Sea wasn't done until , she said. Still, changes are hard to miss, right down to the makeup of the water. Her research interests include nearshore circulation, coastal erosion and renewable wave energy, focusing on field observations of surface waves and storm surges. Before joining ACEP in , Eloise was a Visiting Faculty of Marine and Environmental Sciences at Alaska Pacific University, where she taught oceanography and served as the Diving.
Extreme Storms Leave Coasts Vulnerable May / June Secret Gardens in the Mangroves of St. John April New Study of Pacific Sea Otter Populations and Nearshore Ecosystems March Arctic Could Face Warmer and Ice-Free Conditions Jan. / Feb. Tsunamis Generated from Outer-Rise Earthquakes December the design wave height on a totally ice-free sea are studied. A comparison between Arctic Ocean, free ice sea, extreme wave heights, permafrost melting, shore erosion 1. Introduction such as the Northstar artificial oil and gas production island in the Beaufort Sea, have also been damaged by significantly high waves. In that case during.
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Report of a study the objective of which was to develop new and definitive estimates of the extreme wave climate in the Canadian Beaufort Sea, with emphasis on offshore exploration areas in. Offshore permafrost studies, Beaufort Sea Unknown Binding – January 1, by David Moody Hopkins (Author) See all formats and editions Hide other formats and editions.
The Amazon Book Review Author interviews, book reviews, editors' picks, and more. Read it now. Enter your mobile number or email address below and we'll send you a link to Author: David Moody Hopkins.
Beaufort Sea Extreme Wave Studies Assessment Canadä January 25 20 10 3 30 25 20 3 15 3 Wind Speed (km/ hr) TOTAL THtS 66B 69 69 75 69 75 57 63 9 9 15 15 21 33 59 45 51 Wind Speed (km/hr) i-n-RS MS Hans THS Beaufort Sea extreme wave studies assessment book 53 39 45 51 Wind Speed (km/hr) THtS TOTAL PERCENT and 57 Beaufort Sea extreme waves study.
Published on: /03/01 PDF Document. SAR Sensitivities to surface gravity waves. Published on: /01/ PDF Document. Canadian Climate Centre, Wind Wave Hindcast Extremes for the West Coast of Canada.
Published on: /01/. Beaufort Sea Extreme Wave Studies Assessment (PDF, MB) MA Murray and M Maes: Waves: North: Northern Employment and Training in the Oil and Gas Industry (PDF, MB) DPA Group Inc and Intergroup Consulting Economics Limited: Frontier Social and Economic Issues.
Along the shallow Beaufort Sea coast of the Arctic Ocean, storm events during the summer are responsible for significant sediment resuspension and transport. Given the paucity of data in this difficult field area, a model has been developed to be used as a tool towards investigation of these by: generation wave model was made on a 28km grid covering much of the open waters of the Arctic and nested to a 5 km grid within the Canadian Beaufort.
Extensive validation using a series of MEDS wave measurements in water depths from 11 to 87m water depth was performed. The Beaufort Sea poses a number of special. In The Maritime Engineering Reference Book, Wind.
By tradition, the magnitude of the wind is defined by the Beaufort Scale (Admiral Beaufort, England, ). The Beaufort wind scale is based on observation of the sea, by way of a rough grouping from 1 to 12 Bft. The observed wave pattern in deep sea is related to the generating wind force.
Introduction: History of Studies leading up to the MSC-B •Murray and Maes () extreme wave climate review of year wave m • PERD hindcast of 30 severe storms for Canadian Beaufort using 2-G wave model over period ; year waves varied from 2m near shore to.
Specifically our project focused on detecting extreme sea ice features and studying the dynamics and thermodynamics of these large sea ice features. In April, Dr.
Klaus Hochheim, Dr. Greg McCullough, Anna Crawford and myself spent two weeks living in the town of Sachs Harbour, NWT and conducting helicopter based surveys of the multiyear. In Ocean Numerical Modeling, The SWAMP Group (24 authors).
Plenum Press, New York, Beaufort Sea extreme wind/wave hindcast study. Preprints of the 3RD International Workshop on Wave Hindcasting and Forecasting. Past and Future Forcing of Beaufort Sea Coastal Change Valuable information about regional wave climatology is provided by the extreme wave hindcast study conducted by Eid & Cardone () and.
The wave field in the Beaufort Sea is thus a function of the sea ice both locally, where wave growth primarily occurs in the open water between floes, and regionally, where the ice edge may. This report reviews hindcast studies undertaken to provide wave data for the Beaufort Sea and concludes that the data is limited by lack of information on winds, sea ice and ice effects on storm waves.
When ice is absent, from July to October, energy is efficiently transferred from the atmosphere to the ocean, generating near-inertial internal waves. When ice is present, from November to June, storms also cause near-inertial oscillations in the ice and mixed layer, but kinetic energy is weaker and oscillations are quickly by: Beaufort Sea extreme wind/wave hindcast study.
Preprints of the 3RD International Conference on Wave Hindcasting and Forecasting, Montreal, Quebec, May; Preprints of the 3RD International Conference on Wave Hindcasting and Forecasting, Montreal, Quebec, May 9. A modeling study of coastal circulation and landfast ice in the nearshore Beaufort and Chukchi seas using CIOM Jia Wang1, Kohei Mizobata2, Xuezhi Bai 3, Haoguo Hu, Meibing Jin4, Yanling Yu5, Moto Ikeda6, Walter Johnson7, William Perie8, and Ayumi Fujisaki3File Size: 6MB.
Vertical displacement spectra obtained near the m isobath north of the Yermak Plateau (Levine et al. ) and over the deep Beaufort Sea during the Arctic Internal Wave Experiment (AIWEX) (Levine et al. ; Levine ) show internal wave energies under drifting pack ice are nearly an order of magnitude smaller than subpolar open-ocean Cited by: II EXTREME WAVE HINDCAST STUDY II I WEATHER IV SUPERSTRUCTURE ICING V CASE STUDIES OF STORMS Page II 1.
1 EXTREME WINDS IN THE BEAUFORT SEA 1. of the particular problems involved in deriving extreme wind values. The assessment of the occurrence of strong winds at a site is normally based on the statistical analysis of.
construction of sea-crossing bridge and bridge construction. Studying the coastal bridge’s behaviour in action of extreme wave have significant meanings in design, construction and protection of it In the past decades, many important results on the research of under the extreme wave sea-crossing bridge damage were obtained.
During aerial surveys in September –, a total of live polar bears were observed with 12 (%) animals in open water, defined for purposes of this analysis as marine waters >2 km north of the Alaska Beaufort Sea coastline or associated barrier islands.
No polar bear carcasses were observed. During aerial surveys in early September,55 polar bears (Ursus maritimus) Cited by: During the s the probability of impact by an extreme ice feature, or EIF, that would generate extreme loads on a production platform in the Southern Beaufort Sea, was identified as a key design criterion.
In recent years the effects of climate change on the arctic climate and ice cover has received increasing attention.Lead development of wind and wave reanalyses for the North Atlantic Ocean and Beaufort Sea; Participates in studies of global historical marine climate trend and variability, particularly for winds, waves and marine climate indicators Projection and analysis of extreme wave climate.
J. Climate. 19(21)– Contact Val Swail.