Symposium on the Heat Exchange at Snow and Ice Surfaces
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Symposium on the Heat Exchange at Snow and Ice Surfaces [papers] by Symposium on the Heat Exchange at Snow and Ice Surfaces Ottawa 1962.

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Published by National Research Council of Canada, Associate Committee on Soil and Snow Mechanics in Ottawa .
Written in English


  • Snow -- Thermal properties -- Congresses.,
  • Ice -- Thermal properties -- Congresses.

Book details:

Edition Notes

SeriesNational Research Council of Canada. Associate Committee on Soil and Snow Mechanics. Technical memorandum no. 78, Technical memorandum (National Research Council of Canada. Associate Committee on Soil and Snow Mechanics), no. 78.
ContributionsNational Research Council, Canada. Associate Committee on Soil and Snow Mechanics. Snow and Ice Subcommittee.
LC ClassificationsQC929.S7 S93 1962
The Physical Object
Paginationii, 86, A[1]-A2 p.
Number of Pages86
ID Numbers
Open LibraryOL4297722M
LC Control Number78326079

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  Data of four automatic weather stations (AWSs) are used to calculate the turbulent exchange of sensible heat at the Antarctic snow surface for a 4 year period (–). The AWSs are situated on the ice shelf, in the coastal/inland katabatic wind zone and on the interior plateau in Dronning Maud Land, East by: Sensible heat exchange at the Antarctic snow surface: A study with automatic weather stations Article in International Journal of Climatology 25(8) - June with 69 Reads. Four heat fluxes may be involved: at the lower surface of the layer conductive heat loss to the ice be- neath, Qc; at the upper surface of the layer, heat loss to the atmosphere by radiation, QR; evaporation, QE; and convection, by: 6. Climate and energy exchange at the snow surface in the Alpine Region of the Sierra Nevada: 1. Meteorological measurements and monitoring. change of heat content in the ice B.

INTERNATIONAL SYMPOSIUM ON SNOW SCIENCE Manali, India 5 - 10 April Prem Datt Heat exchange at snow-air interface, variation of albedo and ablation of snow pack of Western surface energy fluxes and accumulation / ablation of the Antarctic ice sheet, near Schirmacher oasis.   () Large scale heat exchange and ice production in the central Arctic, Journal of Geophysical Research, 87(c10), – CrossRef Google Scholar Omstedt, A. and Axell, L. () Modeling the variations of salinity and temperature in the large Gulfs of the Baltic Sea, Continental Shelf Resea –Cited by: The Changing Arctic Cryosphere. The International Glaciological Society will hold a Symposium on ‘The Changing Arctic Cryosphere’. The symposium will take place in Edmonton, Alberta, Canada from 18–22 August Registration and the Icebreaker will take place on Sunday 17 August. A method of estimating the rate of heat loss from water surfaces is needed for such problems as predicting frazil and surface ice formation or determining the heat required to keep ice from forming under given weather conditions. Newton's Law of cooling, which states that the rate of cooling of a body is proportional to the differenceFile Size: KB.

eventually forms an ice layer on the surface the particle has acted as a "de- position nucleus". The nucleation pro- cesses are extremely complex. An ice crystal in a cloud of water droplets grows at the expense of the droplets because the vapor pressure at the ice surface is less than that above the water surface. At temperatures con-. On average, 35% of floor traffic at the best show in snow & ice is local—within miles of the show site. 93% of exhibitors indicated interest in exhibiting at the Symposium the following year. 60% of attendees indicate the trade show as the primary reason they attend the Symposium each year. Snow & Ice. Symposium. Trade Show Dates. June , DeVos Place. Grand Rapids, MI. Page 1. II. Specific Heat and Heat of Fusion of Sea Ice in O>(» -8°C ILL Specific heat of sea ice in 0>0> -8°C The specific heat of sea ice of salinity S at temperature 0 may be written as dmbo cos = miO CiO+mbO cbo+Ao ~, (1) where miO and mbO are the masses of pure ice and of brine m one gram of sea ice atCited by: