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Snow/ice

Shutters mounted above the cooling sections serve to protect them from overhead wind, snow, ice, and hail. In addition they are also used to regulate, either manually or automatically, the flow of air across the finned tubes and thus control the process fluid outlet temperature. [Pg.46]

The primary inconvenience is the relative slowness and lack of comfort, especially during days of inclement weather. Many millions of Americans live gi eat distances from where they work. Some might consider bicycling five miles to work each day, but few live that near to work. The typical 20-or-30-mile commute makes bicycling an unrealistic option for most people. And for those who do live close to work, few are willing to brave the elements to bicycle year around. Ram, snow, ice, high winds, extreme cold, and extreme heat that are minor inconveniences in a vehicle become major inconveniences on a bicycle. Thus, for backup, bicycle riders usually must own a vehicle for had weather days, or have access to convenient mass transit. [Pg.152]

Water Solid (snow, ice), liquid (rain, condensation, standing water), vapour (relative humidity). Rain, hail, sleet or snow may have physical effects... [Pg.402]

Table IV Median Concentrations in Both Old (pre 1900) and New Antarctic and Arctic Snow/Ice (ng... Table IV Median Concentrations in Both Old (pre 1900) and New Antarctic and Arctic Snow/Ice (ng...
In seasonal snow/ice storages frozen water is stored from winter to summer, when the cold is utilized. The snow/ice can be stored indoor, on ground, in open ponds/pits and under ground, Figure 200. [Pg.349]

If snow/ice is stored indoor it is done in a more or less insulated building. In a cavern no insulation except the ground is needed. When the snow/ice is stored on ground or in ponds it is necessary with thermal insulation, henceforth denoted insulation. Both natural and artificial snow and ice may be used and there is no size limitation for snow cooling systems. This snow cooling plant in Sundsvall is an open pond with larger pieces of wood chips as thermal insulation. [Pg.349]

The basic idea of such systems is that snow/ice is stored in a more or less water tight pond where a cold carrier is cooled by the snow, to utilize the large latent heat of fusion. For comfort cooling about 90% of the extracted energy is in the phase change, i.e., the melting. The cold carrier is either circulated between the load and the snow or rejected after it has been used for cooling. [Pg.349]

There are a number of suggested and implemented ways to store the snow/ice. If the snow is stored underground it is not necessary with thermal insulation. Otherwise a more or less insulated building or insulation directly on the snow is needed. There are different types of insulations loose fill, sheets and superstructures, with different advantages and disadvantages. [Pg.363]

Both natural and artificial snow and ice may be used and there is no size or power limitation for snow cooling systems. Here the main issue is to have enough amounts of frozen water at low cost why the only relevant snow/ice distinction is the density. If natural snow or ice is too expensive or not available in enough quantity, it is possible to produce frozen water. Artificial snow/ice is made with different types of water sprayers, including snow blowers (snow guns). The production rate depends on equipment, relative air humidity, and temperatures of the air and water. [Pg.363]

The ubiquity of PCBs is indicated by their presence in environmental samples from the polar regions of air, snow, ice, water, and in living organisms (Norstrom et al. 1988 Hargrave et al. 1989 Larsson et al. 1992 Tanabe et al. 1993). The presence of PCBs in such remote areas suggests the importance of atmospheric transport. The Committee on the Assessment of Polychlorinated Biphenyls... [Pg.1236]

The permanent gases must be pumped off at the lowest position in the condenser. They are more dense than water vapor, concentrate at the bottom of the condenser and fill up the condenser housing in time. This permanent gas reduces the vapor transport to the cold surfaces and form a snow ice as can be seen in Fig. 2.17. A condenser (Fig. 2.18.1) meets these requirements in general, but other designs are possible (see Fig. 2.52 B). [Pg.143]

E. Severe weather response (snow, ice, temperature, lightning)... [Pg.145]

Placement of detectors should consider the need for protection from physical damage, weather effects (snow, icing, wind-driven rain, or dust), or direct water hose spray during an area wash down. Detector placement should also allow safe access to perform required periodic testing and inspection. Typical approaches to flammable gas detection layout are ... [Pg.247]

Ref C.W. Livingston, "Explosions in Ice , US Army Snow Ice and Permafrost Research Establishment, Technical Report 75, December I960 (Corps of Engineers, Wilmette, 111)... [Pg.247]

SIPRE Snow, Ice and Permafrost Research SOA School of Artillery... [Pg.771]

Besides liquid and solid (snow, ice) water surfaces, mineral surfaces play the most important role with respect to adsorption processes involving gaseous organic compounds in the environment. Thus, a brief description of the chemical nature of mineral surfaces is helpful to understand our subsequent discussion of such sorption phenomena. [Pg.392]

Climate, sun, wind, rain, snow, ice, grit, contaminants, humidity, ambient conditions... [Pg.8]

Figure 6.4. Block diagram of energy flows (calm 3 da 3) at the snow-ice-water interface. Figure 6.4. Block diagram of energy flows (calm 3 da 3) at the snow-ice-water interface.
The dynamic equation for nutrients B6A in the environment, where A = S snow, / ice, W water, is given by... [Pg.369]

The siccity is an effect of cold as of heat, and moisture is the principal subject on which heat and cold act. When the latter is powerful, it condenses the moisture we see it in snow, ice and hail. From this comes the fall of leaves in autumn. If the cold increases, winter succeeds, the moisture in the plants congeals, the pores close, the stalk becomes weak through lack of nourishment they finally wither. If the winter is severe, it bears the dryness even to the roots it attacks the vito-humidum and the plants perish. How can one say after this that cold is a quality of Water, since it is its enemy, and since Nature does not suffer that an Element act upon itself. One speaks, it seems to me, more correctly, when one says that the cold has burned the plants. Cold and heat bum equally, but in a different manner heat by expanding, and cold by contracting the parts of the Mixts. [Pg.40]


See other pages where Snow/ice is mentioned: [Pg.126]    [Pg.451]    [Pg.336]    [Pg.337]    [Pg.349]    [Pg.351]    [Pg.362]    [Pg.364]    [Pg.17]    [Pg.1254]    [Pg.21]    [Pg.180]    [Pg.827]    [Pg.1254]    [Pg.916]    [Pg.184]    [Pg.49]    [Pg.341]    [Pg.367]    [Pg.369]    [Pg.136]    [Pg.224]    [Pg.49]    [Pg.62]    [Pg.62]   


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Block diagram of energy flows at the snow -ice-water interface

Snow and ice

Snow and ice strata

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