[en] The role that climatic change may play in altering various components of the hydrologic cycle in Arctic regions is discussed. The hydrologic setting of these regions is first described, noting the importance of subsurface freezing and thawing on hydrologic pathways and the lack of incorporation of soil freezing and thawing into climate models. Major processes of interest in the relation between climate change and hydrology are the timing and magnitude of fluxes entering and leaving a basin: precipitation, evaporation and transpiration, and runoff. The active layer of the soil could be drastically increased by only a few degrees of surface warming. The natural hydrologic cycle has considerable yearly variation, tending to mask any hydrologic changes caused by climatic change. There are too many unknowns at present for an adequate prediction of the impact of climate change on the hydrologic cycle. The biggest uncertainty is how the timing and quantity of precipitation is going to change. This quantity could be altered by any major changes in vegetation, which would be closely related to the amount of warming. In hydrologic scenarios where air temperature rises 4 degree C over 50 y, under stable, high, and low precipitation conditions, there are no significant changes in hydrologic response. 24 refs., 6 figs

No abstract available

[en] Human-induced climate warming is believed to be imminent, although its exact magnitude is uncertain. Such a warming will have a dramatic effect on permafrost, which underlies about half of Canada's land mass. Adaptation of the land to climatic warming will include diminution of permafrost both in lateral and vertical extent, with concomitant responses in the landscape such as development of thermokarst, slides and slumping in hilly terrain, and altering of hydrologic regimes. Since northern development has relied on special techniques that preserve permafrost to ensure foundation stability, climatic warming will demand adjustment in engineering designs for new facilities and alteration of maintenance procedures for existing facilities. Recommendations are presented for future research, both on permafrost and its linkages to climatic and other environmental factors, and on risk analyses of engineering projects

[en] Atmospheric soundings reveal that isothermal layers at temperatures near -40C sometimes occur at high latitudes. In the absence of sufficient ice nuclei, supercooled water frozen by homogeneous freezing would act to produce such layers. The formation of such layers by homogeneous freezing should furthermore result in significant dynamic responses in the atmosphere

[en] Satellite observations show a remarkably frequent occurence of Antarctic mesocyclones in the eastern Weddell Sea close to the British station Halley in the Antarctic summer. With a quasilinear stability analysis, the dynamic features which are believed to be responsible for the mesocyclone formation have been investigated in a conceptual way. For this purpose a model package has been developed and tested consisting of a nonlinear adiabatic and hydrostatic model, which was extended from two to three dimensions. Furthermore, the package includes an algorithm which allows the model to produce linear results. The algorithm is designed to keep the disturbance values of the prognostic field variables under certain small threshold values and therefore forces the nonlinear terms to be negligible. The calculation of the most unstable solution/mode follows the concept of the time integration method introduced by Brown (1969). For the definition of the basic flows on which the instability analyses have been performed, the dynamic components were formulated as idealized fields. The studies have focussed on the two dynamic components called the 'baroclinic shear zone' and the 'katabatic flow/convergence zone'

[en] There is a need for increased development in Arctic regions for obtaining resources such as hydrocarbons and ores. Development of these resources in remote areas requires suitable transportation routes and proper attention to the environmental sensitivity of northern lands. Developing a transport route must take into account such matters as resource location, economic feasibility, type of material to be transported, length of time the route will be needed, the interest of the route to tourism, and the effect of transport on the environment. Design, construction, and maintenance of the transport route requires collection of reliable data and conformity to specifications relevant to the region concerned. Construction and maintenance in northern areas is affected by such complicated and costly factors as the short construction season, long distances for transportation of both equipment and workers, presence of permafrost, and low winter temperatures. 6 figs

[en] The amplification of climatic warming in the Arctic and the sensitivity of physical, biological, and human systems to changes in climate make the Arctic particularly vulnerable to climate changes. Large areas of the Arctic permafrost and sea ice are expected to disappear under climate warming and these changes will have considerable impacts on the natural and built environment of the north. A review is presented of some recent studies on what these impacts could be for the permafrost and sea ice environment and to identify linkages with socioeconomic activities. Terrestrial adaptation to climate change will include increases in ground temperature; melting of permafrost with consequences such as frost heave, mudslides, and substantial settlement; rotting of peat contained in permafrost areas, with subsequent emission of CO₂; increased risk of forest fire; and flooding of low-lying areas. With regard to the manmade environment, structures that will be affected include buildings, pipelines, highways, airports, mines, and railways. In marine areas, climate change will increase the ice-free period for marine transport operations and thus provide some benefit to the offshore petroleum industry. This benefit will be offset by increased wave height and period, and increased coastal erosion. The offshore industry needs to be particularly concerned with these impacts since the expected design life of industry facilities (30-60 y) is of the same order as the time frame for possible climatic changes. 18 refs., 5 figs

No abstract available

[en] With the appetite for living and dead natural resources, the political and economical interest concerning the Antarctic increases throughout the world. There are three interrelated main subjects accounting for the international interest: The shelf tectonic puzzle of the original continent of Gondwana, where the Antarctic is situated in the centre, between Australia, South Africa and South America, and the hopes concerning the existence of mineral resources under the ice of the Antarctic are based thereon. The Antarctic forms the biggest unified living space of the world. (orig.)

No abstract available