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In such climates, for example, coastal districts of Iceland, the frost penetration will be small (usually < 1 m) even if the mean temperature is within a degree or two of 0°C. In markedly continental climates, winters may be very cold, but the counteracting effect of warm summers, means that annual frost penetration will be deep only when the mean temperature is within a few degrees of 0°C. The climatic conditions associated with the deepest annual freezing and thawing are those where the mean ground temperature is around 0 °C, and the annual cycle is characterised by extremes (high continentality).

Van Everdingen (1978) used natural isotope data to study the origin of water and the freezing process of frost blisters, and Michel & Fritz (1978, 1982), Chizov et al. (1983) and Burn & Michel (1988) have examined the tritium content of natural permafrost. Since there is no other method for differentiating the relative age of ground ice masses, the use of isotope data is clearly worth further development. g. Burn et al. 1986). 6 Distribution of ground ice Although several modes of formation of ice masses in permafrost are well understood, it is often difficult to predict the nature and extent of ice in the ground.

More recently, Lorrain & Demeur (1985) used data on both hydrogen (deuterium) and oxygen isotopes from ground ice masses on Victoria Island, NWT, to infer a buried glacial origin. In very young ground ice, the amount of tritium present can also be analysed. This tritium originated from the atmospheric testing of nuclear weapons in the 1950s and 1960s, becoming incorporated into the ground water/ice system via the natural Processes of the hydrologic cycle. Tritium is one of the few viable tracers for studying the process of water movement in permafrost, for whereas dissolved solutes alter the behaviour of water below 0 °C, the isotopes of oxygen and hydrogen are directly incorporated into the water molecule.

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Collins MP1 Mobile Power Supply

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