A study of time dependence during serial needle ice events

@article{Outcalt1970ASO,
  title={A study of time dependence during serial needle ice events},
  author={Samuel I. Outcalt},
  journal={Archiv f{\"u}r Meteorologie, Geophysik und Bioklimatologie, Serie A},
  year={1970},
  volume={19},
  pages={329-337}
}
  • S. Outcalt
  • Published 1 March 1970
  • Geology
  • Archiv für Meteorologie, Geophysik und Bioklimatologie, Serie A
SummarySoil surface temperature, net radiation and soil heave data during a series of eleven consecutive needle ice growth-melt cycles at Vancouver, Canada, were studied using computer-graphic techniques. A method of analyzing the morphologic evolution of a needle growth using surface temperature and soil heave data is presented. Lastly, an atmospheric-geomorphic correlation matrix derived partially from the analysis of surface temperature-heave data is used to highlight the importance of… 
Field observations of soil temperature and water tension feedback effects on needle ice nights
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The climatonomy of a needle ice event: An experiment in simulation climatology
SummarySoil surface temperature, net radiation and surface heave are used to evaluate a computer simulation of a needle ice event at Vancouver, Canada. The simulation which includes fusion and soil
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Sediment Inclusion Events During Needle Ice Growth: A Laboratory Investigation of the Role of Soil Moisture and Temperature Fluctuations
This paper reports on a series of laboratory experiments designed to determine the impact of imposed temperature and moisture variations on the inclusion of sediment within growing needle ice. The
A bibliography of needle ice
Field Observations of Soil Temperature and Water Tension Feedback Effects on Needle Ice Nights
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The global distribution of needle-ice incidence is examined through a detailed literature search which revealed more than 200 relevant studies. A comprehensive database of the 113 locatable
An evaluation of the periglacial morphology in the high Drakensberg and associated environmental implications.
Although periglacial research in the high Drakensberg and Lesotho mountains has received growing interest amongst southern African geomorphologists, little detailed , quantitative information was
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