Soil 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 afternoon evaporation in determining the course of an individual needle ice event within an event series. Bodentemperatur, Strahlungsbilanz und Bodenbewegungsdaten aus Vancouver, Kanada, werden für eine Serie von elf aufeinanderfolgenden Wachstums- und Schmelzzyk...
The frost-heave regime of lake-bottom sediments has been studied during winters 1987-88 and 1988-89 ...
It is possible to construct numerical models of the ice segregation process. However, the model is a...
Frozen soil water is important in hydrologic events because it reduces water infiltration. The prese...
Prediction of needle ice events requires an understanding of energy and water transfer between the a...
Numerous laboratory studies have indicated that thermal gradients may produce appreciable soil water...
Soil surface temperature, net radiation and surface heave are used to evaluate a computer simulation...
Environmental growth conditions and mechanisms involved in sediment transport by needle ice have his...
A series of detailed laboratory experiments have been carried out to investigate the processes of ne...
The freeze-thaw cycles are a process that dominate entire landscapes with different intensity and m...
Needle ice growth is one of the more widespread and easily visible, but less studied, climate relate...
Soil surface temperature, net radiation and surface heave are used to evaluate a computer simulation...
Ice-on date occurred significantly later over 1975–2009 at Dickie Lake, Ontario, while ice-off...
This study aims to uncover the synoptic weather circulation pattern which is associated with the occ...
Icings are common hydrological phenomena in arctic and subarctic regions. Their bodies are made up o...
Artificial ground freezing (AGF) has been applied over 150 years for mining, and was adopted for civ...
The frost-heave regime of lake-bottom sediments has been studied during winters 1987-88 and 1988-89 ...
It is possible to construct numerical models of the ice segregation process. However, the model is a...
Frozen soil water is important in hydrologic events because it reduces water infiltration. The prese...
Prediction of needle ice events requires an understanding of energy and water transfer between the a...
Numerous laboratory studies have indicated that thermal gradients may produce appreciable soil water...
Soil surface temperature, net radiation and surface heave are used to evaluate a computer simulation...
Environmental growth conditions and mechanisms involved in sediment transport by needle ice have his...
A series of detailed laboratory experiments have been carried out to investigate the processes of ne...
The freeze-thaw cycles are a process that dominate entire landscapes with different intensity and m...
Needle ice growth is one of the more widespread and easily visible, but less studied, climate relate...
Soil surface temperature, net radiation and surface heave are used to evaluate a computer simulation...
Ice-on date occurred significantly later over 1975–2009 at Dickie Lake, Ontario, while ice-off...
This study aims to uncover the synoptic weather circulation pattern which is associated with the occ...
Icings are common hydrological phenomena in arctic and subarctic regions. Their bodies are made up o...
Artificial ground freezing (AGF) has been applied over 150 years for mining, and was adopted for civ...
The frost-heave regime of lake-bottom sediments has been studied during winters 1987-88 and 1988-89 ...
It is possible to construct numerical models of the ice segregation process. However, the model is a...
Frozen soil water is important in hydrologic events because it reduces water infiltration. The prese...