Global warming impacts on rockfall frequency and magnitude due to changing frost distribution and frost cracking effectiveness

The distribution of freezing and thawing within rock masses is time varying (day to day or season to season) and controls the effectiveness of the frost cracking processes from the surface until various depths. These processes are major contributors to the development of rock instabilities. By alter...

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Vydáno v:	Earth surface processes and landforms Ročník 49; číslo 11; s. 3399 - 3418
Hlavní autoři:	Birien, Tom, Gauthier, Francis, Meloche, Francis
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Bognor Regis Wiley Subscription Services, Inc 15.09.2024
Témata:	21st century Air temperature Boreholes Climate change Depth Effectiveness Energy balance Freeze thaw cycles Freeze-thawing freeze–thaw cycle Freezing Frost frost cracking frost damage Global warming Historic temperatures Instrumentation Rock Rock falls Rock masses Rockfall Rocks Surface energy Surface energy balance Surface properties Temperature data Thawing Thermistors Weather stations
ISSN:	0197-9337, 1096-9837
On-line přístup:	Získat plný text
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