Abstract
Monitoring of rock-face temperatures at various points within an arctic nivation site indicate that there is great variation in number, duration, and amplitude of freeze-thaw cycles experienced. Th...
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
