Ice Wall Growth and Decay: Meteorological Analysis and Modelling

Francis Gauthier1, Michel Allard2 and Bernard Hétu1, (1)UQAR, Geography, Rimouski, QC, Canada, (2)Laval University, Quebec City, QC, Canada

Contact First Author: Francis Gauthier; francis_gauthier@uqar.ca

Previously Published Material: Recently accepted by a scientific journal (Permafrost and Periglacial Processes)

Abstract ID#: 33796

 

English Abstract:
The growth and decay of three ice walls was surveyed and analyzed during the winter of 2010-2011. Ice walls form on a cliff face due to the freezing of seeping ground water: two of the studied ice walls are on north-facing rock faces and one over a south-facing cliff. Ice walls growth and decay models were developed using meteorological data collected in their immediate surroundings and checked against growth and decay rates measured by volume changes from terrestrial LiDAR images. A complete energy balance model is first proposed and compared with two other simplified models. The first one is a temperature index or freezing degree-hours model (FDHm), and the second one is a model that combines the FDHm and the radiation heat budget (Qrad). Both models reveal that heat loss from air convection from the seeping water to the atmosphere is the dominant heat transfer flux responsible for the north-facing ice walls growth and decay. Solar radiation also plays a major role for the melting of these ice walls. The overall evolution of the south-facing ice wall is more dependent of the daily variation of Qrad. When the air temperature is cold, the ice forms mostly during the night while solar radiation favours its melting during the day.