in the Hamon method were defined by comparison with Pennman-Monteith
ETP. Snow accumulation and melt were modelled according to a simple temperature-index ap-
proach with various thresholds defining the rain/snow fraction and snowmelt. A simple bucket
approach is used to model interception, with a leaf area index dependent storage capacity. In-
filtration of water into the soil is modelled after
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
plate spreading motion, according to the
NUVEL-1A plate motion model (DeMets et al., 1990, 1994). Using a simple screw
dislocation model to interpret GPS campaign measurements on the RP from 1993 and
1998, Hreinsdóttir et al. (2001) suggested that rifting on the peninsula occurred in pulses,
since their research indicated present accumulation of left-lateral shear strain parallel to the
peninsula
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf