and Y direction. The hydraulic conductivity is adjusted in distributed
grids unlike other parameters that have one value for each sub-basin and are defined in the
control file of the model. The four snow model parameters that were adjusted were (8)
temperature threshold for rain/snow TR/S, (9) temperature threshold for snow melt T0, (10)
degree-day factor without wind consideration c1
/media/ces/2010_016.pdf
Int., 119, 277–296.
Hooper, A. (2008). A multi-temporal InSAR method incorporating both persistent
scatterer and small baseline approaches. Geophys. Res. Lett., 35, L16302, doi:
10.1029/2008GL034654.
28
Iio, Y. (1996). Depth-dependent change in the focal mechanism of shallow earthquakes:
Implications for brittle-plastic transition in a seismogenic region, J. Geophys. Res., 101,
11209–11216
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf
). Experiences of
HARMONIE at IMO. ALADIN – HIRLAM Newsletter, 1:52–63.
Seity, Y., Brousseau, P., Malardel, S., Hello, G., Bénard, P., Bouttier, F., Lac, C., and Masson, V.
(2011). The AROME-France convective-scale operational model. Mon. Wea. Rev., 139:976–
991.
Troen, I. and Petersen, E. L. (1989). European Wind Atlas. Risø National Laboratory, Roskilde,
Denmark.
WMO (2008). Guide to Meteorological
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
Q. J. R. Meteorol.
Soc., 137, 409-422.
Giesen, R. H., Andreassen, L. M., Oerlemans, J., & van den Broeke, M. R. (2014). Surface
energy balance in the ablation zone of Langfjordjøkelen, an arctic, maritime glacier in
northern Norway. J. Glaciol., 60(219), 57-70.
Seity, Y., Brousseau, P., Malardel, S., Hello, G., Bénard, P., Bouttier, F., . . . Masson, V. (2011).
The AROME-France convective-scale
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_006.pdf