: Significant at 90% CL
Norwegian Meteorological Institute met.no
Fokstugu (973 m.a.s.l.)
Introduction Data & Methods Results
Trends in start and end:
Significant at 99% CL
/media/ces/Dyrrdal_Anita_CES_2010.pdf
), most of the earthquakes (80%)
occur in the upper crust down to 17 km in depth, a minority (19%) in the middle crust (17-31 km) and
only a few in the lower crust 31-45 km (1%) [1]. The seismogenic layer is less than 30 km in depth.
The layer seems to be rather uniform across Fennoscandia. We suggest that the middle to lower crustal
boundary may add compositional and rheological constraints
/media/norsem/norsem_korja.pdf
to highly
negative summer balances, but also lower bw than
the average for 1949–2006. Calculated change in
specific mass balance for a ±1°C change in air tem-
perature was ±0.55 m w.e., whereas a ±10 % in-
crease in precipitation represented a change of ±
0.20 m w.e. Model results further indicated that for
a 2°C warming, the ablation season will be extend-
ed by c. 30 days and that the period
/media/ces/GA_2009_91A_4_Andreassen.pdf
-
lations for regional climate downscaling. Mon. Wea. Rev., 131, 2857–2874.
Rögnvaldsson, Ó., Jónsdóttir J. F. and Ólafsson H. 2007. Numerical simulations
of precipitation in the complex terrain of Iceland—Comparison with glaciolog-
ical and hydrological data. Meteorol. Z., 16(1), 71–85.
Sigurðsson, O., and Sigurðsson Ó. J. 1998. Afkoma nokkurra jökla á Íslandi
1992–1997 (Mass balance of a number
/media/ces/Paper-Olafur-Rognvaldsson_91.pdf