domain in the eight
main cases. The periods calculated are the entire 21st century (2000–2100), the mid-
century (2041–2060), and the late-century (2081–2100). For explanation of these cases
see Table 3.
Case GCM,RCM,RCP Mid-century Late-century Entire 21st century
1 HAD,RCA4,45 .28 .27 .29
3 HAD,COSMO,45 .26 .25 .26
5 MPI,RCA4,45 .24 .16 .26
7 MPI,COSMO,45 .22 .15 .21
2 HAD,RCA4,85 .33 .41/media/vedurstofan-utgafa-2017/VI_2017_009.pdf
An ice edge was observed in the area from 67°31'N and 023°35'W to 66°41'N and 23°43'W. Westerlies were a little more prevailing in the Greenland Strait and north of Iceland than on average
/sea-ice/monthly/2010/nr/2340
influence
models using only natural forcings
models using both natural and anthropogenic forcings
observations
41
Topic 2 Causes of change
on the hydrological cycle, including the observed large-scale pat-
terns of changes in land precipitation over the 20th century. It is
more likely than not that human influence has contributed to a glo-
bal trend towards increases in area affected by drought since
/media/loftslag/IPPC-2007-ar4_syr.pdf
offshore north Iceland
1.10.2013
Two earthquakes reaching magnitude 3 and 3.2 occurred this morning at 06:14 and 07:41 offshore North Iceland, 10 km NW of Gjögurtá.
They are a part of swarm activity which has been ongoing since September 25. Roughly 1000
/about-imo/news/nr/2757
in the following locations: 80 nm WNW of Bjargtangar, 46 nm NW of Barði, 40 nm NW of Straumnes and 41 nm N of Kögur. No icebergs were to be seen near the ice edge.
On the Greenland Strait, northeasterly wind directions were dominant to begin with, and most of the month, but at the end of the month there were a few days with southwesterly wind
/sea-ice/monthly/2011/nr/2348