Eruption in Eyjafjallajökull
Status Report: 19:00 GMT, 28 April 2010
Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland
Compiled by: MJR / SSJ / MTG / FS / SRG / GS / KH
Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO river gauges; web
cameras of the eruption site from Vodafone, Mila, and Múlakot; IMO weather
radar measurements; information
/media/jar/Eyjafjallajokull_status_2010-04-28_IES_IMO.pdf
Eruption in Eyjafjallajökull
Status Report: 18:00 GMT, 29 April 2010
Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland
Compiled by: MJR / HB / MTG / SSJ / GS / BO
Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO river gauges; web
cameras of the eruption site from Vodafone, Mila, and Múlakot; IMO weather
radar measurements; information
/media/jar/Eyjafjallajokull_status_2010-04-29_IES_IMO.pdf
Eruption in Eyjafjallajökull
Status Report: 17:00 GMT, 30 April 2010
Icelandic Meteorological Office and Institute of Earth Sciences, University of Iceland
Compiled by: MJR / MTG / FS / GS / SSJ
Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO hydrological data; web
cameras of the eruption site from Vodafone, Mila, and Múlakot; IMO weather
radar measurements; information from
/media/jar/Eyjafjallajokull_status_2010-04-30_IES_IMO.pdf
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