decade within the 2004–50
period, for the UKMO HadCM3, and the MPI ECHAM5-r3. . . . . . . . . . . . . 28
7 Mean annual surface air temperature and total precipitation during the 1961–90
control period, and linear trends within the 1958–2001 period, for the ERA-40
reanalyses. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . 29
8 Differences between the RCM and underlying
/media/ces/2010_005_.pdf
domain and data followed by the description
of the mass balance model. Subsequently modeled mass balance will be presented along with
the evaluation of the RCM output. Finally we will discuss the relationship of modeled mass
balance and biases in the RCM data and will conclude on the suitability of the latter for future
scenarios.
2 Model Domain and Data
2.1 Model Domain
Paakitsôq is the name
/media/ces/ces_geus_paakitsoq_full_report.pdf
in
Akureyri, also 0.6°C above the mean. In Vestmannaeyjar the mean was 4.8°C, equal to the
1961-1990 mean. In the country as a whole the temperature was 0.5°C above the 1961-1990
mean, but -0.6°C below the mean of the last ten years (2005-2014).
September was the warmest month of the year in about 30 percent of the country. This is
unusual, the last time it occurred on this scale was in 1958/media/vedurstofan/utgafa/skylduskil/ved-eng-2015.pdf
fire is the largest known in Iceland, about 67 sq kilometers (6700 hectares) were burned. The squads fighting the fire managed to shield all farmhouses in the very sparsely populated area. The area will presumably recover in a few years as there is no forest there.
Reykjavík
Figure 2. Reykjavik from the air on January 23rd 2006. The headquarters of IMO are in the center of the picture
/about-imo/news/2007
fire is the largest known in Iceland, about 67 sq kilometers (6700 hectares) were burned. The squads fighting the fire managed to shield all farmhouses in the very sparsely populated area. The area will presumably recover in a few years as there is no forest there.
Reykjavík
Figure 2. Reykjavik from the air on January 23rd 2006. The headquarters of IMO are in the center of the picture
/about-imo/news/2007/
fire is the largest known in Iceland, about 67 sq kilometers (6700 hectares) were burned. The squads fighting the fire managed to shield all farmhouses in the very sparsely populated area. The area will presumably recover in a few years as there is no forest there.
Reykjavík
Figure 2. Reykjavik from the air on January 23rd 2006. The headquarters of IMO are in the center of the picture
/about-imo/news/nr/1206
fire is the largest known in Iceland, about 67 sq kilometers (6700 hectares) were burned. The squads fighting the fire managed to shield all farmhouses in the very sparsely populated area. The area will presumably recover in a few years as there is no forest there.
Reykjavík
Figure 2. Reykjavik from the air on January 23rd 2006. The headquarters of IMO are in the center of the picture
/about-imo/news/nr/1206/
the Icelandic standards in terms of population numbers and it ranges from <200 (2)
to > 10000 (7). In this way the analysis between the Icelandic volcanoes is still consistent, but
the results here shown are not directly comparable with those produced for volcanoes world-
wide as in the original formulations the population categories are designed to be valid for very
highly-inhabited regions
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
years (2005-2014).
September was the warmest month of the year in about 30 percent of the country. This is unusual, the last time it occurred on this scale was in 1958.
The annual mean was highest in Surtsey, off the Southern coast, 5.8°C, but lowest at Þverfjall (753 m a.s.l) in the Northwest, -2.2°C. Inhabited areas had the lowest annual temperature at Svartárkot, 0.8°C.
The positive deviation
/about-imo/news/nr/3273
seismographs, measuring all three components, were installed. The old seismographs were moved to Akureyri, in the north of the country, in 1954, and to Vík, south of the Mýrdalsjökull ice cap, in 1955. It then became possible to locate earthquakes of magnitude three and larger, and the number of earthquakes recorded increased considerably.
In 1958, a new recording station, equipped
/earthquakes-and-volcanism/conferences/jsr-2009/100_years/