vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 7–9
108 Reykjavík
Sara Barsotti, Veðurstofa Íslands
Sigrún Karlsdóttir, Veðursstofa Íslands
Anna María Ágústsdóttir, Landgræðslan
Björn Oddsson, Almannavarnadeild Ríkislögreglustjóra
Íris Marelsdóttir, Embætti landlæknis
Þorvaldur Þórðarson, Jarðvísindastofnun H áskólans
Þórólfur Guðnason, Embætti landlæknis
Bogi B. Björnsson, Veðurstofa Íslands
/media/vedurstofan-utgafa-2020/VI_2020_004.pdf
and precipitation (Schmidt et al., 2019), were
extended back to 1980. Glacier margins have been mapped at different times,
based on various data, the outermost margin showing the maximum extent of the glaciers
in recent centuries. The maximum was in most places reached towards the end of
the 19th century and the year 1890 is being used as a reference. An
overview of glacier variations in Iceland since
/about-imo/news/new-article-on-glacier-changes-in-iceland-over-the-past-130-years
be underlined. A cover letter to the
editor should be on a separate sheet. The
manuscript should be arranged as follow:
1.Title page, containing authors names,
affiliations and e-mail addresses. 2. Abstract
(not exceeding 300 words). 3. Main body of
the paper. 4. Reference list. 5. Figure legends
* 6. Table * 7. Figures * 8. Appendices *
Sections marked (*) are discretionary.
Titles should
/media/jar/Jokull-guidlines.pdf
(run-off, soil humidity)
Risks concerning decision making (policy risks)
303/02/2010
Illustrative map of future climate change impacts related to freshwater which threaten the
sustainable development of the affected regions. Ensemble mean change in annual runoff (%)
between present (1980–1999) and 2090–2099 for the SRES A1B emissions scenario. Areas
with blue (red) colours indicate
/media/ces/Savolainen_Ilkka_CES_2010.pdf
line shows the difference between the
years 1980–2000 and 2060–2080.
7 Discussion
It was the original idea of this work to use a mini-ensemble of climate model scenario runs
to establish a range of future scenarios of surface mass balance of the ice sheet margin at
Paakitsôq. However, it turned out that apart from two older time slice experiments where
HIRHAM4 was driven from ECHAM4/OPYC3 (cf
/media/ces/ces_geus_paakitsoq_full_report.pdf
to 36 km
(~7- 32 mi)
head2right ECHAM5 forcing
head2right CCSM3 forcing
(A1B and A2 scenarios)
HadRM
Resolution: 25 km
(~15 mi)
head2right HadCM3 forcing
Land-Atmosphere Interactions
Snow Cover Change Temperature Change
Change in winter temperature (degrees C)Change in fraction of days with snow cover
Wintertime Change from 1990s to 2050s
Salathé et al. 2008
Extreme Precipitation
Change from 1970
/media/ces/Lettenmaier_Dennis_CES_2010pdf.pdf
and a river close to the site and a lake nearby. Elevation is 65 m above sea level, distance from the sea is 26 km and distance to towns of about 1000 inhabitants is about 15 km. This is an ideal inland background station at 64oN 21oW.
Since 1980, daily sampling has been done at Írafoss, monitoring sulphur concentrations and related substances. In fact, daily sampling was done at Rjúpnahæð
/pollution-and-radiation/pollution/
Iceland twice, once going North to walk around Krafla and visit the geothermal station in the mid 1980's. For the past five months I have - daily - checked into your site and studied the data you have shared. I have spent many hours watching the video coverage - many in September are the finest fountain reports available. In November I was fitting the subsidence data with a rate curve. The earthquake
/about-imo/the-web/awards_and_press/
in the north and Reykjavík in the southwest reveals some inter-station differences.
The first cold interval, the "ice years", was the coldest of the three in the north and east, but the 1979 to 1986 was the coldest in southwestern Iceland. Figure 2 highlights this by expressing the variability as 7-year running means of temperature. We see the end of the warm period in 1965 and three cold sub
/climatology/articles/nr/1213