. Framhlaupsjöklar eru ekki taldir með. Myndin sýnir gögn frá til jökul-sporð um fyrir est ár.
The annual proportion of moni to ed
non-surging Icelandic glacier termini that
ad vanc ed or retreated in the period to . The gure is based on data from
to glaciers for most years.
Síðan um aldamótin hafa skipst á köld og hlý tímabil í veðurfari á Íslandi eins og sjá
/media/Eplicanámskeið/VAT_newsletter_2018_06.pdf
Wednesday (18.03) to review the
latest data.The deformation is occurring in the
same location as before, but at a slower rate. The uplift started in January
and halted temporarily at the end of February. The most recent data show that
since the beginning of March the uplift is about 20 mm. “The deformation now
seems to be quite slow, slower than in January. Indeed, 20 mm is a small uplift
/about-imo/news/continued-inflation-around-mt-thorbjorn
and in a
brief written report at the end of the course. A break-out group is composed of 2-3 students.
Imagine that the group is part of a policy agency responsible for designing a long term (20 years) planning process that should enable the society to cope with
the climate change effects and its uncertainties allowing sufficiently robust and flexible management practices. We would then ask
/media/vedurstofan/NONAM-PhD_program.pdf
parameters
– In the light of climate change
Norwegian Meteorological Institute met.no
Observed changes in Norway between
1961-90 and 1979-08
• Winter precipitation has
increased by 5-25 %
• Winter temperature has
increased by 0.91–1.34 ºC
(Hanssen-Bauer et al., 2009)
What about snow conditions?
Introduction Data & Methods Results
Norwegian Meteorological Institute met.no
Snow parameters
Start End
/media/ces/Dyrrdal_Anita_CES_2010.pdf