of the glaciers at their maximum at the end of the Little Ice Age (about 1890) and also at the end of the 20th century. On the map surge-type glaciers are distinguished from non-surge-type glaciers with a darker green color. A symbol shows volcanic calderas which are located underneath the glaciers. Also shown are place-names of all of the glaciers that have been given names.
An explanatory
/about-imo/news/nr/2712
Regional Flood Frequency Analysis:
A case study in eastern Iceland
Philippe Crochet
Tinna Þórarinsdóttir
VÍ 2015-007
Report
Regional Flood Frequency Analysis:
A case study in eastern Iceland
VÍ 2015-007
ISSN 1670-8261
Report
+354 522 60 00
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 7–9
108 Reykjavík
Philippe Crochet, Icelandic Met Office
Tinna Þórarinsdóttir, Icelandic Met Office
Contents
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_007.pdf
Psolid and redistribution of snow is
not taken into account. A threshold range of 1 to 2 ◦C is used to distinguish snowfall and rain.
Melt-water refreezing is parameterized according to Reeh (1991), using a melt-water retention
capacity of 60% of the water equivalent of the snow cover.
The glacier mass balance model is designed to operate on large areas. For model input
entire grids from RCM output
/media/ces/ces_geus_paakitsoq_full_report.pdf
Probabilistic daily streamflow forecast
using an analogue sorting method
Philippe Crochet
VÍ 2013-008
Report
Probabilistic daily streamflow forecast
using an analogue sorting method
VÍ 2013- 008
ISSN 1670- 8261
Report?
+354 522 60 00
vedur @vedur . is
Veður st of a Íslands
Búst aðaveg ur 7 – 9
150 Reyk j avík
Philippe Crochet, Icelandic Met Office
Contents
1
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
by 25 % in the interior of Ice-
land, where the large ice caps are located (Nawri and Björns-
son, 2010).
Before year 2010, the glacier model is forced with daily
mean records constructed from the monthly mean observed
temperature and precipitation as previously explained. Pos-
sible natural variations in the climate are important for near-
future projections as the magnitude of the expected
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
commercial use.
Data means any type of forecast, measurement, observation, calculated result or derived data (i.e. from model calculations). Many pages on the IMO web-site contain real-time data that has not been assessed; note that these data are preliminary and that they might change after revision. The Icelandic Meteorological Office does not guarantee that data on its web-site will always
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commercial use.
Data means any type of forecast, measurement, observation, calculated result or derived data (i.e. from model calculations). Many pages on the IMO web-site contain real-time data that has not been assessed; note that these data are preliminary and that they might change after revision. The Icelandic Meteorological Office does not guarantee that data on its web-site will always
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;script type="text/javascript" src="http://vedur.is/js/iframe.js"></script>
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To show other areas, a different digit must be entered after 'Vi.ifrm.area'. The area codes are as follows:
101 = whole country
111
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be copied to your html file where the frame should appear:
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<script type="text/javascript"><!--
VI.ifrm.type = 'wst';
VI.ifrm.area = 101;
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VI.ifrm.displayWeather();
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</script>
To show other areas, a different digit must be entered after 'Vi.ifrm.area
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