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
J A
0 100 200 30020
0
60
0
100
0
Days since Sept. 1st
Q
(m
^3
/s)
Obs
Pred−nearest
Pred−weight
Method 4 T+2: RMSE−nearest= 69.6 RMSE−weight= 44.5
S O N D J F M A M J J A
Figure 7. Observed and predicted daily discharges at vhm 64 for a forecast range (T) of 2 days
and water-year 2004–2005, using methods 1 to 4 with rescaling. The 80%, 90% and 95% pre-
diction intervals are represented by grey
/media/vedurstofan/utgafa/skyrslur/2013/VI_2013_008.pdf
Probabilistic daily streamflow forecasts
based on the combined use of a
hydrological model and an analogue
method
Philippe Crochet
VÍ 2014-006
Report
Probabilistic daily streamflow forecasts
based on the combined use of a
hydrological model and an analogue
method
VÍ 2014-006
ISSN 1670-8261
Report
+354 522 60 00
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 7–9
150
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_006.pdf
Fjölbrautaskólanum við Ármúla
Kristín S. Vogfjörð, Veðurstofu Íslands
VÍ 2009-012
ISSN 1670-8261
Skýrsla
+354 522 60 00
+354 522 60 06
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 9
150 Reykjavík
5
Project no. 036935
Project acronym: SAFER
Project title: Seismic eArly warning For EuRope
Instrument : Specific Targeted Research Project
Thematic Priority: Sustainable development
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_012.pdf