) noted that Iceland had a maritime
climate that was much milder than its position on the globe might suggest. In
data from 1981–2010, Iceland annual average temperatures ranged from 6°C at the
south coast to 3°C at the north coast, with a substantially colder highland
interior. In comparison with the latitudinal average for the same period, the
coastal temperatures in Iceland are 8–10°C warmer
/climatology/iceland/climate-report/
Surface Air Temperature and
Precipitation Trends for Iceland
in the 21st Century
Nikolai Nawri
Halldór Björnsson
VÍ 2010-005
Skýrsla
Surface Air Temperature and
Precipitation Trends for Iceland
in the 21st Century
VÍ 2010-005
ISSN 1670-8261
Skýrsla
+354 522 60 00
+354 522 60 06
vedur@vedur.is
Veðurstofa Íslands
Bústaðavegur 9
150 Reykjavík
Nikolai Nawri, Icelandic Meteorological Office
Halldór
/media/ces/2010_005_.pdf
Evaluation of HARMONIE reanalyses of
surface air temperature and wind speed
over Iceland
Nikolai Nawri
VÍ 2014-005
Skýrsla
2
Evaluation of HARMONIE reanalyses of
surface air temperature and wind
speed over Iceland
VÍ 2014- 005
ISSN 1670- 8261
Skýrsla
+354 522 60 00
vedur @vedur . is
Veður st of a Íslands
Búst aðaveg ur 7 – 9
108 Reyk j avík
Nik olai Nawr i
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_005.pdf
2609 BEITO NO +61:14:35 +08:51:20 754 P
2610 BIRI NO +60:57:10 +10:35:49 190 P
2611 ABJORSBRATEN NO +60:55:05 +09:17:25 639 TP
2612 BOVERDAL NO +61:43:14 +08:14:39 701 P
2613 ESPEDALEN NO +61:25:00 +09:32:04 752 P
2614 LUNNER NO +60:17:39 +10:34:49
/media/ces/CES_D2.4_task1.pdf
; Jylhä et al., 2008; Räisänen, 2008) and to de-
crease snowmelt floods, which are currently the largest floods in
most parts of Finland. Significant changes in seasonality of runoff
and floods may occur in areas where a large proportion of runoff
is from snowmelt (e.g. Lettenmaier et al., 1999; Bates et al., 2008).
Finland extends from 70 North with sub-arctic climate to 60
North in the margins
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
26 October 2012
ESC statement on L’Aquila sentence
The European Seismological Commission (ESC) as a Commission of the
International Association of Seismology and Physics of the Earth’s Interior
(IASPEI) endorses and adheres to the IASPEI Press Release on the L'Aquila
sentence (http://www.iaspei.org/news_items/laquila_IASPEI_press_release_final.pdf
/media/vedurstofan/utgafa/hlidarefni/ESC-IASPEI-statement-LAquila-2012-1.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
in southern Norway (Fig.1). The glacier has a total area of 5.4 km2 and rangesin altitude from 1390 to 2090 m a.s.l. The glacierhas been mapped repeatedly, the most recent mapis from 1997. Areas calculated from the 1951 and1997 maps reveal an area reduction of about 0.4km2 in this period (Andreassen 1999). Lengthchange observations reveal a net retreat of about 60
m from 1997 to 2006 (data: NVE; e.g
/media/ces/GA_2009_91A_4_Andreassen.pdf
The wind energy potential of Iceland
Nikolai Nawri
Guðrún Nína Petersen
Halldór Björnsson
Kristján Jónasson
VÍ 2013-001
Report
The wind energy potential of Iceland
VÍ 2013- 001
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
Nikolai Nawri, Icelandic Met Office
Guðrún Nína Petersen, Icelandic Met
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf