100 mm over 24 hours. Rising stream and river
levels are likely on the Snæfellsnes peninsula, around the Eyjafjallajökull and
Mýrdalsjökull ice-caps, and south of the Vatnajökull ice cap. Travellers are cautioned
against fording rivers in these regions.
On behalf of IMO
Elín Björk Jónasdóttir, coordinator of public weather services.
Hrafn Guðmundsson, forecaster on duty
Þorsteinn V. Jónsson
/media/frettir/vedur/2016-10-18_Ovedur_en.pdf
activities.
Anne K. Fleig et al. “Regional hydrological droughts and weather types in north-western Europe “
University of Oslo Droughts WTs SummaryRelationsIntroduction Outlook
Hydrological drought in NW-Europe: Data
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/media/ces/AnneFleig_May2010_CES.pdf
Elvehøy, H., Guðmundsson, S., Hock, R., Machguth, H., Melvold, K., Pálsson, F., Radic, V.,
Sigurðsson, O. and Þorsteinsson, Þ.
The impact of climate change on glaciers and glacial runoff in the Nordic countries .......................................... 38
Radic, V. and Hock, R.
Volume changes of the glaciers in Scandinavia and Iceland in the 21st century
/media/ces/ces-oslo2010_proceedings.pdf
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/media/vatnafar/maelar/vhmkerfi_mars_2012.pdf
to land 52 nm NW of Barði and 48 nm NW of Straumnes. Two observations were received on icebergs, the 4th and the 5th.
An observation from a ship on the 18th reported sea ice from 66°31´N and 26°08´W to 66°26´N and 25°47´W.
Northeasterlies were somewhat less prevalent on the Greenland Strait than the average this month
/sea-ice/monthly/2010/nr/2339
WNW of Straumnes and the ice was scattered.
Two observations from ships were received 29th November, on a strip at location 66°50´N - 24°36´W and at 67°00´N - 24°02´W. Wind directions were mostly from the northeast and the east, however southwesterlies occurred for a few days at the Greenland Strait
/sea-ice/monthly/2010/nr/2346
which implies the need of caution for passing ships.
Two observations were received on icebergs from ships:
21st July in location 66°40.23‘N 025°13.34‘W
31st July in location 66°48.6‘N 023°03.7‘W
In the Greenland Strait northeasterly wind directions were predominant but there were also a few days with southwesterlies
/sea-ice/monthly/2011/nr/2403
in average wind power density at 10 mAGL are
between 0 and 750 W m 2 along the coast, and down to -750 W m 2 at station locations in the
interior (not shown). These differences are of about half the magnitude of the absolute measured
values.
Nawri et al. (2012b) and Nawri et al. (2012c) introduced a methodology for adjusting WRF model
results based on surface measurements. This is done through a linear
/media/vedurstofan/utgafa/skyrslur/2013/2013_001_Nawri_et_al.pdf
in sea-ice and snow sesearch
Allen Pope, Ian C. Willis, Finnur Pálsson, Neil S. Arnold1, W. Gareth Rees and Lauren
Grey ......................................................................................................................................... 31
Elevation change, mass balance, dynamics and surging of Langjökull, Iceland from 1997 to
2007
Peter Rieger
/media/vatnafar/joklar/Reykholt-abstracts.pdf