-5.2 km height
between 13:00 and 15:00 GMT. The plume rises higher after large
explosions.
Heading: East-south-east to south-east from the eruption site. Plume track clearly
visible at least 200 km from the eruption site and probably another 200
further to the SE on MODIS (11:20 GMT) satellite imagery.
Colour: Observation from ICG-flight: Dark grey (ash) clouds observed over
/media/jar/Eyjafjallajokull_status_2010-05-03_IES_IMO.pdf
6University of Washington,
Seattle, WA 98195, USA. 7NOAA Geophysical Fluid
Dynamics Laboratory, Princeton, NJ 08540, USA.
*Author for correspondence. E-mail: cmilly@usgs.gov.
An uncertain future challenges water planners.
Published by AAAS
on July 12, 201
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/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf
the eruption site. Plume track visible at least 200 km
from the eruption site on MODIS (12:35 GMT) and EUMETSAT
(17:15 GMT) satellite imagery.
Colour: Dark grey (ash) clouds observed over the eruptive site. White (steam)
plumes rising from Gígjökull, north of the eruption site.
Tephra fallout: Moderate ash-fall reported in the village of Vík (12:00 GMT),
located 40 km south-east
/media/jar/2010-05-02_En-IES_IMO.pdf
increases by 2.1ºC, and the interannual standard deviation dec-
reases by 6%, when the simulated global mean T increases by 1ºC.
Of course, there is variation between different models!
Time series of winter mean temperature
in Helsinki (1961-2008)
Blue line = observations
Red line = best-estimate present-day (2010) climate
Grey dots = results for individual models
Probability distribution
/media/ces/RaisanenJouni_CES_2010.pdf
and grey, and a light easterly wind blows it to the west.
No reports of ashfall today; no lightning strikes have been detected since two days ago and there are no reports of noise from the eruption. Meltwater discharge from Gígjökull is small. The eruption is ongoing similar to yesterday with occasional explosions in the crater. Neither crater nor lava is visible due to clouds over the volcano
/earthquakes-and-volcanism/articles/nr/1884
connects the NVZ to the
offshore Kolbeinsey ridge (KR). The block bounded by the WVZ, EVZ and SISZ is
sometimes called the Hreppar micro-plate (HM). Seismicity is mainly confined to the two
transform zones, the TFZ and the SISZ. This thesis focuses on seismicity in the SISZ, RP
and WVZ.
Figure 1.1.The plate boundary in Iceland. Fissure swarms are shown as grey areas and central volcanoes
/media/vedurstofan/utgafa/skyrslur/2010/2010_003rs.pdf
Resources and Energy Directorate (NVE), Norway. Lidar measurements of Norwegian glaciers ‒ an overview
René Forsberg, Henriette Skourup and Sine M. Hvidegaard, DTU Space, Technical University of Denmark. A decade of lidar measurements for ice, ocean and land applications
Allen Pope, Ian C. Willis*, Finnur Pálsson Neil S. Arnold, W. Gareth Rees, Lauren Grey, Scott Polar Research Institute (SPRI
/lidar/lidar-2013/program/
the simulated AMF series made with
WaSiM, at the gauged sites. The solid red line corresponds to the distribution estimated
with the IFM (Eqs. 1 and 12) developed with WaSiM simulations within vhm52 (top) and
vhm51 (bottom). Dashed lines and shaded grey region correspond to the 95% confidence
intervals (CI) (see Crochet 2012a). Uncertainty related to hydrological modeling is not
included in the CI
/media/vedurstofan/utgafa/skyrslur/2014/VI_2014_001.pdf