it takes the floodwater around 8-10 hours to come through from the meter at Sveinstindur and the meter at Eldvatn by Ása. Hydrogen sulfide travels with the running water from under the glacier.The flow is gradually increasing downstream, but typically it takes the
floodwater around 8-10 hours to come through from the meter at
Sveinstindur and the meter at Eldvatn by Ása.From 1.9.Steadily increased
/about-imo/news/flood-in-estern-skafta
it takes the floodwater around 8-10 hours to come through from the meter at Sveinstindur and the meter at Eldvatn by Ása. Hydrogen sulfide travels with the running water from under the glacier.The flow is gradually increasing downstream, but typically it takes the
floodwater around 8-10 hours to come through from the meter at
Sveinstindur and the meter at Eldvatn by Ása.From 1.9.Steadily increased
/about-imo/news/flood-in-estern-skafta/
part of Upper Tisza. Based on data from EM-DAT:
The OFDA/CRED International Disaster Database 2008
1 For a disaster to be entered into the Emergency Events Database
(EM-DAT) at least one of the following criteria must be fulfilled: (1)
Ten or more people reported killed; (2) Hundred people reported
affected; (3) Declaration of a state of emergency; (4) Call for
international assistance (From: EM
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
of the dyke and around the eruption site.
GPS measurements show continuing slow land depression towards the centre of Bardarbunga as has been the trend
over the last two weeks.
No change was detected in water monitoring that cannot be explained with changing weather.
Air quality:
Yesterday a high concentration of SO2 was measured around lake Myvatn (2000 microgram pr. cubic meter/media/jar/Factsheet_Bardarbunga_20140925.pdf
monitoring that cannot be explained with changing weather.
Air quality:
Yesterday a high concentration of SO2 was measured around lake Myvatn (2000 microgram pr. cubic meter) and last
night in Reydarfjordur (2600 microgram pr. cubic meter). The Environmental Agency of Iceland is waiting for
shipment of SO2 meters that will be put up around Iceland.
Pollution from the eruption is mostly
/media/jar/Factsheet_Bardarbunga_20140926.pdf
of future climate change, i.e. sea level rise which may on average exceed one meter in the 21st century. Photo: Halldór Björnsson, 12 May 2009.
News
2023
2022
2021
2020
2019
2018
2017
2016
2015
2014
/about-imo/news/nr/2138
bursts of
seismic tremor (1–3 Hz), and later becoming
periodic with energy between 2 and 8 Hz. After
18 October, seismicity increased to three events
per day (Figure 2b). Synchronous with this
increase, the ISGPS station SKRO (Figure 1b)
moved 9 mm westward over the following eight
days, and returned to its original position on 1
November (Figure 2c), suggesting subsurface
magma movement
/media/jar/myndsafn/2005EO260001.pdf
Assessment Re-
port (AR4).
Topic 1 summarises observed changes in climate and their ef-
fects on natural and human systems, regardless of their causes, while
Topic 2 assesses the causes of the observed changes. Topic 3 pre-
sents projections of future climate change and related impacts un-
der different scenarios.
Topic 4 discusses adaptation and mitigation options over the
next few decades
/media/loftslag/IPPC-2007-ar4_syr.pdf