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at the operational/local level.
A calibrated approach (standardized questionnaires and
interviews, expert judgment, and reinterpretation of out-
comes by means of relevant literature) was used to com-
pare the state of affairs in water management in the
selected case-studies.
Adaptive and integrated water management
Given the expected increase of climate-related extreme
events, water governance capabilities
/media/loftslag/Huntjens_etal-2010-Climate-change-adaptation-Reg_Env_Change.pdf
km south-southwest of the
eruption site at 15:00 GMT.
Lightning: Four lightning strikes detected over the summit of Eyjafjallajökull between
19:47 and 20:03 GMT on 28 April.
Noises: Booming sounds were reported yesterday evening, and again this morning,
from Selsund, located ~40 km north-northwest of the eruption site.
Additional note: 16:13 GMT: A sulphur smell was detected at 3
/media/jar/Eyjafjallajokull_status_2010-04-29_IES_IMO.pdf
Storm in the North at noon or after noon.
Southwest 18 - 28 and wintry showers by noon, strongest wind in the north. Decreasing winds late afternoon. Mostly dry in the northeast tonight. South and southeast 8 - 15 m/s tonight and tomorrow, snow or snow showers but mostly dry in the north. Temperature 0 to 5 °C today but colder tomorrow.
The text forecast on the web gives the most reliable
/about-imo/news/nr/3258
was broken by an astounding 1,7 degree margin, the former record being 18.8 degrees, measured in Eskifjörður in the Eastern Fjords on 28 March 2000.
Many local maximum temperature records where also exceeded, amongst those at Teigarhorn in the Eastern Fjords where the maximum rose to 18.2 degrees. The daily recording of maximum temperature at Teigarhorn began in 1872 and the new record exceeded
/about-imo/news/nr/2459
by
rescaling a dimensionless regional flood frequency distribution or growth curve, qR(D;T ), com-
mon to all sites of the homogeneous region, with the so-called index flood, µi(D), of the target
site:
bQi(D;T ) = µi(D)qR(D;T ); (1)
where bQi(D;T ) is the estimated flood quantile, i.e. the T -year flood peak discharge averaged
over duration D, at site i. The regional growth curve, qR(D;T
/media/vedurstofan/utgafa/skyrslur/2015/VI_2015_009.pdf
Such landslides fall from a comparatively high
elevation, cause extensive disruption and upheaval of loose materials and soils in their
way, and can travel considerable distances uphill against opposing slopes.
Secondly, there are medium-sized or large, rapid debris flows that are released from com-
paratively high elevations and are confined to gullies as they travel down the mountain-
side, similar
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
showers at sea level. Average wind speeds may be expected to exceed 28 m/s, which is whole gale according to the Beaufort wind scale. Wind gusts can be exptected to reach 50 m/s, especially to the north and east of mountains (the leeside).
On Monday morning, southwest gale or strong gale (18-25 m/s) is forecasted, with winds moderating somewhat during the afternoon (13-20 m/s). Snowshowers
/about-imo/news/nr/3020