and Relative Changes When Comparing the A2
and B2 Scenarios to the Current Climatea
Scenario Net Recharge Horizontal Boundary Outflow Drain Flow Base Flow Water Supply Irrigation
Simulations Not Including Abstractions and Irrigation
Current climate 550 23 279 252
A2 scenario + 67 (12%) + 1 (4%) + 56 (20%) + 13 (5%)
B2 scenario + 113 (21%) + 1 (4%) + 92 (33%) + 22 (9%)
Simulations Including Abstractions
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
recorded at 5-13 km depth, but fewer than
yesterday.
GPS deformation: Measurements from around Eyjafjallajökull indicate no major net
discplaceaments, suggesting a stabilization of the surface deformation
since yesterday.
Other remarks: Grainsize analysis of samples taken of ash that fell on May 3rd at 64
km distance from the eruption site shows that about 5 % of the ash is
smaller
/media/jar/Eyjafjallajokull_status_2010-05-07_IES_IMO.pdf
opportunity evaluation
Case studies
NOE Net
SEAS-NVE
Findings of case studies
• Distribution companies generally well
equipped for climate change
– Cabling of all overhead lines well under way
– Distribution boxes in areas with increased risk of
flooding are elevated already
– Salt spray further inland is becoming an increasing
problem for substations and transformers
Cabling in Denmark
/media/ces/James-Smith_Edward_CES_2010.pdf
anomalies of the WTs during the periods leading up to the five
most severe droughts as compared to the average frequency of a given WT for the same
period of the year over the entire data record. A period equal to dreg preceding the drought
plus the 20 first days of the drought was used. All WTs with a net positive frequency anomaly
over the five events were considered to be associated
/media/ces/ces-oslo2010_proceedings.pdf
961–975, 2011
966 G. Aðalgeirsdóttir et al.: 20th and 21st century evolution of Hoffellsjökull glacier
Table 1. Specific winter (bw), summer (bs) and net balance (bn) for
Hoffellsjökull in mw.e. a−1. A conservative error estimate is on the
order of 15–20 % for both bw and bs.
Glacier year bw bs bn
1935–1936 2.0 −3.4 −1.4
1936–1937 2.4 −2.1 0.3
1937–1938 1.7 −2.4 −0.6
2000–2001 2.0 −2.1 −0.1
2001
/media/ces/Adalgeirsdottir-etal-tc-5-961-2011.pdf
level coursed by tides is small with a range of less than 0.5 m.
Figur 1. Horsens Fjord catchment. WFD main catchment area is 794 km2
NONAM Summerschool Copenhagen 22-26 August 2011 2
Physical features and ecosystem
The fjord landscape is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations
/media/loftslag/Horsens_case.pdf
is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens
fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and
scattered habitation. One of the most important plant community on the islands are along the East coast
/media/loftslag/CASE_A___Jes_Pedersen_(Region_Midt,_Dk)_Introduction.pdf
is formed by glacial deposits. The average depth is 5 meters and the residence time
of water in the fjord is about 20 days. As to tidal variations the amplitude is about 0.4 meters. Horsens
fjord consists of marine coastal ecosystems. There are three fairly large islands with cultivated land and
scattered habitation. One of the most important plant community on the islands are along the East coast
/media/loftslag/Case_A___Horsens_Fjord.pdf
NONAM PhD course – Adaptive management in relation to climate change – Copenhagen 21-26/8/2011
……………………………………………………………………………………………………………………………………………………………………
1
Outline for the case Road maintenance in a changing climate
Introduction
Roads and transport systems are vulnerable to climate change impacts (VTT 2011; Koetse and
Rietveld, 2009; Regmi & Hanaoka, 2011; Road ERA-net 2009 & 2010
/media/loftslag/Outline_for_the_case_Road_maintenance_in_a_changing_climate.pdf
line shows the number of all measured earthquakes but the red line shows the number of earthquakes above 1.5 in magnitude.
During these years, the measuring net has improved and become more sensitive. That is the reason for showing the larger earthquakes separately.
18 August 2014 20:45 - An overview of the first three days
Since the onset of the earthquake swarm at Bárðarbunga on Saturday
/earthquakes-and-volcanism/articles/nr/3000