A A SM J J O N D J F M A A SM J J O N D J F M A A SM J J O N D
J F M A A SM J J O N D J F M A A SM J J O N D J F M A A SM J J O N D
2010–39
(a) (b)
93.
0
93.
5
94.
0
94.
5
2040–69
Lake Pielinen
93.
0
93.
5
94.
0
94.
5
2070–9994.
5
95.
5
96.
5
2010–39
94.
5
95.
5
96.
5
2040–69
Lake Syväri
94.
5
95.
5
96.
5
2070–99
75.
4
75.
8
76.
2
76.
6
2010–39
75.
4
75.
8
76.
2
76.
6
2040–69
Lake Saimaa
75.
4
75
/media/ces/Water_resources_man_Veijalainen_etal.pdf
wide and
1000 m long shelf called Þófi, terminating at 80–100 m a.s.l., see Map 4. The inclination of
the shelf is 15 on average. The surface of Þófi is covered with unconsolidated glacial till and
landslide deposits and marked with five gullies. The brook called Þófalækur near the middle of
the shelf divides it into an inner and outer part. On the outermost part of the shelf, there is a small
/media/vedurstofan-utgafa-2016/VI_2016_006_rs.pdf
/a in dry
summers, which is the maximum amount licensed by
the local government. 80% of the water is abstracted
from aquifers located above 20 masl [Henriksen and
Sonnenborg, 2003].
3. Methods
3.1. Climate-Forcing Data
[16] The confidence in Atmosphere-Ocean general circu-
lation models (GCM) providing credible quantitative esti-
mates of future climate change has increased the past few
years
/media/loftslag/vanRoosmalen_etal-2009-WRR_2007WR006760.pdf
was therefore formed
by ice lifting and deformation induced by subglacial water pressures higher than ice
overburden pressure.
The discharge data and the derived size of the subglacial flood path, as indicated
by the volume of water stored subglacially, indicates a development towards more
efficient subglacial flow over the course of the jökulhlaup. Thus, a discharge in the
iii
range 80–90 m3 s 1
/media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf