on the slopes the volcano, the jökulhlaups are quick to hit the lowlands once floodwater has reached the glacier's surface — in as little as ~5 minutes at peak discharge.
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/hydrology/hazard-risk-assessments/glacial-outburst-floods/markarfljotsaurar-oraefajokull/
for the data connections ..........................................................33
6
Appendix V. Coordinates for recommended national network and volcano monitoring
stations ..................................................................................................................................36
Appendix VI. Overview map for the CGPS network
/media/vedurstofan/utgafa/skyrslur/2011/2011_005.pdf
for efficient wide-area and high point density mapping of mixed-terrain, ice-sheets, and glaciers
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/media/vedurstofan/PhD_course-Programme_26Aug2011-final.pdf
Eyjafjallajo¨kull (E), Tindfjallajo¨kull (Ti), Torfajo¨kull (To) and My´rdalsjo¨kull (M) ice caps. The Gı´gjo¨kull outlet glacier (G) of Eyjafjallajo¨kull is also
indicated. The inset map of Iceland shows the location of the study area as well as Langjo¨kull (L), Hofsjo¨kull (H) and Vatnajo¨kull (Va) ice caps and these
weather stations: Vı´k (V) in My´rdalur (15 m a.s.l., ca. 30 km south-east
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/media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf