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grundvelli myndatöku með
flygildum og leysimælitæki (TLS) hefur verið notað við kortlagningu
flóðfara og við mat á útbreiðslu og umfangi hlaupa.
Þétt net jarðskjálftamæla, sem staðsettir eru á jökulskerjum eða
grafnir í jökul, hefur gefið góða raun við ákvörðun á dýpi jarðskjálfta
undir jöklum. Kvikuhreyfingar hafa þannig verið kortlagðar og
myndun gosrása staðfest af meiri nákvæmni en áður. Þó
/media/vedurstofan/utgafa/arsskyrslur/VI_Arsskyrsla_2018_vef.pdf
precipitation and time of year (an index for
available net radiation) (Vehviläinen and Huttunen, 1997). This
equation has been calibrated and verified against observations of
Class A pan evaporation values (Vehviläinen and Huttunen,
1997). The actual evaporation is calculated from potential evapora-
tion and the soil moisture deficit. The changes in temperature and
precipitation affect
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
100
15 17 19 21 23 25
Mean annual peak runoff (mm/day)
P
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r
c
e
n
t
a
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b
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l
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w
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v
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e
g39g72g79g87g68g3g70g75g68g81g74g72g3
g40g80g83g76g85g76g70g68g79g3g68g71g77g88g86g87g80g72g81g87
Percentage change in 200-year flood
Uncertainty – Relative magnitude of
sampled s urces
N = 115
GCM/RCM = 50
EA/DC = 38
HBV = 27
• Differences in GCM/RCM
tend to be more significant
in inland
/media/ces/Lawrence_Deborah_CES_2010.pdf
Nature 438,
303 (2005).
8. J. Lu, G. A. Vecchi, T. Reichler, Geophys. Res. Lett. 34,
L06805 (2007).
9. S. Manabe, R. J. Stouffer, J. Geophys. Res. 85, 5529
(1980).
10. P. S. Eagleson, in Scientific Basis of Water-Resource
Management (National Academy Press, Washington, DC,
1982).
11. N. C. Matalas, in Global Change and Water Resources
Management (Water Resources Update No. 112,
Universities
/media/loftslag/Milly_etal-2008-Stationarity-dead-Science.pdf