) in Europe yield contradictory results on the changes
in floods in many parts of Europe, including Finland. Dankers and
Feyen (2008) reported a considerable reduction of 10–40% in
100-year discharges in Finland, much of northern Sweden and
north-western Russia by the end of the century due to decrease
in snow accumulation; however Lehner et al. (2006) evaluated that
the 100-year floods in the same areas
/media/ces/Journal_of_Hydrology_Veijalainen_etal.pdf
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
-2007) and past years (1931 –
1960) with data of reference period (1961-1990).
10 hydrological regions:
Western, Central and
Southeastern Lithuania;
Western, Central, Southeastern
and Northeastern Latvia;
Western, Northern and
Eastern Estonia.
Geographical and hydrometeorological description of Baltic regions
• Lakes cover, forest cover, wetland cover, fields cover, %
• The average density
/media/ces/Kriauciuniene_Jurate_CES_2010.pdf