Recent Change—River Run-off and Ice CoverRiver runoff




Apsite E, Bolek A, Filatov N, Kondratyev S, Korhonen J, Kriaučiūnienė J, Lindström G, Nazarova L, Pyrh A, Sztobryn M

The BACC II Author Team

PublisherSpringer International Publishing AG Switzerland

2015

Second Assessment of Climate Change for the Baltic Sea Basin

Regional Climate Studies

99

116

18

978-3-319-16005-4

978-3-319-16006-1

1862-0248

1865-505X

DOIhttps://doi.org/10.1007/978-3-319-16006-1_5




This chapter compiles and assesses information on run-off and discharge from rivers within the

Baltic Sea drainage basin. Some information is also available on ice duration on inland waterways. Although decadal and regional variability is large, no significant long-term change has been detected in total river run-off to the Baltic Sea over the past 500 years. A change in the timing of the spring flood has been observed due to changes in the timing of snowmelt. Change in temperature seems to explain change in run-off better than does precipitation. Later start dates for ice formation on waterways, and earlier ice break-up dates have resulted in shorter periods of ice cover.

Last updated on 2024-26-11 at 12:19