Rivers of Europe 2009
DOI: 10.1016/b978-0-12-369449-2.00015-1
|View full text |Cite
|
Sign up to set email alerts
|

Rivers of the Boreal Uplands

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
7
0

Year Published

2013
2013
2019
2019

Publication Types

Select...
5
1

Relationship

1
5

Authors

Journals

citations
Cited by 8 publications
(7 citation statements)
references
References 13 publications
0
7
0
Order By: Relevance
“…Their economic and societal value has been classified as high to very high (Museth et al ., ). Furthermore, 26 tributaries and seven individual river reaches have been protected within the river system through the Norwegian Protection Plan for River Systems (L'Abée‐Lund et al ., ). Two power stations already exist within the 200 km main river stem (Figure ).…”
Section: Introductionmentioning
confidence: 97%
“…Their economic and societal value has been classified as high to very high (Museth et al ., ). Furthermore, 26 tributaries and seven individual river reaches have been protected within the river system through the Norwegian Protection Plan for River Systems (L'Abée‐Lund et al ., ). Two power stations already exist within the 200 km main river stem (Figure ).…”
Section: Introductionmentioning
confidence: 97%
“…The Vefsna watershed is located in Norway in the northern reach of the Boreal Uplands [ 28 ]. The river mouth is located in the innermost part of the Vefsnfjorden fjord at 65°51′N, 13°11′E.…”
Section: Methodsmentioning
confidence: 99%
“…Svenningdalselva has less water than Austervefsna, with mean annual discharges of 35 and 98 m 3 s −1 , respectively. The watercourse is rather steep, with several waterfalls, and an average gradient of 2.6 m km −1 [ 28 ]. The western part of the catchment (the Svenningdalen valley) consists of strongly transformed bedrocks from the Cambro-Silurian period, while the eastern catchment (Austervefsna) has little transformed bedrock from the same period, and a wide limestone belt.…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The seventh order River Suldalslågen is 22 km long, running from the lake, Suldalsvatnet (69 m a.s.l., area 28.8 km 2 ) to the inner part of the Ryfylkefjord (59°N, 6°E) at Sand (L'Abée‐Lund et al, ; Figure ). The flow is strongly influenced by the two hydropower developments in the catchment (see below).…”
Section: The River Suldalslågenmentioning
confidence: 99%