2015
DOI: 10.1007/978-3-319-16006-1_12
|View full text |Cite
|
Sign up to set email alerts
|

Projected Change—Hydrology

Abstract: This chapter reviews studies on projected hydrological changes within the Baltic Sea catchment area published since the first assessment of climate change in the Baltic Sea region in 2008. Hydrological impact studies have been carried out in almost all countries in the area. The large differences in hydrological conditions (present and projected) from northern Scandinavia to the southern Baltic Sea area are addressed. The chapter considers the impacts of snow accumulation and melt, river discharge and flooding… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1
1

Citation Types

0
2
0

Year Published

2016
2016
2019
2019

Publication Types

Select...
3
1

Relationship

0
4

Authors

Journals

citations
Cited by 4 publications
(2 citation statements)
references
References 21 publications
0
2
0
Order By: Relevance
“…Freshwater runoff is projected to increase by 15-22% in the Baltic Sea during the coming century due to increased precipitation over land (Meier et al 2012). This will likely increase the input of terrestrially derived material in estuarine parts of the northern Baltic Sea where the largest increases in precipitation and runoff are expected to occur (Sonnenborg 2015; Table 2).…”
Section: Marine and Terrestrial Sources Of Organic Mattermentioning
confidence: 99%
“…Freshwater runoff is projected to increase by 15-22% in the Baltic Sea during the coming century due to increased precipitation over land (Meier et al 2012). This will likely increase the input of terrestrially derived material in estuarine parts of the northern Baltic Sea where the largest increases in precipitation and runoff are expected to occur (Sonnenborg 2015; Table 2).…”
Section: Marine and Terrestrial Sources Of Organic Mattermentioning
confidence: 99%
“…Increasing winter precipitation is result in increased river discharge during winter. Groundwater recharge increase in areas where the infiltration capacity is not currently exceeded, resulting in higher groundwater levels (Sonnenborg, 2015). Fluctuation of groundwater level depends on three main factors: hydrological or between -rivers regime, infiltration seasonality, and lithology and thickness of sediments in aeration zone (Juodkazis, 1992).…”
Section: Introductionmentioning
confidence: 99%