2005
DOI: 10.1007/s10236-005-0110-6
|View full text |Cite
|
Sign up to set email alerts
|

Discharge and transport processes along the German Baltic Sea Coast

Abstract: The western Baltic Sea infront of the German coast is a highly variable dynamical system, dominated by a complex and small-scale morphometry, the water exchange between the Baltic and North Seas, and driven by local wind. Neither data collection, nor satellite images or model simulations alone were able to explain the observed spatial patterns and transport processes. Therefore, all these methods were combined to explain the dynamical features and to systematise them according to the typical local wind pattern… Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

0
8
0

Year Published

2008
2008
2015
2015

Publication Types

Select...
6
1

Relationship

2
5

Authors

Journals

citations
Cited by 14 publications
(8 citation statements)
references
References 15 publications
0
8
0
Order By: Relevance
“…Then, upwelling can be detected by a local sharp temperature drop in the surface water, which can last a couple of days. A well-developed method to observe this phenomenon, recurring in time and location, is satellite imaging of the sea surface temperature (Siegel et al, 1994(Siegel et al, , 2005Lass et al, 2010).…”
Section: Upwellingmentioning
confidence: 99%
“…Then, upwelling can be detected by a local sharp temperature drop in the surface water, which can last a couple of days. A well-developed method to observe this phenomenon, recurring in time and location, is satellite imaging of the sea surface temperature (Siegel et al, 1994(Siegel et al, , 2005Lass et al, 2010).…”
Section: Upwellingmentioning
confidence: 99%
“…The western Baltic Sea is a highly dynamic system (Siegel et al, 2005), influenced by the mainly wind-driven exchange with the more saline North Sea through the narrow Danish Streets and the less saline Baltic Proper (Feistel et al, 2008). As a consequence a salinity gradient from west to east occurs with the Darß Sill as a barrier for inflowing salty and oxygen-enriched bottom water (Fig.…”
Section: Introductionmentioning
confidence: 99%
“…1). Siegel et al (2005) combined ship measurements, satellite data and model simulations to show how the hydrographical conditions of the western Baltic Sea change under different wind conditions. Although the Darß Sill holds oxygen-rich bottom water back in the Mecklenburger Bay, seasonal hypoxias occur (HELCOM, 2009), as well in the Arkona Sea.…”
Section: Introductionmentioning
confidence: 99%
“…The systematisation performed for the Pomeranian Bight was extended to the entire coast of the German state, to study the dynamical features and processes there. The derived features were related not only to the dominating wind directions but also to transitions between these directions (Siegel et al 2005b). The issued catalogue of processes supports the interpretation of monitoring data and the optimisation of the coastal monitoring programme of regional authorities.…”
Section: Coastal Processes and River Dischargementioning
confidence: 99%