The Role of the Barotropic Water Exchange in the Formation of the Baltic Sea-Level Spectrum

2015 ◽  
Vol 55 (1) ◽  
pp. 5-15
Author(s):  
E. A. Kulikov ◽  
I. P. Medvedev ◽  
K. P. Koltermann
Keyword(s):  
Baltic Sea ◽  
Sea Level ◽  
Water Exchange ◽  
The Baltic Sea ◽  
Level Spectrum ◽  
The Baltic

Role of the barotropic water exchange in the formation of the Baltic Sea level spectrum

Oceanology ◽  
2015 ◽  
Vol 55 (1) ◽  
pp. 1-10 ◽  
Author(s):  
E. A. Kulikov ◽  
I. P. Medvedev ◽  
K. P. Koltermann
Keyword(s):  
Baltic Sea ◽  
Sea Level ◽  
Water Exchange ◽  
The Baltic Sea ◽  
Level Spectrum ◽  
The Baltic

Formation of the Baltic Sea level spectrum

2015 ◽  
Vol 463 (1) ◽  
pp. 760-764
Author(s):  
I. P. Medvedev
Keyword(s):  
Baltic Sea ◽  
Sea Level ◽  
The Baltic Sea ◽  
Level Spectrum ◽  
The Baltic

scholarly journals Multidecadal Sea Level Variability in the Baltic Sea and Its Impact on Acceleration Estimations

2021 ◽  
Vol 8 ◽  
Author(s):  
Armin Agha Karimi ◽  
Mohammad Bagherbandi ◽  
Milan Horemuz
Keyword(s):  
Baltic Sea ◽  
Sea Level Rise ◽  
Sea Level ◽  
Tide Gauge ◽  
Linear Trend ◽  
The Baltic Sea ◽  
Warming Hiatus ◽  
The Baltic

Multidecadal sea level variation in the Baltic Sea is investigated from 1900 to 2020 deploying satellite and in situ datasets. As a part of this investigation, nearly 30 years of satellite altimetry data are used to compare with tide gauge data in terms of linear trend. This, in turn, leads to validation of the regional uplift model developed for the Fennoscandia. The role of North Atlantic Oscillation (NAO) in multidecadal variations of the Baltic Sea is also analyzed. Although NAO impacts the Baltic Sea level on seasonal to decadal time scales according to previous studies, it is not a pronounced factor in the multidecadal variations. The acceleration in the sea level rise of the basin is reported as statistically insignificant in recent studies or even decelerating in an investigation of the early 1990s. It is shown that the reason for these results relates to the global warming hiatus in the 1950s−1970s, which can be seen in all eight tide gauges used for this study. To account for the slowdown period, the acceleration in the basin is investigated by fitting linear trends to time spans of six to seven decades, which include the hiatus. These results imply that the sea level rise is accelerated in the Baltic Sea during the period 1900–2020.

scholarly journals A Holocene relative sea-level database for the Baltic Sea

2021 ◽  
Vol 266 ◽  
pp. 107071
Author(s):  
Alar Rosentau ◽  
Volker Klemann ◽  
Ole Bennike ◽  
Holger Steffen ◽  
Jasmin Wehr ◽  
...  
Keyword(s):  
Baltic Sea ◽  
Sea Level ◽  
The Baltic Sea ◽  
Relative Sea Level ◽  
The Baltic

scholarly journals The pathway of the water exchange over the Gdańsk-Gotland Sill of the Baltic Sea and its impact on habitat formation during the stagnation period

Oceanologia ◽  
2020 ◽  
Author(s):  
Alexander Krek ◽  
Andrey Gusev ◽  
Elena Krek ◽  
Viktor Krechik ◽  
Mariia Kapustina ◽  
...  
Keyword(s):  
Baltic Sea ◽  
Water Exchange ◽  
The Baltic Sea ◽  
The Baltic ◽  
Stagnation Period

scholarly journals GIS analysis of effects of future Baltic Sea level rise on the island of Gotland, Sweden

2016 ◽  
Author(s):  
Karin Ebert ◽  
Karin Ekstedt ◽  
Jerker Jarsjö
Keyword(s):  
Baltic Sea ◽  
Sea Level Rise ◽  
Sea Level ◽  
Coastal Aquifers ◽  
Salt Water ◽  
Global Perspective ◽  
Salt Water Intrusion ◽  
The Baltic Sea ◽  
Water Intrusion ◽  
The Baltic

Abstract. Future sea level rise as a consequence of global warming will affect the world's coastal regions. Even though the pace of sea level rise is not clear, the consequences will be severe and global. Commonly the effects of future sea level rise are investigated for relatively vulnerable development countries; however, a whole range of varying regions need to be considered in order to improve the understanding of global consequences. In this paper we investigate consequences of future sea level rise along the coast of the Baltic Sea island of Gotland, Sweden, with the aim to fill knowledge gaps regarding comparatively well-suited areas in non-development countries. We study both the quantity of loss of infrastructure, cultural and natural values for the case of a two metre sea level rise of the Baltic Sea, and the effects of climate change on seawater intrusion in coastal aquifers, causing the indirect effect of salt water intrusion in wells. We conduct a multi-criteria risk analysis by using Lidar data on land elevation and GIS-vulnerability mapping, which gives formerly unimaginable precision in the application of distance and elevation parameters. We find that in case of a 2 m sea level rise, 3 % of the land area of Gotland, corresponding to 99 km2, will be inundated. The features most strongly affected are items of touristic or nature values, including camping places, shore meadows, sea stack areas, and endangered plants and species habitats. In total, 231 out of 7354 wells will be directly inundated, and the number of wells in the high-risk zone for saltwater intrusion in wells will increase considerably. Some values will be irreversibly lost due to e.g. inundation of sea stacks and the passing of tipping points for sea water intrusion into coastal aquifers; others might simply be moved further inland, but this requires considerable economic means and prioritization. With nature tourism being one of the main income sources of Gotland, monitoring and planning is required to meet the changes. Seeing Gotland in a global perspective, this island shows that holistic multi-feature studies of future consequences of sea level rise are required, to identify overall consequences for individual regions.

Sea level variations in the coastal region from altimetry – Using optimal interpolation in the Baltic Sea for 3-day mean sea level from altimetry, tide gauge and model data

2021 ◽  
Author(s):  
Ida Margrethe Ringgaard ◽  
Jacob L. Høyer ◽  
Kristine S. Madsen ◽  
Adili Abulaitijiang ◽  
Ole B. Andersen
Keyword(s):  
Baltic Sea ◽  
Sea Level ◽  
Temporal Resolution ◽  
Satellite Altimetry ◽  
Tide Gauge ◽  
Coastal Region ◽  
Optimal Interpolation ◽  
The Baltic Sea ◽  
Spatial Coverage ◽  
The Baltic

<p>The rise and fall of the sea surface in the coastal region is observed closely by two different sources: tide gauges measure the relative sea level anomaly at the coast at high temporal resolution (minutes or hours) and satellite altimeters measure the absolute sea surface height of the open ocean along tracks multiple times a day. However, these daily tracks are scattered across the Baltic Sea with each track being repeated at a lower temporal resolution (days). Due to the inverse relationship between spatial and temporal coverage of the satellite altimetry data, gridded satellite altimetry products often prioritize spatial coverage over temporal resolution, thus filtering out the high sea level variability. In other words, the satellite data, and especially averaged products, often miss the daily sea level variability, such as storm surges, which is most important for all societies in the coastal region. To compensate for the sparse spatial coverage from satellite altimetry, we here present an experimental product developed as part of the ESA project Baltic+SEAL:  on a 3-day scale, the DMI Optimal Interpolation (DMI-OI) method is combined with error statistics from a storm surge model as well as 3-day averages from both tide gauge observations and satellite altimetry tracks to generate a gridded sea level anomaly product for the Baltic Sea for year 2017. The product captures the overall temporal evolution of the sea level changes well for most areas with an average RMSE wrt. tide gauge observations of 17.2 cm and a maximum of 34.2 cm. Thus, the 3-day mean gridded product shows potential as an alternative to monthly altimetry products, although further work is needed.</p>

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