V.—The Connection of the Glacial Period with Oscillation of the Land, especially in Scandinavia

1901 ◽  
Vol 8 (5) ◽  
pp. 205-216 ◽  
Author(s):  
Nils Olof Holst ◽  
F. A. Bather
Keyword(s):  
Baltic Sea ◽  
Fresh Water ◽  
Higher Plants ◽  
Geological Survey ◽  
Glacial Period ◽  
The Baltic Sea ◽  
Gulf Of Bothnia ◽  
The Baltic ◽  
Published Paper

[In a recently published paper Dr. N. O. Holst, of the Geological Survey of Sweden, has given a detailed description of the Post-Glacial deposits of the Baltic Sea and the Gulf of Bothnia. The paper is accompanied by a map showing the chief points of observation. The determination of the different horizons depends on (1) the stratigraphy; (2) the sub-fossil diatomaceous flora; (3) the sub-fossil higher flora. The stratigraphical evidence is in the form of numerous sections, taken all along the coast. The diatoms are used chiefly, but not solely, to distinguish the marine from the fresh-water deposits; their determinations, nearly 3,000 in number, are due to Professor P. T. Cleve and his daughter, Dr. Astrid Cleve. The remains of the higher plants have been determined by Dr. Gunnar Andersson.

Geodetic determination of the surface topography of the Baltic Sea

1997 ◽  
Vol 20 (4) ◽  
pp. 307-316 ◽  
Author(s):  
Juhani Kakkuri ◽  
Markku Poutanen
Keyword(s):  
Baltic Sea ◽  
Surface Topography ◽  
The Baltic Sea ◽  
The Baltic

scholarly journals Density and Absolute Salinity of the Baltic Sea 2006–2009

2009 ◽  
Vol 6 (2) ◽  
pp. 1757-1817 ◽  
Author(s):  
R. Feistel ◽  
S. Weinreben ◽  
H. Wolf ◽  
S. Seitz ◽  
P. Spitzer ◽  
...  
Keyword(s):  
Equation Of State ◽  
Baltic Sea ◽  
Fresh Water ◽  
Decadal Variability ◽  
Sea Water ◽  
Large Area ◽  
The Baltic Sea ◽  
Sulphate Content ◽  
Density Anomaly ◽  
The Baltic

Abstract. The brackish water of the Baltic Sea is a mixture of ocean water from the Atlantic/North Sea with fresh water from various rivers draining a large area of lowlands and mountain ranges. The evaporation-precipitation balance results in an additional but minor excess of fresh water. The rivers carry different loads of salts washed out of the ground, in particular calcium carbonate, which cause a composition anomaly of the salt dissolved in the Baltic Sea in comparison to Standard Seawater. Directly measured seawater density shows a related anomaly when compared to the density computed from the equation of state as a function of Practical Salinity, temperature and pressure. Samples collected from different regions of the Baltic Sea during 2006–2009 were analysed for their density anomaly. The results obtained for the river load deviate significantly from similar measurements carried out forty years ago; the reasons for this decadal variability are not yet fully understood. An empirical formula is derived which estimates Absolute from Practical Salinity of Baltic Sea water, to be used in conjunction with the new Thermodynamic Equation of Seawater 2010 (TEOS-10), endorsed by IOC/UNESCO in June 2009 as the substitute for the 1980 International Equation of State, EOS-80. Our routine measurements of the samples were accompanied by studies of additional selected properties which are reported here: conductivity, density, chloride, bromide and sulphate content, total CO2 and alkalinity.

CLOUDINESS IN THE POLISH COASTAL ZONE OF THE BALTIC SEA AND CONDITIONS FOR RECREATION

2017 ◽  
Vol 45 ◽  
pp. 51-63
Author(s):  
Czesław Koźmiński ◽  
Bożena Michalska
Keyword(s):  
Baltic Sea ◽  
Coastal Zone ◽  
Temporal Variations ◽  
The Baltic Sea ◽  
Summer Half ◽  
The Mean ◽  
Bioclimatic Conditions ◽  
The Baltic ◽  
Time Specific

Purpose. Determination of size, variability and gradient of cloudiness on the Polish coast of the Baltic sea during the summer half-year and identification of zones with variable suitability for recreation due to cloudiness. Method. The research is based on daily values of cloudiness in the warm half-year (April-September) recorded on a scale from 0 to 8 octants, obtained from six meteorological stations located on the Polish coast of the Baltic sea during the period 2000–2016. Methods of linear regression were used in the analysis of temporal variations of cumulative monthly deviations in cloudiness for consecutive years from the mean multiannual value. In terms of recreational suitability, days were categorised into four classes according to cloudiness. Three zones of varying conditions for recreation were identified. Results. The essential characteristic of cloudiness on the Polish coast of the Baltic sea is very high variability from one day to another and the resulting change in the value of solar radiation, which, consequently affects bioclimatic stimuli. Cumulative deviations of monthly cloudiness values from the mean multiannual value show a decrease in cloudiness in April, June and July, and an increase in the remaining months of the warm half-year. It is possible to distinguish three periods regarding increased frequency of clear and moderately clear weather lasting continuously for at least 3 and 5 days on the coastal zone in summer. The Polish coast of the Baltic sea is marked by three zones of varying conditions for recreation due to cloudiness in the summer – moderately favourable, favourable and very favourable. Research and conclusion limitations. Lack of access to time-specific results of cloudiness measurement. Practical implications. The results obtained in the course of this research may be used by individuals as well as the organizers of their stays, and for the purpose of characterisation of bioclimatic conditions of the coast. Originality. In view of the recent climatic changes recorded over the last 30 years, the present research demonstrates the current cloudiness level on the Polish coast of the Baltic sea. Type of research. Presentation of the results of empirical research.

scholarly journals Density and Absolute Salinity of the Baltic Sea 2006–2009

Ocean Science ◽  
2010 ◽  
Vol 6 (1) ◽  
pp. 3-24 ◽  
Author(s):  
R. Feistel ◽  
S. Weinreben ◽  
H. Wolf ◽  
S. Seitz ◽  
P. Spitzer ◽  
...  
Keyword(s):  
Equation Of State ◽  
Baltic Sea ◽  
Fresh Water ◽  
Decadal Variability ◽  
Sea Water ◽  
Large Area ◽  
The Baltic Sea ◽  
Sulphate Content ◽  
Density Anomaly ◽  
The Baltic

Abstract. The brackish water of the Baltic Sea is a mixture of ocean water from the Atlantic/North Sea with fresh water from various rivers draining a large area of lowlands and mountain ranges. The evaporation-precipitation balance results in an additional but minor excess of fresh water. The rivers carry different loads of salts washed out of the ground, in particular calcium carbonate, which cause a composition anomaly of the salt dissolved in the Baltic Sea in comparison to Standard Seawater. Directly measured seawater density shows a related anomaly when compared to the density computed from the equation of state as a function of Practical Salinity, temperature and pressure. Samples collected from different regions of the Baltic Sea during 2006–2009 were analysed for their density anomaly. The results obtained for the river load deviate significantly from similar measurements carried out forty years ago; the reasons for this decadal variability are not yet fully understood. An empirical formula is derived which estimates Absolute from Practical Salinity of Baltic Sea water, to be used in conjunction with the new Thermodynamic Equation of Seawater 2010 (TEOS-10), endorsed by IOC/UNESCO in June 2009 as the substitute for the 1980 International Equation of State, EOS-80. Our routine measurements of the samples were accompanied by studies of additional selected properties which are reported here: conductivity, density, chloride, bromide and sulphate content, total CO2 and alkalinity.

scholarly journals SEA LEVEL VARIATIONS IN THE GULF OF BOTHNIA

1973 ◽  
Vol 4 (1) ◽  
pp. 41-53 ◽  
Author(s):  
EUGENIE LISITZIN
Keyword(s):  
Baltic Sea ◽  
Sea Level ◽  
Water Volume ◽  
Tide Gauges ◽  
The Baltic Sea ◽  
Land Uplift ◽  
Gulf Of Bothnia ◽  
Sea Level Variations ◽  
The Baltic

An attempt is made to compute the sea level variations in the Gulf of Bothnia, which is isolated by islands and thresholds from the Baltic Sea proper. Observations from tide gauges during the 30-year period 1931–1960 were used. The effect of land uplift was taken into consideration. The maximum annual deviation in water volume from the long-term mean corresponded to 20.74 km3..

Collision Consequence Assessment of ROPAX Vessels Operating in the Baltic Sea

2012 ◽  
Author(s):  
Kristjan Tabri ◽  
Sören Ehlers ◽  
Mihkel Kõrgesaar ◽  
Kaarle Ståhlberg ◽  
Martin Heinvee
Keyword(s):  
Baltic Sea ◽  
Collision Risk ◽  
The Baltic Sea ◽  
Severe Injuries ◽  
Damage Scenarios ◽  
Structural Resistance ◽  
Cross Traffic ◽  
The Baltic ◽  
Initial Choice

A Ship collision accident represents a daily threat for vessels operating in dense traffic zones. The collision consequences may include loss of life or severe injuries if passengers are on board. The latter would be the case for ROPAX vessels, which are fairly dominant in the Baltic Sea connecting various member states. Furthermore, their routes tend to be in cross-traffic with the cargo vessels travelling through the full extent of the Baltic Sea. Therefore, it is of utmost importance to be able to assess the collision consequences for ROPAX vessels operating in the Baltic Sea with sufficient accuracy. This will result in an overview of possible damage scenarios for the actual traffic situation at a given location. As an example location the dense cross traffic between Helsinki and Tallinn will be analyzed and discussed. The analysis procedure combines three steps: (1) determination of possible accidental scenarios based on traffic statistics; (2) assessment of the structural resistance of the colliding ship and (3) the evaluation of selected accidental scenarios using a time-efficient semi-analytical approach. The level of structural resistance of the chosen ships is assessed in a quasi-static manner using finite element method. This information is the basis for the calibration of a semi-analytical collision simulation model used to simulate large number of the accidental scenarios typical to the selected location. The presented results will be limited to the initial choice between vessels and dimensions, respectively masses, but the procedure can easily be extended to cover a vast amount of colliding vessels. However, the actual collision risk can be obtained using the presented results if the traffic along the vessels route is known.

DETERMINATION OF COMBINED PROBABILITIES OF OCCURRENCE OF WATER LEVELS AND WAVE HEIGHTS FOR THE SAFETY OF DIKES AT THE BALTIC SEA

2017 ◽  
pp. 6
Author(s):  
Christian Kaehler ◽  
Christian Schlamkow ◽  
Fokke Saathoff
Keyword(s):  
Baltic Sea ◽  
Storm Surges ◽  
Water Levels ◽  
The Baltic Sea ◽  
Copula Models ◽  
Protective Function ◽  
Safety Standards ◽  
Wave Heights ◽  
The Baltic

Large parts of the Baltic Sea coast in Germany are protected by dikes against storm surges and floods. The dikes are designed to resist storm surges and floods, also taking into consideration of climate changes and sea level rise. To ensure the protective function the safety standards of the dikes are validated in regular intervals. This paper presents an approach to determine combined probabilities of occurrence of water level and wave heights for three selected sections. The probabilities of occurrence for defined return periods have been calculated by comparing several Copula models from the Archimedean Copula family.

scholarly journals Biodegradation of poly(ε-caprolactone) in natural water environments

2017 ◽  
Vol 19 (1) ◽  
pp. 120-126 ◽  
Author(s):  
Aleksandra Heimowska ◽  
Magda Morawska ◽  
Anita Bocho-Janiszewska
Keyword(s):  
Weight Loss ◽  
Surface Morphology ◽  
Baltic Sea ◽  
Fresh Water ◽  
Sea Water ◽  
Characteristic Parameters ◽  
The Baltic Sea ◽  
Loss Of Weight ◽  
Water Pond ◽  
The Baltic

AbstractThe environmental degradation of poly(ε-caprolactone)[PCL] in natural fresh water (pond) and in The Baltic Sea is presented in this paper. The characteristic parameters of both environments were measured during experiment and their influence on the biodegradation of the samples was discussed. The loss of weight and changes of surface morphology of polymer samples were tested during the period of incubation. The poly(ε-caprolactone) was more biodegradable in natural sea water than in pond. PCL samples were completely assimilated over the period of six weeks incubation in The Baltic Sea water, but after forty two weeks incubation in natural fresh water the polymer weight loss was about 39%. The results have confirmed that the investigated polymers are susceptible to an enzymatic attack of microorganisms, but their activity depends on environments.

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