Natural and medical sciences

2013 Issue №1

The types of atmospheric water circulation over the Atlantic and the formation of the extreme North Sea water inflows into the Baltic Sea

Abstract

This article emphasises that one of the conditions for the formation of extreme inflow events from the North into the Baltic Sea is the long-time impact of same-type atmospheric processes on the water surface. There is a need to consider the intensity and the duration of one-direction atmospheric processes. The authors focus on the features and types of large-scale atmospheric circulation over
the North-East Atlantic, which determined the regional atmospheric processes over the Baltic Sea during the formation of a large inflow. The article analyses the inflows of December 22, 1975 — January 14, 1976, and the inflow of January 16—222003, as well as baric topography (500hPa) and daily synoptic maps.

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The results of the weekly monitoring of the Vistula Bay coast in the area of Pribrezhny village in 2011-2012

Abstract

This article offers the results of regular (weekly) monitoring of the coast of the Vistula Lagoon in the area of the village of Pribrezhny (the Kaliningrad region) throughout the year. The steady profile measurements of the beach width, photographing, coast description, the calculation of changes in the relative level of the Vistula Lagoon, and the analysis of the wind regime over the observation period made it possible to reveal the coast dynamics, assess the stability of the beach and coastal slope condition, as well as the influence of the
main regime-forming factor — the wind.

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The computer simulation of tsunami wave breaking against a steep shore

Abstract

This article offers a computer simulation for incompressible stratified fluid based on Euler’s equations. The ocean and the atmosphere above it are considered as an integral continuous environment. At the water-air surface, the density changes abruptly from ρ = ρwater = 1000 kg/m3 for water to ρ = ρair = 1.2 kg/m3 for air. The solution to model equations is generalised. The mathematical mechanism
of equation solving suggests automatic smoothing of density in the area of wave breaking and formation of a thin fluid layer with an intermediate density.

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