Wyniki wyszukiwania

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Frequency and strength of storm surges in the Oder River estuary area

100%

Kowalewska-Kalkowska H.

Acta Scientiarum Polonorum. Formatio Circumiectus

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2018

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tom 17

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nr 3

The aim of the study was to estimate the frequency and strength of storm surges in the Oder River mouth area during the 1993/94–2016/17 seasons. The analyses involved water level readings recorded at gauges located in the Oder River mouth area, including the coasts of the Pomeranian Bay (Zatoka Pomorska) and the Szczecin Lagoon (Zalew Szczeciński), as well as the downstream reach of the Oder. Recognition of temporal and spatial water level variations in the region under investigation revealed signicant irregularities in storm surge occurrence; periods with an increased frequency of surges followed long periods with their scant occurrence. During the year, most of the storm events were observed between November and January. In the period discussed, the most severe and extensive storm surge in the Oder River mouth area was observed in October 2009. Very high surges were recorded in November 1995, January 2012, and January 2017. The long-lasting and extensive high water events in the downstream reach of Oder River resulted from the progressive and prolonged increase in sea level in the Pomeranian Bay. Long-term persistence of high water levels in the Oder River mouth area were also registered when storm surges limited the outflow of the Oder River during snow-melt events, ice jams developing on the lower Oder at the same time. Finally, severe storm events were observed under the condition of the increased water volume in the Baltic Sea.

2

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Linking sea level dynamic and exceptional events to large-scale atmospheric circulation variability: A case of the Seine Bay, France

75%

Turki I., Massei N., Laignel B.

Oceanologia

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2019

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tom 61

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nr 3

3

Influence of water exchange between the Baltic Sea and the North Sea on storm surges in the Baltic

75%

Chilicka Z., Kowalik Z.

Oceanologia

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1984

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tom 19

4

Verification of a certain numerical model with the real storm surge of December 1976 in the Baltic Sea

75%

Chilicka Z.

Oceanologia

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1984

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tom 19

5

Water exchange between the Baltic and the North Sea based on a barotropic model

75%

Kowalik Z., Staskiewicz A.

Oceanologia

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1978

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tom 09

6

The storm surge recorded in a thin section

75%

Vierek A.

International Letters of Natural Sciences

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2015

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tom 38

Limestone and sandstone beds deposited by storms are called tempestites, and exhibit much variation in thickness, grain size and internal structures, depending on the proximity and on the intensity of the storm waves. In this paper, diagnostic features of storm beds observed in thin sections, was presented. Characteristic features are investigated on the basis of detailed study in the Upper Devonian carbonates in the western part of the Holy Cross Mountains (Poland).

7

Sedimentary structure of the storm surge washover fan on the Lake Bukowo spit

75%

Rudowski S., Wroblewski R.

Oceanological Studies

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2000

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tom 29

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nr 3

8

Sea level and storm surge forecasting in the Southern Baltic

63%

Wroblewski A.

Oceanologia

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1991

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tom 31

9

Erosion and its rate on an accumulative Polish dune coast: the effects of the January 2012 storm surge

63%

Labuz T. A.

Oceanologia

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2014

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tom 56

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nr 2

10

Extreme sea levels at selected stations on the Baltic Sea coast

63%

Wolski T., Wisniewski B., Giza A., Kowalewska-Kalkowska H., Boman H., Grabbi-Kaiv S., Hammarklint T., Holfort J., Lydeikaite Z.

Oceanologia

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2014

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tom 56

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nr 2

11

Consltruction of a numerical model of storm surges with a refined grid

63%

Chilicka Z., Kowalik Z., Wierzbicki Z.

Oceanologia

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1983

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tom 16

12

Water level fluctuations in the Odra River mouth area in relation to passages of deep low-pressure systems

63%

Wisniewski B., Kowalewska-Kalkowska H.

Oceanological and Hydrobiological Studies

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2007

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tom 36

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nr 1

13

Physical aspects of extreme storm surges and falls on the Polish coast

51%

Wisniewski B., Wolski T.

Oceanologia

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2011

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tom 53

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nr (1-TI)

Extreme sea levels – storm-generated surges and falls – on the Polish coast are usually the effects of three components: the volume of water in the southern Baltic (the initial level preceding a given extreme situation), the action of tangential wind stresses in the area (wind directions: whether shore- or seaward; wind velocities; and wind action duration), and the sea surface deformation produced by deep, mesoscale baric lows moving rapidly over the southern and central Baltic that generate the so-called baric wave. Among these factors, the baric wave is particularly important for, i.e. the water cushion underneath the baric depression, moving along the actual atmospheric pressure system over the sea surface.

14

Analysis and forecast of long-term sea level changes along the Polish Baltic Sea coast. Part I. Annual sea level maxima

51%

Wroblewski A.

Oceanologia

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1992

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tom 33

Ograniczanie wyników

Frequency and strength of storm surges in the Oder River estuary area

Linking sea level dynamic and exceptional events to large-scale atmospheric circulation variability: A case of the Seine Bay, France

Influence of water exchange between the Baltic Sea and the North Sea on storm surges in the Baltic

Verification of a certain numerical model with the real storm surge of December 1976 in the Baltic Sea

Water exchange between the Baltic and the North Sea based on a barotropic model

The storm surge recorded in a thin section

Sedimentary structure of the storm surge washover fan on the Lake Bukowo spit

Sea level and storm surge forecasting in the Southern Baltic

Erosion and its rate on an accumulative Polish dune coast: the effects of the January 2012 storm surge

Extreme sea levels at selected stations on the Baltic Sea coast

Consltruction of a numerical model of storm surges with a refined grid

Water level fluctuations in the Odra River mouth area in relation to passages of deep low-pressure systems

Physical aspects of extreme storm surges and falls on the Polish coast

Analysis and forecast of long-term sea level changes along the Polish Baltic Sea coast. Part I. Annual sea level maxima