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1
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Statistical analysis of Mediterranean coastal storms

100%
Martzikos N. T., Prinos P. E., Memos C. D., Tsoukala V. K.
Oceanologia
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2021
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tom 63
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nr 1
2
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Content available

Assessment of coastal vulnerability in Chabahar Bay due to climate change scenarios

86%
Armanfar M., Goharnejad H., Niri M. Z., Perrie W.
Oceanologia
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2019
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tom 61
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nr 4
3

Relation between the type of wave exposure and seagrass losses (Cymodocea nodosa) in the South of Gran Canaria (Canary Islands – Spain)

86%
Portillo E.
Oceanological and Hydrobiological Studies
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2014
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tom 43
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nr 1
4
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Simulating tropical storms in the Gulf of Mexico using analytical models

86%
Kalourazi M. Y., Siadatmousavi S. M., Yeganeh-Bakhtiary A., Jose F.
Oceanologia
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2020
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tom 62
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nr 2
5

Dependence of severe storm occurrence on circulation types in Poland

86%
Lupikasza E., Bielec-Bakowska Z.
Badania Fizjograficzne nad Polską Zachodnią. Seria A: Geografia Fizyczna
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2012
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tom 63
6

Etude numerique de l’influence de l’état de la mer sur la propagation d’ondes dans un canal

86%
Geringer J.
Oceanologia
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1978
|
tom 09
7
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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What has changed in France in coastal flood risk management after Xynthia storm

86%
Cunge J., Erlich M.
Annals of Warsaw University of Life Sciences - SGGW. Land Reclamation
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2014
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tom 46
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nr 3
One year after the Xynthia storm surge, which struck the Vendée and the Charente-Maritime counties of the French Atlantic Coast in the night of 27/28 February 2010, French authorities implemented a national plan for mitigation and management of the flash submersions (MEDDTL 2011). In this paper authors analyse partial results of this plan after almost three years of its effectiveness in the perspective of Xynthia catastrophic event, but also taking into account other dramatic coastal submersions, which occured during winter 2014 in the same region.
8
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Effects of global climate oscillations on intermonthly to interannual variability of sea levels along the English Channel Coasts (NW France)

72%
Turki I., Massei N., Laignel B., Shafiei H.
Oceanologia
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2020
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tom 62
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nr 2
9
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Extreme wind waves in the Black Sea

72%
Divinsky B. V., Fomin V. V., Kosyan R. D., Ratner Y. D.
Oceanologia
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2020
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tom 62
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nr 1
10

Factors affecting the intensity and character of cliff evolution near Ustka

72%
Florek W., Kaczmarzyk J., Majewski M.
Oceanological and Hydrobiological Studies
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2009
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tom 38
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nr Suppl.1
9-25
11
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Formation and species composition of stormcast beach wrack in the Gulf of Riga, Baltic Sea

72%
Suursaar U., Torn K., Martin G., Herkul K., Kullas T.
Oceanologia
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2014
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tom 56
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nr 4
12

Dynamics of the Polish coast east of Ustka

72%
Florek W., Kaczmarzyk J., Majewski M.
Geographia Polonica
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2010
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tom 83
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nr 1
13
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Decadal variations in wave heights off Cape Kelba, Saaremaa Island, and their relationships with changes in wind climate

72%
Suursaar U., Kullas T.
Oceanologia
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2009
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tom 51
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nr 1
39-61
Based on wind data from the Vilsandi meteorological station and a 5-month calibration measurement with a bottom-mounted Recording Doppler Current Profiler (RDCP), a semi-empirical hindcast of wave parameters near the quickly developing accumulative Kelba Spit is presented for the period 1966–2006. The significant wave heights with a gross mean value of 0.56 m exhibited some quasiperiodic cycles, with the last high stage in 1980–95 and a decreasing overall trend of −0.001 m per year. At the same time, both the frequency and intensity of high wave events showed rising trends, and the mean wave heights during winter (December to February) increased as well. As the study area has the longest fetches in westerly directions, the discussed tendencies in wave conditions are sensitive to regional changes in the wind climate and can be related to a decrease in the local average wind speed on the one hand, but an intensification of westerly winds, storm events and the wintertime NAO index on the other. The roughest wave storms on record were associated with prominent W-storms on 2 November 1969 and 9 January 2005; a few other extreme wind events (e.g. in 1967, 1999, 2001), however, did not yield equally prominent waves.
14

Bathymetric fluctuations as an effect of breaking wave action based: example of a selected section of the Baltic Sea coastal zone

72%
Choinski A.
Badania Fizjograficzne nad Polską Zachodnią. Seria A: Geografia Fizyczna
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2016
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tom 67
15

Sea level variability in the eastern part of the Polish Baltic Sea coast 1975-2004

72%
Marosz K. J., Jakusik E.
Geographia Polonica
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2010
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tom 83
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nr 1
16
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

An integrated wave modelling framework for extreme and rare events for climate change in coastal areas – the case of Rethymno, Crete

72%
Tsoukala V. K., Chondros M., Kapelonis Z. G., Martzikos N., Lykou A., Belibassakis K., Makropoulos C.
Oceanologia
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2016
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tom 58
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nr 2
17
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

A brief analysis of North Sea physics

58%
Sundermann J., Pohlmann T.
Oceanologia
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2011
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tom 53
|
nr 3
The current state of understanding the North Sea’s physical system is presented. First, basic phenomena like astronomical tides and general circulation will be described and analysed with respect to their physical nature and respective interactions. There will be special focus on fundamental dynamic balances. Next, some specific topics relevant to the marine ecosystem, the economy and society will be considered: among them, spreading and transport processes, the fresh water budget, the heat budget and storm surges. A separate section is dedicated to the North Sea of Tomorrow, i.e. the prospective variations of the physical environment resulting from global changes in future decades. The statements are based on the long experience of the authors and their groups and include findings that are little known if at all. The review finishes with a list of open questions and the corresponding research demands.
18
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
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Effect of mangrove forest structures on wave attenuation in coastal Vietnam

58%
Bao T. Q.
Oceanologia
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2011
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tom 53
|
nr 3
This paper analyses wave attenuation in coastal mangrove forests in Vietnam. Data from 32 mangrove plots of six species located in 2 coastal regions are used for this study. In each plot, mangrove forest structures and wave height at different cross-shore distances are measured. Wave height closely relates to cross- shore distances. 92 exponential regression equations are highly significant with R2 >0.95 and P val. <0.001. Wave height reduction depends on initial wave height, cross-shore distances, and mangrove forest structures. This relationship is used to define minimum mangrove band width for coastal protection from waves in Vietnam.
19
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Flow, waves and water exchange in the Suur Strait, Gulf of Riga, in 2008

58%
Raudsepp U., Laanemets J., Haran G., Alari V., Pavelson J., Kouts T.
Oceanologia
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2011
|
tom 53
|
nr 1
Wind, flow and wave measurements were performed in November–December in 2008 in the relatively narrow and shallow Suur Strait connecting the waters of the V¨ainameri and the Gulf of Riga. During the measurement period wind conditions were extremely variable, including a severe storm on 23 November. The flow speed along the strait varied between ±0.2 m s−1, except for the 0.4 m s−1 that occurred after the storm as a result of the sea level gradient. The mean and maximum significant wave heights were 0.53 m and 1.6 m respectively. Because of their longer fetch, southerly winds generated higher waves in the strait than winds from the north. All wave events caused by the stronger southerly winds induced sediment resuspension, whereas the current-induced shear velocity slightly exceeded the critical value for resuspension only when the current speed was 0.4 m s−1. A triplenested two-dimensional high resolution (100 m in the Suur Strait) circulation model and the SWAN wave model were used to simulate water exchange in 2008 and the wave-induced shear velocity field in the Suur Strait respectively. Circulation model simulations demonstrated that water exchange was highly variable, that cumulative transport followed an evident seasonal cycle, and that there was an gross annual outflow of 23 km3 from the Gulf of Riga. The horizontal distribution of waveinduced shear velocity during the strong southerly wind event indicated large shear velocities and substantial horizontal variability. The shear velocities were less than the critical value for resuspension in the deep area of the Suur Strait.
20

Towards validating a last generation, integrated wave-current-sediment numerical model in coastal regions using video measurements

58%
Carniel S., Sclavo M., Archetti R.
Oceanological and Hydrobiological Studies
|
2011
|
tom 40
|
nr 4
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