Temat: process condition - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Spatiotemporal changes in the concentration and composition of suspended particulate matter in front of Hansbreen, a tidewater glacier in Svalbard
Autorzy:: Moskalik, M.
Cwiakala, J.
Szczucinski, W.
Dominiczak, A.
Glowacki, O.
Wojtysiak, K.
Zagorski, P.
Powiązania:: https://bibliotekanauki.pl/articles/958169.pdf
Data publikacji:: 2018
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: tidewater glacier
suspended particulate matter
particulate organic matter
Hansbreen glacier
Svalbard Fjord
biological process
meteorological condition
oceanographic condition
glacial bay
Źródło:: Oceanologia; 2018, 60, 4
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 2.

Tytuł:: Effect of drag coefficient formula choice on wind stress climatology in the North Atlantic and the European Arctic
Autorzy:: Wrobel-Niedzwiecka, I.
Drozdowska, V.
Piskozub, J.
Powiązania:: https://bibliotekanauki.pl/articles/48480.pdf
Data publikacji:: 2019
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: drag coefficient
parametrization
boundary condition system
wind stress
climatology
physical process
biogeochemical process
European Arctic
North Atlantic
wind field
Źródło:: Oceanologia; 2019, 61, 3
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 3.

Tytuł:: Relationships between coastal processes and properties of the nearshore sea bed dynamic layer
Autorzy:: Ostrowski, R.
Pruszak, Z.
Powiązania:: https://bibliotekanauki.pl/articles/47468.pdf
Data publikacji:: 2011
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: Baltic coast
Baltic dune
cliff
coastal process
coastal zone
geomorphological condition
hydrodynamic impact
Polska
sandy sediment
sediment transport
Opis:: The paper discusses the notion of a layer of sandy sediments overlying a substratum of cohesive deposits in the coastal zone. This layer of sand is generally more mobile and is therefore conventionally referred to as the dynamic layer. Its parameters are important to coastal lithodynamic and morphodynamic processes caused by waves and currents. On the other hand, the dynamic layer is formed by nearshore hydrodynamic impact. The variability of the features of the dynamic layer on the southern Baltic dune and cliff shores in Poland is analysed on the basis of selected geological data supported by local seismo-acoustic field investigations. It appears that the conventional notion of the dynamic layer makes sense only in specific geomorphologic conditions. In such cases, mostly related to cliff shores, theoretical modelling of sediment transport should take the properties of the dynamic layer into account.
Źródło:: Oceanologia; 2011, 53, 3
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

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Skocz do pozycji: 4.

Tytuł:: Morphological and lithodynamic conditions in the marine coastal zone of the Vistula Spit (Gulf of Gdansk, Baltic Sea)
Autorzy:: Kobelyanskaya, J.
Bobykina, V.P.
Piekarek-Jankowska, H.
Powiązania:: https://bibliotekanauki.pl/articles/48143.pdf
Data publikacji:: 2011
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: Baltic Sea
coastal process
coastal zone
dynamic environment
Gdansk Gulf
grain size
lithodynamic condition
morphology
Vistula River
Vistula Spit
Opis:: The paper presents a lithodynamic interpretation of the Polish-Russian morpholog- ical and lithological research project along the marine coastal zone of the Vistula Spit, carried out between July and September 2008. 78.4% of the coastal zone is characterized by a balanced environment, with fractional transport of sediments as bed and suspended load. Deposition was observed in 8.2% of the study area. A dynamic environment with a deficit of bed material, local turbulences and erosive trends were found in 13.2% of the coastal zone. The critical erosive current velocities vary from 16 to 20–26 cm s−1.
Źródło:: Oceanologia; 2011, 53, 4
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki