Zobrazeno 1 - 10
of 41
pro vyhledávání: '"M.-J. Lilover"'
Publikováno v:
Ocean Science, Vol 18, Pp 857-879 (2022)
Circulation plays an essential role in the creation of physical and biogeochemical fluxes in the Baltic Sea. The main aim of the work was to study the quasi-steady circulation patterns under prevailing forcing conditions. A total of 6 months of con
Externí odkaz:
https://doaj.org/article/00b3afe3d57641acb02e72e0276925e9
Publikováno v:
Ocean Science, Vol 16, Pp 1475-1490 (2020)
Stratification plays an essential role in the marine ecosystem, with a shallow mixed layer being one of the preconditions for enhanced primary production in the ocean. In the Baltic Sea, the general understanding is that the upper mixed layer (UML) i
Externí odkaz:
https://doaj.org/article/d1eb2f19f1394bc3b94faff6bda3e500
Akademický článek
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Publikováno v:
Journal of Marine Systems. 129:66-75
This study aims to explain those factors influencing low-frequency currents in a shallow unstratified sea with complex topography. Current velocity measurements using a bottom-mounted ADCP, deployed at 8 m depth on the slope of Naissaar Bank (norther
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c1a99fea1926791fbb712e96fa481bf
https://doi.org/10.1016/j.jmarsys.2013.06.008
https://doi.org/10.1016/j.jmarsys.2013.06.008
Akademický článek
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Autor:
A. Stips, M.-J. Lilover
Publikováno v:
Journal of Marine Systems. 74:S108-S115
The formation of wintertime excess dissolved inorganic phosphorus concentration (eDIP) in the surface layer and its influence on the late-summer diazotrophic cyanobacteria development have been evaluated on the base of 30 years nutrients and river ru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e4019e5c241bde87b48108f9d0a3169
https://doi.org/10.1016/j.jmarsys.2008.03.029
https://doi.org/10.1016/j.jmarsys.2008.03.029
Autor:
M.-J Lilover, L. Talpsepp
Publikováno v:
2014 IEEE/OES Baltic International Symposium (BALTIC).
The aim of this study was to determine the depths which were most influenced by low-frequency motions and to reveal the processes behind the observed distribution of kinetic energy. The long term records of five bottom-mounted ADCP deployed along the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c674988a5b769c421e5196002a9270cb
https://doi.org/10.1109/baltic.2014.6887844
https://doi.org/10.1109/baltic.2014.6887844
Publikováno v:
2014 IEEE/OES Baltic International Symposium (BALTIC).
The winter navigation occurs mostly in ice channels, which icebreakers break into the fast or drift ice. Every ship proceeding in such an ice channel experiences the ice resistance, which influences the ship speed and navigational capabilities. Marit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be3eda9a59c6b0e77453a4396738d446
https://doi.org/10.1109/baltic.2014.6887861
https://doi.org/10.1109/baltic.2014.6887861
Autor:
T. Kouts, M.-J. Lilover
Publikováno v:
2012 IEEE/OES Baltic International Symposium (BALTIC).
Ice compression is serious navigational hazard for all ships proceeding in ice. In most cases no obvious indications of compression precense can be observed from the ice surface, the phenomenon could activate and develop very fast being sometimes loc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd15541b3e7772c6a589cc7941307960
https://doi.org/10.1109/baltic.2012.6249187
https://doi.org/10.1109/baltic.2012.6249187
Autor:
M.-J. Lilover
Publikováno v:
2012 IEEE/OES Baltic International Symposium (BALTIC).
The Baltic Sea has been usually described as “practically non-tidal sea”. The statement is motivated by the landlocked intracontinental location of the sea connected to the ocean (North Sea) via narrow and sallow Danish Straits (Belt Sea). For mo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0e6016cd340584f45eabd810829d7cc4
https://doi.org/10.1109/baltic.2012.6249181
https://doi.org/10.1109/baltic.2012.6249181