The Baltic Region

2011 Issue №1(7)

Back to the list Download the article

An assessment of the potential impact of the construction of a deepwater seaport on the hydrological regime of the Vistula lagoon

DOI
10.5922/2079-8555-2011-1-6
Pages
48-53

Abstract

This article focuses on the level fluctuation in the Vistula Lagoon. In view of the planned construction of a deepwater seaport in its waters, the author emphasizes the negative impact on its hydrological regime: rise in the levels which could lead to the flooding of the territories adjoining the mouth of the Pregolya river, increase in salinity, extinction of hydrobionts, and destruction of the ecological systems.

Reference

1. Volcinger, V. E. Pjaskovskij, R. V. 1977. Teorija melkoj vody. Leningrad.
2. Velander, P. 1964. Chislennoe predskazanie shtormovyh nagonov. Leningrad,pp. 10—46.
3. Sergeeva, L. G. 2005. Povyshenie urovennoj poverhnosti morja i temperatury vozduha v jugo-vostochnoj chasti Baltijskogo morja kak projavlenie global'nyh processov.In: Bezopasnost' moreplavanija i nadezhnost' sudovyh tehnicheskih sredstv.Saint Petersburg, pp. 180—185.
4. Sergeeva, L., Krasnov, E. 2001. The Baltik — Sea-level events in the system of global change. Third Study Conference on BALTEX. Assembly Hall of Alands Parlament Building Mariehamn, Aland, Finland, pp. 119—120.
5. Sergeeva, L. G. 2003. Mehanizm nagonnyh javlenij i ego osobennosti u poberezh'ja juzhnoj chasti Baltijskogo morja. In: Jekologija regiona Baltijskogo morja.Kaliningrad, pp. 12—18.
6. Inzhebejkin, Ju. I. 2003. Kolebanija urovnja Belogo morja. Ekaterinburg.
7. Davydenko, L. I., Ljadvik, N. S. 2001. Kaliningradskij morskoj kanal. Kaliningrad.
8. Mihajlov, V. N. 1998. Geografija, № 37, pp. 1—3.