Autor: Zajaczkowski, W. M. - Katalog OPAC zbiorów

Skocz do pozycji: 1.

Tytuł:: Report on the development of the Vistula River plume in the coastal waters of the Gulf of Gdańsk during the May 2010 flood
Autorzy:: Zajaczkowski, M.
Darecki, M.
Szczucinski, W.
Powiązania:: https://bibliotekanauki.pl/articles/47599.pdf
Data publikacji:: 2010
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: Vistula River
river plume
flood
flood wave
Gdansk Gulf
coastal water
hydrological condition
water discharge
suspended matter
concentration
Opis:: The hydrological conditions, suspended matter concentrations and vertical par- ticulate matter flux were measured as the River Vistula flood wave (maximum discharge) was flowing into the southern part of the Gulf of Gdańsk on 26 May 2010. Extending offshore for several tens of kilometres, the river plume was well stratified, with the upper layer flowing away from the shore and the near-bottom water coastwards.
Źródło:: Oceanologia; 2010, 52, 2; 311-317
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

Artykuł

Skocz do pozycji: 2.

Tytuł:: Recent changes in sediment accumulation rates in Adventfjorden, Svalbard
Autorzy:: Zajaczkowski, M.
Szczucinski, W.
Bojanowski, R.
Powiązania:: https://bibliotekanauki.pl/articles/48792.pdf
Data publikacji:: 2004
Wydawca:: Polska Akademia Nauk. Instytut Oceanologii PAN
Tematy:: accumulation rate
caesium
subpolar fjord
210 lead
sediment
Adventfjorden
lead
137 caesium
Svalbard
Opis:: Recent sediment accumulation rates in Adventfjorden (Svalbard), a small subpolar fjord, were determined by 210Pb and 137Cs dating. Modern rates in the central basin decrease downfjord from 1.87 to 0.87 cm y−1 (2.6 to 1.19 g cm−2 y−1). Comparison of the modern values (1986–2001) with older ones (1963–86) reveals a marked increase in sediment accumulation rates in the last ten years. This correlates well with recent climate changes (warming and increase in precipitation). Comparison with particulate matter flux data indicates that a portion of the sediment is passed on to Isfjorden.
Źródło:: Oceanologia; 2004, 46, 2
0078-3234
Pojawia się w:: Oceanologia
Dostawca treści:: Biblioteka Nauki

Artykuł

Informacja