
Elementa Science of the Anthropocene, Год журнала: 2024, Номер 12(1)
Опубликована: Янв. 1, 2024
In the Arctic Ocean peak of phytoplankton bloom occurs around period sea ice break-up. Climate change is likely to impact phenology and its crucial contribution production dynamics marine ecosystems. Here we explore quantify controls on timing spring using a one-dimensional biogeochemical/ecosystem model configured for coastal western Baffin Bay. The reproduces observations made assemblage community from an camp in region. Using sensitivity experiments, found that two essential were biomass before initiation light under level nitrate was less important. delayed up 20 days if overwintering too low. This result highlights importance survival mechanisms during polar winter pelagic ecosystem dynamics.
Язык: Английский