In addition, as the deeper layers have an earlier impact on the transport of nutrients during the upwelling along the southern coast, the total amounts of nutrients transported to the upper 10-m layer were larger during the upwelling along the southern coast. During the upwelling along the northern coast, water masses from depths of > 50 m reached the upper 10-m layer at least 1.5 days later and

the total amount of nutrients transported to the surface layer were therefore lower compared than that off the southern coast. The aim of this paper was to describe nutrient transport from different depths to the surface layer during an upwelling event in the Gulf of Finland. Modelling results showed that during upwelling events off either the northern or the VEGFR inhibitor southern coast of the Gulf, the highest phosphorus transport to the upper 10-m layer was from depths buy RAD001 shallower than 35 m. The largest amounts of nitrogen were transported to the surface layer from depths of 40–50 m off the northern and 40–60 m off the southern coast. The volume of water transported to the upper 10-m layer from the deeper layers is greater during the upwelling along the southern coast – there was a clear decrease in the water volume reaching the surface layer from depths greater than 50 m during the upwelling along the northern coast. The impact of the upwelling wind impulse

was higher on the southern coast; the transport of water from deeper layers started earlier than on the northern coast. Owing to the earlier transport from the bottom layers during the upwelling along the southern coast, the total amount of nutrients transported to the upper 10-m layer at the culmination of the event are larger during the upwelling along the southern coast. Although the reduction in wind stress lowered the amounts of nutrients transported to the upper 10-m layer during the Histamine H2 receptor upwelling event on both coasts, the main transport of phosphorus remained at the depths of 15– 25 m. Nitrogen transport from the deeper layers was vanishingly small for the upwelling along the northern coast, whereas for the southern coast, the largest transport remained in the depth range of 40–55 m. The Finnish Meteorological Institute

kindly provided wind data. Special thanks go to Oleg Andrejev for supplying the meteorological data. We also thank the anonymous reviewers for their constructive recommendations. “
“The numerous threats and natural disasters elicited by changes in the environment have persuaded experts to radically intensify ecological investigations and forecasts at a regional and global scale. A key part in these changes is played by marine ecosystems, especially the organic matter production processes occurring in them. Marine production is the most important mechanism of carbon exchange between the sea and the atmosphere and therefore requires to be monitored continuously with both traditional methods (from on board ship) and modern remote sensing techniques.