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partially influenced by inflowing water from the Kattegat. In the Eastern Gotland Basin deep water, nutrient levels were clearly affected by the variations between completely oxygen-free and oxygenated water below the halocline. The levels of both inorganic nitrogen and phosphate increased at 70 - 80 m Last updated: Jan 21, 2020

produce even more specific and detailed information. All knowledge needs to be updated regularly to reflect the evolving state of science. Focus Although we know that climate is changing and that the society has to adapt to that, there is still information missing. Both in terms of how climate actually Last updated: Aug 19, 2021

over 80-90 meters, in the Eastern Gotland basin at intermediate depth and at the bottom. Due to a longer period with strong northerly/easterly winds and high air pressure over the Baltic, the water level is now low in the whole Baltic Sea. This provides favourable conditions for a new large inflow to Last updated: Oct 19, 2016

oxygenated zones below the intermediary layer, does influence the sediment to water nutrient exchange. Areal extent and volumes are presented in relation to the area and volume of the Baltic Proper, including the Gulf of Finland and the Gulf of Riga, see Figure 1[Fonselius, 1995]. Report Oceanography No. 58 Last updated: Feb 10, 2017

the dynamics and variability is often required to predict accurately light penetration and hereafter e.g. primary production. The present st udy i s a first attempt to include CDOM into a Balt ic Sea model. The model integrations a re b ased on a fixe d c oncentration in the 30 m ajor rivers. I n t he Last updated: Nov 26, 2015

the dynamics and variability is often required to predict accurately light penetration and hereafter e.g. primary production. The present st udy i s a first attempt to include CDOM into a Balt ic Sea model. The model integrations a re b ased on a fixe d c oncentration in the 30 m ajor rivers. I n t he Last updated: Nov 26, 2015

(SMHI) Language English A FIELD TEST OF THERMOMETER SCREENS by Tage Andersson and Ingemar Mattisson Swedish Meteorological and Hydrological Institute (SMHI) l. lntroduction For small temperature sensors used in automatic data acquisition systems the old conventional screens, capable of housing several Last updated: Jun 03, 2019

atmospheric weather data are taken from some externa! source and fed into the model at regular time intervals, normally every 3 or 6 hours. Such data are usually interpolated in time to yield hourly data. Special attention is given to interpolation of the horizontal wind where vector increments are applied Last updated: Mar 30, 2020

. Concentrations of dissolved inorganic phosphorus, DIP (only in the form of phosphate), were on normal levels, somewhat higher at Å13 down to 40 metres and at Å15 between 10 and 40 metres. Values in the surface water went from around 0.4 µmol/l closest to the coast down to around 0.2 µmol/l in the open sea at Å17 Last updated: Nov 28, 2017

The surface water temperature was well above normal and ranged between 4 - 6°C which is about 2-3°C above normal for the season. The deep waters in the Baltic Proper were also warmer than normal. In the Baltic Proper, the salinity was higher than usual. The concentrations of dissolved inorganic Last updated: Mar 30, 2020