2011
DOI: 10.5697/oc.53-4.925
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SatBałtyk – A Baltic environmental satellite remote sensing system – an ongoing project in Poland. Part 2: Practical applicability and preliminary results**This work was carried out within the framework of the SatBałtyk project funded by the European Union through European Regional Development Fund, (contract No. POIG.01.01.02-22-011/09 entitled ‘The Satellite Monitoring of the Baltic Sea Environment’) and also as a part of IO PAS’s statutory research.The paper was presented in part at the 6th Internationa

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Cited by 34 publications
(7 citation statements)
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“…For these reasons, remote monitoring of optical properties in the Baltic Sea has become increasingly used tool [14,15]. For example, the user-friendly monitoring system of the Baltic environment developed by a Polish research team within the 'SatBaltic' project [16,17] that provides maps of hydrodynamic and bio-optical properties in the Baltic Sea.…”
Section: Introductionmentioning
confidence: 99%
“…For these reasons, remote monitoring of optical properties in the Baltic Sea has become increasingly used tool [14,15]. For example, the user-friendly monitoring system of the Baltic environment developed by a Polish research team within the 'SatBaltic' project [16,17] that provides maps of hydrodynamic and bio-optical properties in the Baltic Sea.…”
Section: Introductionmentioning
confidence: 99%
“…Excess nutrient input is the main cause of eutrophication and, consequently, frequent algal blooms. This is why the inherent optical properties of the Baltic are measured on a regular basis, both in situ [47][48][49] and from space [50][51][52].…”
Section: Optical Characteristics Of the Background Natural Seawatermentioning
confidence: 99%
“…One such service is SatBałtyk (http://satbaltyk.iopan.gda.pl), which monitors on a continuous basis and publishes information on changes in the Baltic Sea environment on its Internet website. Every six hours each day, it shares high resolution (of 1 km) and high accuracy (of the tenth part) information on the sea surface temperature, water temperature at the following depths: 0, 3, 5, 10, 20, 30 m, and sea surface salinity [28,29].…”
Section: Other Oceanographic Measurementsmentioning
confidence: 99%
“…If one assumes that the gravitational acceleration and water density are constant, then the hydrostatic pressure will depend only on the height of the liquid column. For example, a comparison of the speed of sound in water at a depth of 0 and 1 m shows a small difference of approximately 0.01 m/s [26][27][28][29].…”
Section: Other Oceanographic Measurementsmentioning
confidence: 99%