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Transparency of the Baltic Sea during the growth season 2009 according to MERIS Satellite data

 

Seppo Kaitala, FIMR, Antoine Mangin, Philippe Garnesson and Odile Fanton d’Andon, ACRI-ST



syke.jpg      Acri logo.jpg         Marcoast logo.jpg

Assessment

Decreased water transparency was observed during the spring bloom in April, May and August in the Bothnian Sea, the Archipelago Sea, the Gulf of Finland and in the Gulf of Riga.

In the summer (July), the water transparency decreased in the Northern Baltic Proper.  The water transparency increased again in August in the Southern Baltic and in the rest of Baltic area towards the late summer (September).



 

April May
Fig1April.jpg   Fig1May.jpg
   JuneJuly   
   Fig1June.jpg   Fig1July.jpg
   AugustSeptember   
   Fig1August.jpg   Fig1September.jpg

Fig. 1.  Monthly averages of water transparency (m) according to MERIS satellite observations. The white area in the Bothnian Bay is covered by ice. Click image to enlarge.

 

Technical information

 

1.       Data source: The data is provided by Marine & Coastal Environmental Information Services (MarCoast), a three year Global Monitoring for Environment and Security (GMES) Service Element started in 2005. Funding is from the European Space Agency (ESA) focusing in marine and coastal information services. The pan-European water quality assessment service is provided by ACRI-ST. The service is targeted to end-users in charge of providing information to support decisions regarding measures to take to protect lives, properties and loss of natural values in protected areas. In the case of the Baltic Sea, the purpose of the service is to provide transparency data interpreted as monthly Secchi depths for the Baltic Sea monitoring.

Ind2009fig2 .jpg
Fig. 2. In situ Secchi depth (m) against MERIS water transparency data (m) during the period 2003 to 2005 in the Gulf of Finland.
2.       Description of data: Water transparency information obtained by MERIS satellites and validated against in situ Secchi measurements. The validation shows from 2 to 3 meters distortion showing lower values measured by satellite than by the Secchi white-disc.

3.       Geographical coverage: All regions of the Baltic Sea.

4.       Temporal coverage: April 2009 to September 2009.

5.       Methodology and frequency of data collection:  Secchi depths have been evaluated daily from Meris satellite data. 

6.       Methodology of data manipulation: Monthly averages have been counted from the daily cloud free data.

7.       Strength and weakness of data: Satellite mapping provides frequent data with high spatial resolution, enabling coverage of the entire Baltic Sea. Data cannot be collected from cloud-covered areas, and this may cause bias in the monthly averages during time-periods with frequent cloudiness.

8.       Reliability, accuracy, robustness, uncertainty (at data level):   The Secchi depths are underestimated about 2 – 3 meters evaluated from satellite data. The regression of satellite data against in situ Secchi depth data explains 42 % of the variation.

9.       Further work required (for data level and indicator level):  Underestimation and distortion are considerable and satellite data analysis algorithm needs further development.

 

Return to main report:   Water transparency in the Baltic Sea between 1903 and 2007

 

For reference purposes, please cite this indicator fact sheet as follows:

[Author’s name(s)], [Year]. [Indicator Fact Sheet title]. HELCOM Indicator Fact Sheets 2009. Online. [Date Viewed], http://www.helcom.fi/environment2/ifs/en_GB/cover/.

 

Last updated:: 16 February 2010