Remote sensing of chlorophyll in the Baltic Sea at basin scale from 1997 to 2012 using merged multi-sensor data
A 15-year (1997–2012) time series of chlorophyll <i>a</i> (Chl <i>a</i>) in the Baltic Sea, based on merged multi-sensor satellite data was analysed. Several available Chl <i>a</i> algorithms were sea-truthed against the largest in situ publicly available Chl <...
| Main Authors: | , , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2016-03-01
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| Series: | Ocean Science |
| Online Access: | http://www.ocean-sci.net/12/379/2016/os-12-379-2016.pdf |
| Summary: | A 15-year (1997–2012) time series of chlorophyll <i>a</i> (Chl <i>a</i>) in the Baltic
Sea, based on merged multi-sensor satellite data was analysed. Several
available Chl <i>a</i> algorithms were sea-truthed against the largest in situ
publicly available Chl <i>a</i> data set ever used for calibration and validation over
the Baltic region. To account for the known biogeochemical heterogeneity of
the Baltic, matchups were calculated for three separate areas: (1) the Skagerrak and Kattegat,
(2) the central Baltic, including the Baltic Proper
and the gulfs of Riga and Finland, and (3) the Gulf of Bothnia. Similarly,
within the operational context of the Copernicus Marine Environment
Monitoring Service (CMEMS) the three areas were also considered as a whole
in the analysis. In general, statistics showed low linearity. However, a
bootstrapping-like assessment did provide the means for removing the bias
from the satellite observations, which were then used to compute basin
average time series. Resulting climatologies confirmed that the three regions
display completely different Chl <i>a</i> seasonal dynamics. The Gulf of Bothnia
displays a single Chl <i>a</i> peak during spring, whereas in the Skagerrak and
Kattegat the dynamics are less regular and composed of highs and lows during
winter, progressing towards a small bloom in spring and a minimum in summer. In the
central Baltic, Chl <i>a</i> follows a dynamics of a mild spring bloom followed by a
much stronger bloom in summer. Surface temperature data are able to explain
a variable fraction of the intensity of the summer bloom in
the central Baltic.< |
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| ISSN: | 1812-0784 1812-0792 |