Geoscience Reference
In-Depth Information
Fig. 20.3
Secchi depth measurement (Photo: Susanne Kratzer, Irish Sea 1997)
been explained by the increase in phytoplankton biomass (Sandén and Håkansson
the coastal areas and the Stockholm archipelago, a recovery of the Secchi depth has
been observed over the last decade, whereas the decreasing trend seems to continue
Another way to measure water transparency is by measuring the rate of decrease
of light with depth. Light energy which enters the water from above and is transmit-
ted downwards is known as downwelling irradiance,
E
d
.
In the case of monochro-
matic light with uniform angular distribution
E
d
diminishes in an approximately
exponential manner with depth:
E
d
(0) e
−
K
d
Z
(Beer's Law)
E
d
(
z
)
=
where
E
d
(0) and
E
d
(
z
) are the values of downward irradiance just below the surface
uation coefficient for the downwelling light field over any defined depth interval;
note that
K
d
, the rate of light decrease, is wavelength dependent. The diffuse attenu-
concentration but also by CDOM and TSM load. Secchi depth can therefore only
be used as an indicator for eutrophication where phytoplankton clearly dominates
the two other optical components.
Chemical parameters such as the nutrient concentrations cannot be retrieved opti-
cally as they do not sufficiently interact with light. However, they may be retrieved
indirectly, e.g. by relating Secchi depth to the total nitrogen concentration (Tett et al.