Abstract

Potential zone for photosynthesis in natural waters is restricted to a relatively thin illuminated surface water layer. The thickness of this layer is often indirectly estimated by measuring the depth in which 1% of the photosynthetically active radiation entering the water remains. This depth is referred to as the euphotic depth. A coarser way to evaluate the underwater light penetration is to measure the Secchi depth, which is a visual measure of water transparency. The numerical relationship between these two optical parameters, i.e., conversion coefficient m, varies according to the changes in the optical properties of water, especially in transitional coastal waters. The aim of our study is to assess which is the most suitable criterion to base these coefficients on. We tested nine methods, seven of which were locally calibrated with our own in situ data from the optically heterogeneous Baltic Sea archipelago coast of SW Finland. We managed to significantly improve the accuracy of modeling euphotic depths from Secchi depths by using scalable and locally calibrated methods instead of a single fixed coefficient. The best results were achieved by using methods, either continuous functions or series of constants, which are based on water transparency values.

Highlights

  • Underwater light is an important environmental variable because its low availability limits the photosynthetic activity, and thereby the primary production of the aquatic ecosystem [1]

  • Light is attenuated by water molecules, suspended particulate matter (SPM), colored dissolved organic matter (CDOM, yellow substances), and chlorophyll along with other photosynthetic pigments of living phytoplankton

  • The original training data included a total of 88 Secchi depths and light profiles

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Summary

Introduction

Underwater light is an important environmental variable because its low availability limits the photosynthetic activity, and thereby the primary production of the aquatic ecosystem [1]. Light is attenuated by water molecules, suspended particulate matter (SPM), colored dissolved organic matter (CDOM, yellow substances), and chlorophyll along with other photosynthetic pigments of living phytoplankton. Each of these components attenuates light from different wavelengths, and some components are primarily absorbers and some scatterers. The thickness of the photosynthetically active water layer can be assessed by comparing the amounts of photoautotrophic production and heterotrophic consumption, but it can be roughly estimated by measuring the amount of light in the water column, e.g., [1]. A common variable is the euphotic depth (Zeu), which is relatively easy and accurate to determine [2] by measuring the depth in which 1% of the photosynthetically active radiation (PAR, 400–700 nm) entering the water remains

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