Abstract

Measuring the diffuse attenuation coefficient () allows for monitoring the water body’s environmental status. This parameter is of particular interest in water quality monitoring programs because it quantifies the presence of light and the euphotic zone’s depth. Citizen scientists can meaningfully contribute by monitoring water quality, complementing traditional methods by reducing monitoring costs and significantly improving data coverage, empowering and supporting decision-making. However, the quality of the acquisition of in situ underwater irradiance measurements has some limitations, especially in areas where stratification phenomena occur in the first meters of depth. This vertical layering introduces a gradient of properties in the vertical direction, affecting the associated . To detect and characterize these variations of in the water column, it needs a system of optical sensors, ideally placed in a range of a few cm, improving the low vertical accuracy. Despite that, the problem of self-shading on the instrumentation becomes critical. Here, we introduce a new concept that aims to improve the vertical accuracy of the irradiance measurements: the underwater annular irradiance (). This new concept consists of measuring the irradiance in an annular-shaped distribution. We first compute the optimal annular angle that avoids self-shading and maximizes the light captured by the sensors. Second, we use different scenarios of water types, solar zenith angle, and cloud coverage to assess the robustness of the corresponding diffuse attenuation coefficient, . Finally, we derive empirical functions for computing from . This new concept opens the possibility to a new generation of optical sensors in an annular-shaped distribution which is expected to (a) increase the vertical resolution of the irradiance measurements and (b) be easy to deploy and maintain and thus to be more suitable for citizen scientists.

Highlights

  • We generate the annular irradiances from Ea10 to Ea80 from the data set described in the case study 1

  • This study presents the underwater annular irradiance Ea as a new radiometric approach to compute underwater irradiances and its derived annular diffuse attenuation coefficient Ka as an effective proxy to estimate the downwelling diffuse attenuation coefficient Kd in the PAR region

  • We find that the optimal angle to measure underwater annular irradiance is at 40 degrees, which is the angle measured from the z-axis in spherical coordinates

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Summary

Introduction

This radiation at the sea surface is conventionally measured as spectrally resolved downward planar irradiance, Ed (λ), and the attenuation of this quantity with depth (z) can be described by the diffuse attenuation coefficient Kd (z, λ) [4]. This parameter is of particular interest in water quality monitoring programs because it represents 4.0/). Monitoring water transparency provides an indicator of the environmental status of the water body by providing information about phytoplankton concentrations or levels of dissolved organic and inorganic compounds This is especially relevant in coastal areas and lakes that are strongly affected by human activities and rivers, winds, and waves

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