Measurements of the absorption coefficient of chromophoric dissolved organic matter (a(y)) are needed to validate existing ocean-color algorithms. In the surface open ocean, these measurements are challenging because of low a(y) values. Yet, existing global datasets demonstrate that a(y) could contribute between 30% to 50% of the total absorption budget in the 400-450 nm spectral range, thus making accurate measurement of ay essential to constrain these uncertainties. In this study, we present a simple way of determining ay using a commercially-available insitu spectrophotometer operated in underway mode. The obtained a(y) values were validated using independent collocated measurements. The method is simple to implement, can provide measurements with very high spatio-temporal resolution, and has an accuracy of about0.0004 m(-1) and a precision of about 0.0025 m(-1) when compared to independent data (at 440 nm). The only limitation for using this method at sea is that it relies on the availability of relatively large volumes of ultrapure water. Despite this limitation, the method can deliver the a(y) data needed for validating and assessing uncertainties in ocean-colour algorithms. (C) 2017 Optical Society of America

Determination of the absorption coefficient of chromophoric dissolved organic matter from underway spectrophotometry

Organelli Emanuele;
2017

Abstract

Measurements of the absorption coefficient of chromophoric dissolved organic matter (a(y)) are needed to validate existing ocean-color algorithms. In the surface open ocean, these measurements are challenging because of low a(y) values. Yet, existing global datasets demonstrate that a(y) could contribute between 30% to 50% of the total absorption budget in the 400-450 nm spectral range, thus making accurate measurement of ay essential to constrain these uncertainties. In this study, we present a simple way of determining ay using a commercially-available insitu spectrophotometer operated in underway mode. The obtained a(y) values were validated using independent collocated measurements. The method is simple to implement, can provide measurements with very high spatio-temporal resolution, and has an accuracy of about0.0004 m(-1) and a precision of about 0.0025 m(-1) when compared to independent data (at 440 nm). The only limitation for using this method at sea is that it relies on the availability of relatively large volumes of ultrapure water. Despite this limitation, the method can deliver the a(y) data needed for validating and assessing uncertainties in ocean-colour algorithms. (C) 2017 Optical Society of America
2017
Istituto di Scienze Marine - ISMAR
chromophoric dissolved organic matter
autonomous measurements
Atlantic Ocean
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/381881
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