Under-ice light field analysis in the western Arctic Ocean during late summer

Veyssière, Gaëlle; Castellani, Giulia; Wilkinson, Jeremy ORCID: https://orcid.org/0000-0002-7166-3042; Karcher, Michael; Hayward, Alexander; Stroeve, Julienne C.; Nicolaus, Marcel; Kim, Joo-Hong; Yang, Eun-Jin; Valcic, Lovro; Kauker, Frank; Khan, Alia L.; Rogers, Indea; Jung, Jinyoung. 2022 Under-ice light field analysis in the western Arctic Ocean during late summer. Frontiers in Earth Science, 9, 643737. https://doi.org/10.3389/feart.2021.643737

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Text (Open Access) Copyright © 2022 Veyssière, Castellani, Wilkinson, Karcher, Hayward, Stroeve, Nicolaus, Kim, Yang, Valcic, Kauker, Khan, Rogers and Jung. feart-09-643737.pdf - Published Version Available under License Creative Commons Attribution 4.0. Download (3MB) | Preview

Abstract/Summary

The Arctic is no longer a region dominated by thick multi-year ice (MYI), but by thinner, more dynamic, first-year-ice (FYI). This shift towards a seasonal ice cover has consequences for the under-ice light field, as sea-ice and its snow cover are a major factor influencing radiative transfer and thus, biological activity within- and under the ice. This work describes in situ measurements of light transmission through different types of sea-ice (MYI and FYI) performed during two expeditions to the Chukchi sea in August 2018 and 2019, as well as a simple characterisation of the biological state of the ice microbial system. Our analysis shows that, in late summer, two different states of FYI exist in this region: 1) FYI in an enhanced state of decay, and 2) robust FYI, more likely to survive the melt season. The two FYI types have different average ice thicknesses: 0.74 ± 0.07 m (N = 9) and 0.93 ± 0.11 m (N = 9), different average values of transmittance: 0.15 ± 0.04 compared to 0.09 ± 0.02, and different ice extinction coefficients: 1.49 ± 0.28 and 1.12 ± 0.19 m−1. The measurements performed over MYI present different characteristics with a higher average ice thickness of 1.56 ± 0.12 m, lower transmittance (0.05 ± 0.01) with ice extinction coefficients of 1.24 ± 0.26 m−1 (N = 12). All ice types show consistently low salinity, chlorophyll a concentrations and nutrients, which may be linked to the timing of the measurements and the flushing of melt-water through the ice. With continued Arctic warming, the summer ice will continue to retreat, and the decayed variant of FYI, with a higher scattering of light, but a reduced thickness, leading to an overall higher light transmittance, may become a more relevant ice type. Our results suggest that in this scenario, more light would reach the ice interior and the upper-ocean.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.3389/feart.2021.643737
ISSN:	1364503X
Additional Keywords:	transmittance, arctic, late summer, first-year ice, ice extinction coefficient, under-ice irradiance
Date made live:	23 Feb 2022 15:35 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/527063

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