2021
DOI: 10.1007/978-3-030-87683-8_1
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Light-Absorbing Particles in Snow and Ice: A Brief Journey Across Latitudes

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Cited by 9 publications
(2 citation statements)
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“…While most of the surface snow in the interior of the Antarctic Ice Sheet is uncontaminated, on the margins of the continent several processes occur and they can deposit or resurface light-absorbing particles, as observed in different studies (Dadic et al, 2013;Casey et al, 2017;Warren, 2019a;2019b;Kavan et al, 2020;Di Mauro et al, 2021;Gray et al, 2021;Cordero et al, 2022). Recent observation from the Antarctic Peninsula showed that surface snow may contain cryospheric algae (Gray et al, 2020(Gray et al, , 2021 and black carbon (Cordero et al, 2022).…”
Section: Introductionmentioning
confidence: 96%
“…While most of the surface snow in the interior of the Antarctic Ice Sheet is uncontaminated, on the margins of the continent several processes occur and they can deposit or resurface light-absorbing particles, as observed in different studies (Dadic et al, 2013;Casey et al, 2017;Warren, 2019a;2019b;Kavan et al, 2020;Di Mauro et al, 2021;Gray et al, 2021;Cordero et al, 2022). Recent observation from the Antarctic Peninsula showed that surface snow may contain cryospheric algae (Gray et al, 2020(Gray et al, , 2021 and black carbon (Cordero et al, 2022).…”
Section: Introductionmentioning
confidence: 96%
“…Surface and volume scattering governs ice reflection characteristics (Gardner & Sharp, 2010), and increasing ice thickness can increase the albedo (Grenfell & Perovich, 1984). An increase in pollutants content can weaken the ice reflection signature, similar to the effects of impurities in the snow (Di Mauro et al., 2021). Moreover, increasing bubbles and salt cell radius can enhance volume scattering intensity and increase ice reflection (Carns et al., 2015; Dadic et al., 2013).…”
Section: Introductionmentioning
confidence: 99%