Effect of wind speed on the size distribution of gel particles in the sea surface microlayer: insights from a wind–wave channel experiment

Gel particles, such as transparent exopolymer particles (TEP) and Coomassie stainable particles (CSP), are important organic components in the sea surface microlayer (SML). Here, we present results on the effect of different wind speeds on the accumulation and size distribution of TEP and CSP du...

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Main Authors: C.-C. Sun, M. Sperling, A. Engel
Format: Article
Language:English
Published: Copernicus Publications 2018-06-01
Series:Biogeosciences
Online Access:https://www.biogeosciences.net/15/3577/2018/bg-15-3577-2018.pdf
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spelling doaj-5bb71015c82b42f280861d6a752b82d92020-11-24T21:37:58ZengCopernicus PublicationsBiogeosciences1726-41701726-41892018-06-01153577358910.5194/bg-15-3577-2018Effect of wind speed on the size distribution of gel particles in the sea surface microlayer: insights from a wind–wave channel experimentC.-C. Sun0C.-C. Sun1C.-C. Sun2M. Sperling3A. Engel4GEOMAR Helmholtz Centre for Ocean Research Kiel, 24105 Kiel, GermanyState Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, 510301, Guangzhou, ChinaDaya Bay Marine Biology Research Station, Chinese Academy of Sciences, 518000, Shenzhen, ChinaGEOMAR Helmholtz Centre for Ocean Research Kiel, 24105 Kiel, GermanyGEOMAR Helmholtz Centre for Ocean Research Kiel, 24105 Kiel, GermanyGel particles, such as transparent exopolymer particles (TEP) and Coomassie stainable particles (CSP), are important organic components in the sea surface microlayer (SML). Here, we present results on the effect of different wind speeds on the accumulation and size distribution of TEP and CSP during a wind wave channel experiment in the Aeolotron. Total areas of TEP (TEP<sub>SML</sub>) and CSP (CSP<sub>SML</sub>) in the surface microlayer were exponentially related to wind speed. At wind speeds  &lt;  6 m s<sup>−1</sup>, accumulation of TEP<sub>SML</sub> and CSP<sub>SML</sub> occurred, decreasing at wind speeds of  &gt;  8 m s<sup>−1</sup>. Wind speeds  &gt;  8 m s<sup>−1</sup> also significantly altered the size distribution of TEP<sub>SML</sub> in the 2–16 µm size range towards smaller sizes. The response of the CSP<sub>SML</sub> size distribution to wind speed varied through time depending on the biogenic source of gels. Wind speeds  &gt;  8 m s<sup>−1</sup> decreased the slope of CSP<sub>SML</sub> size distribution significantly in the absence of autotrophic growth. For the slopes of TEP and CSP size distribution in the bulk water, no significant difference was observed between high and low wind speeds. Changes in spectral slopes between high and low wind speed were higher for TEP<sub>SML</sub> than for CSP<sub>SML</sub>, indicating that the impact of wind speed on size distribution of gel particles in the SML may be more pronounced for TEP than for CSP, and that CSP<sub>SML</sub> are less prone to aggregation during the low wind speeds. Addition of an <i>E. huxleyi</i> culture resulted in a higher contribution of submicron gels (0.4–1 µm) in the SML at higher wind speed ( &gt;  6 m s<sup>−1</sup>), indicating that phytoplankton growth may potentially support the emission of submicron gels with sea spray aerosol.https://www.biogeosciences.net/15/3577/2018/bg-15-3577-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author C.-C. Sun
C.-C. Sun
C.-C. Sun
M. Sperling
A. Engel
spellingShingle C.-C. Sun
C.-C. Sun
C.-C. Sun
M. Sperling
A. Engel
Effect of wind speed on the size distribution of gel particles in the sea surface microlayer: insights from a wind–wave channel experiment
Biogeosciences
author_facet C.-C. Sun
C.-C. Sun
C.-C. Sun
M. Sperling
A. Engel
author_sort C.-C. Sun
title Effect of wind speed on the size distribution of gel particles in the sea surface microlayer: insights from a wind–wave channel experiment
title_short Effect of wind speed on the size distribution of gel particles in the sea surface microlayer: insights from a wind–wave channel experiment
title_full Effect of wind speed on the size distribution of gel particles in the sea surface microlayer: insights from a wind–wave channel experiment
title_fullStr Effect of wind speed on the size distribution of gel particles in the sea surface microlayer: insights from a wind–wave channel experiment
title_full_unstemmed Effect of wind speed on the size distribution of gel particles in the sea surface microlayer: insights from a wind–wave channel experiment
title_sort effect of wind speed on the size distribution of gel particles in the sea surface microlayer: insights from a wind–wave channel experiment
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2018-06-01
description Gel particles, such as transparent exopolymer particles (TEP) and Coomassie stainable particles (CSP), are important organic components in the sea surface microlayer (SML). Here, we present results on the effect of different wind speeds on the accumulation and size distribution of TEP and CSP during a wind wave channel experiment in the Aeolotron. Total areas of TEP (TEP<sub>SML</sub>) and CSP (CSP<sub>SML</sub>) in the surface microlayer were exponentially related to wind speed. At wind speeds  &lt;  6 m s<sup>−1</sup>, accumulation of TEP<sub>SML</sub> and CSP<sub>SML</sub> occurred, decreasing at wind speeds of  &gt;  8 m s<sup>−1</sup>. Wind speeds  &gt;  8 m s<sup>−1</sup> also significantly altered the size distribution of TEP<sub>SML</sub> in the 2–16 µm size range towards smaller sizes. The response of the CSP<sub>SML</sub> size distribution to wind speed varied through time depending on the biogenic source of gels. Wind speeds  &gt;  8 m s<sup>−1</sup> decreased the slope of CSP<sub>SML</sub> size distribution significantly in the absence of autotrophic growth. For the slopes of TEP and CSP size distribution in the bulk water, no significant difference was observed between high and low wind speeds. Changes in spectral slopes between high and low wind speed were higher for TEP<sub>SML</sub> than for CSP<sub>SML</sub>, indicating that the impact of wind speed on size distribution of gel particles in the SML may be more pronounced for TEP than for CSP, and that CSP<sub>SML</sub> are less prone to aggregation during the low wind speeds. Addition of an <i>E. huxleyi</i> culture resulted in a higher contribution of submicron gels (0.4–1 µm) in the SML at higher wind speed ( &gt;  6 m s<sup>−1</sup>), indicating that phytoplankton growth may potentially support the emission of submicron gels with sea spray aerosol.
url https://www.biogeosciences.net/15/3577/2018/bg-15-3577-2018.pdf
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