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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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 < 6 m s<sup>−1</sup>, accumulation of TEP<sub>SML</sub> and CSP<sub>SML</sub> occurred, decreasing at wind speeds of > 8 m s<sup>−1</sup>. Wind speeds > 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 > 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 ( > 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 < 6 m s<sup>−1</sup>,
accumulation of TEP<sub>SML</sub> and CSP<sub>SML</sub> occurred, decreasing at wind
speeds of > 8 m s<sup>−1</sup>. Wind speeds > 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 > 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
( > 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 |
work_keys_str_mv |
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