Maintenance of coastal surface blooms by surface temperature stratification and wind drift.

Algae blooms are an increasingly recurrent phenomenon of potentially socio-economic impact in coastal waters globally and in the coastal upwelling region off northern Baja California, Mexico. In coastal upwelling areas the diurnal wind pattern is directed towards the coast during the day. We regular...

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Main Authors: Mary Carmen Ruiz-de la Torre, Helmut Maske, José Ochoa, César O Almeda-Jauregui
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2013-01-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC3623857?pdf=render
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spelling doaj-dd8fd75862af4c65b4f8fd844dd1f4192020-11-25T02:42:36ZengPublic Library of Science (PLoS)PLoS ONE1932-62032013-01-0184e5895810.1371/journal.pone.0058958Maintenance of coastal surface blooms by surface temperature stratification and wind drift.Mary Carmen Ruiz-de la TorreHelmut MaskeJosé OchoaCésar O Almeda-JaureguiAlgae blooms are an increasingly recurrent phenomenon of potentially socio-economic impact in coastal waters globally and in the coastal upwelling region off northern Baja California, Mexico. In coastal upwelling areas the diurnal wind pattern is directed towards the coast during the day. We regularly found positive Near Surface Temperature Stratification (NSTS), the resulting density stratification is expected to reduce the frictional coupling of the surface layer from deeper waters and allow for its more efficient wind transport. We propose that the net transport of the top layer of approximately 2.7 kilometers per day towards the coast helps maintain surface blooms of slow growing dinoflagellate such as Lingulodinium polyedrum. We measured: near surface stratification with a free-rising CTD profiler, trajectories of drifter buoys with attached thermographs, wind speed and direction, velocity profiles via an Acoustic Doppler Current Profiler, Chlorophyll and cell concentration from water samples and vertical migration using sediment traps. The ADCP and drifter data agree and show noticeable current shear within the first meters of the surface where temperature stratification and high cell densities of L. polyedrum were found during the day. Drifters with 1m depth drogue moved towards the shore, whereas drifters at 3 and 5 m depth showed trajectories parallel or away from shore. A small part of the surface population migrated down to the sea floor during night thus reducing horizontal dispersion. The persistent transport of the surface bloom population towards shore should help maintain the bloom in favorable environmental conditions with high nutrients, but also increasing the potential socioeconomic impact of the blooms. The coast wise transport is not limited to blooms but includes all dissolved and particulate constituents in surface waters.http://europepmc.org/articles/PMC3623857?pdf=render
collection DOAJ
language English
format Article
sources DOAJ
author Mary Carmen Ruiz-de la Torre
Helmut Maske
José Ochoa
César O Almeda-Jauregui
spellingShingle Mary Carmen Ruiz-de la Torre
Helmut Maske
José Ochoa
César O Almeda-Jauregui
Maintenance of coastal surface blooms by surface temperature stratification and wind drift.
PLoS ONE
author_facet Mary Carmen Ruiz-de la Torre
Helmut Maske
José Ochoa
César O Almeda-Jauregui
author_sort Mary Carmen Ruiz-de la Torre
title Maintenance of coastal surface blooms by surface temperature stratification and wind drift.
title_short Maintenance of coastal surface blooms by surface temperature stratification and wind drift.
title_full Maintenance of coastal surface blooms by surface temperature stratification and wind drift.
title_fullStr Maintenance of coastal surface blooms by surface temperature stratification and wind drift.
title_full_unstemmed Maintenance of coastal surface blooms by surface temperature stratification and wind drift.
title_sort maintenance of coastal surface blooms by surface temperature stratification and wind drift.
publisher Public Library of Science (PLoS)
series PLoS ONE
issn 1932-6203
publishDate 2013-01-01
description Algae blooms are an increasingly recurrent phenomenon of potentially socio-economic impact in coastal waters globally and in the coastal upwelling region off northern Baja California, Mexico. In coastal upwelling areas the diurnal wind pattern is directed towards the coast during the day. We regularly found positive Near Surface Temperature Stratification (NSTS), the resulting density stratification is expected to reduce the frictional coupling of the surface layer from deeper waters and allow for its more efficient wind transport. We propose that the net transport of the top layer of approximately 2.7 kilometers per day towards the coast helps maintain surface blooms of slow growing dinoflagellate such as Lingulodinium polyedrum. We measured: near surface stratification with a free-rising CTD profiler, trajectories of drifter buoys with attached thermographs, wind speed and direction, velocity profiles via an Acoustic Doppler Current Profiler, Chlorophyll and cell concentration from water samples and vertical migration using sediment traps. The ADCP and drifter data agree and show noticeable current shear within the first meters of the surface where temperature stratification and high cell densities of L. polyedrum were found during the day. Drifters with 1m depth drogue moved towards the shore, whereas drifters at 3 and 5 m depth showed trajectories parallel or away from shore. A small part of the surface population migrated down to the sea floor during night thus reducing horizontal dispersion. The persistent transport of the surface bloom population towards shore should help maintain the bloom in favorable environmental conditions with high nutrients, but also increasing the potential socioeconomic impact of the blooms. The coast wise transport is not limited to blooms but includes all dissolved and particulate constituents in surface waters.
url http://europepmc.org/articles/PMC3623857?pdf=render
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