Cited by 40Marine and coastal ecosystemsOceanographic and Atmospheric ProcessesAtmospheric aerosols and clouds

Biological response to coastal upwelling and dust deposition in the area off Northwest Africa

Ohde, T., Siegel, H.·2010·Continental Shelf Research

Abstract

Nutrient supply in the area off Northwest Africa is mainly regulated by two processes, coastal upwelling and deposition of Saharan dust. In the present study, both processes were analyzed and evaluated by different methods, including cross-correlation, multiple correlation, and event statistics, using remotely sensed proxies of the period from 2000 to 2008 to investigate their influence on the marine environment. The remotely sensed chlorophyll-a concentration was used as a proxy for the phytoplankton biomass stimulated by nutrient supply into the euphotic zone from deeper water layers and from the atmosphere. Satellite-derived alongshore wind stress and sea-surface temperature were applied as proxies for the strength and reflection of coastal upwelling processes. The westward wind and the dust component of the aerosol optical depth describe the transport direction of atmospheric dust and the atmospheric dust column load. Alongshore wind stress and induced upwelling processes were most significantly responsible for the surface chlorophyll-a variability, accounting for about 24% of the total variance, mainly in the winter and spring due to the strong north-easterly trade winds. The remotely sensed proxies allowed determination of time lags between biological response and its forcing processes. A delay of up to 16 days in the surface chlorophyll-a concentration due to the alongshore wind stress was determined in the northern winter and spring. Although input of atmospheric iron by dust storms can stimulate new phytoplankton production in the study area, only 5% of the surface chlorophyll-a variability could be ascribed to the dust component in the aerosol optical depth. All strong desert storms were identified by an event statistics in the time period from 2000 to 2008. The 57 strong storms were studied in relation to their biological response. Six events were clearly detected in which an increase of chlorophyll-a was caused by Saharan dust input and not by coastal upwelling processes. Time lags of <8 days, 8 days, and 16 days were determined. An increase in surface chlorophyll-a concentration of up to 2.4 mg m-3 after dust storms in which the dust component of the aerosol optical depth was up to 0.9 was observed. © 2010 Elsevier Ltd. All rights reserved.

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Crossref · 10.1016/j.csr.2010.02.016

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Research works printed but not linked: 5

  1. Eppley, 1972, Temperature and phytoplankton growth in the sea, Fishery Bulletin, 70, 1063
  2. Fedoseev, 1970, Geostrophic circulation of surface waters on the shelf of north-west Africa, Rapports et Procès-Verbeaux des Réunions, Conseille International pour l’Exploration de la Mer, 159, 32
  3. Hill, 1998, Eastern ocean boundaries. Coastal segment (E), vol. 11, 29
  4. Kalu, A.E., 1979a. The African dust plume: its characteristics and propagation across West Africa in winter. In: Morales, C. (Hg.), Saharan Dust. Mobilization, Transport, Deposition. Papers and Recommendations from a Workshop held in Gothenburg, Sweden, 25–28 April 1977, Chichester, New York, Brisbane, Toronto, pp. 95–118.
  5. Kalu, 1979, The African dust plume: its characteristics and propagation across West Africa in winter, SCOPE, 14, 95

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Authors
Ohde, T., & Siegel, H.
Affiliations
Leibniz Institute for Baltic Sea Research Warnemünde (DE)
Corresponding author
Ohde, T.
Venue
Continental Shelf Research
Publisher
Elsevier BV
Published
2010-05
Volume
30
Issue
9
Pages
1108-1119
ISSN
0278-4343 (ISSN-L)
OpenAlex
W2007308890
Cited by
40
References
61
Citations by year
2026: 3 · 2025: 4 · 2024: 4 · 2023: 3 · 2022: 2 · 2021: 2 · 2020: 4 · 2019: 1 · 2017: 2 · 2016: 3 · 2015: 2 · 2014: 4 · 2013: 3 · 2012: 1
FWCI
1.39
Type
journal article
Language
en
Open access
closed
Locations
  • Continental Shelf Research (publishedVersion)
  • Helmholtz Centre for Ocean Research Kiel (GEOMAR) (acceptedVersion)
Funders
  • National Aeronautics and Space Administration
  • Bundesministerium für Bildung und Forschung
  • Leibniz-Gemeinschaft
Topics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
  • Physical Sciences › Environmental Science › Global and Planetary Change › Atmospheric aerosols and clouds
Keywords
coastal upwelling, Saharan dust deposition, chlorophyll-a variability, phytoplankton biomass, nutrient supply, alongshore wind stress, trade winds, aerosol optical depth, dust storms, time delay, ocean color remote sensing

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