Cited by 260Oceanographic and Atmospheric ProcessesClimate variability and modelsMarine and coastal ecosystems

Spatial and temporal seasonal trends in coastal upwelling off Northwest Africa, 1981–2012

Open access
Cropper, Thomas E., Hanna, Edward, Bigg, Grant R.·2014·Deep Sea Research Part I: Oceanographic Research Papers

Abstract

Seasonal coastal upwelling was analyzed along the NW African coastline (11–35°N) from 1981 to 2012. Upwelling magnitudes are calculated by wind speed indices, sea-surface temperature indices and inferred from meteorological station, sea-surface height and vertical water column transport data. A permanent annual upwelling regime is documented across 21–35°N and a seasonal regime across 12–19°N, in accordance with the climatology of previous studies. Upwelling regions were split into three zones: (1) the Mauritania–Senegalese upwelling zone (12–19°N), (2) the strong permanent annual upwelling zone (21–26°N) and (3) the weak permanent upwelling zone (26–35°N). We find compelling evidence in our various indices for the Bakun upwelling intensification hypothesis due to a significant coastal summer wind speed increase, resulting in an increase in upwelling-favorable wind speeds north of 20°N and an increase in downwelling-favorable winds south of 20°N. The North Atlantic Oscillation plays a leading role in modifying interannual variability during the other seasons (autumn–spring), with its influence dominating in winter. The East Atlantic pattern shows a strong correlation with upwelling during spring, while El Niño Southern Oscillation and Atlantic Multi-decadal Oscillation teleconnections were not found. A disagreement between observationally-based wind speed products and reanalysis-derived data is explored. A modification to the Bakun upwelling intensification hypothesis for NW Africa is presented, which accounts for the latitudinal divide in summer wind regimes.

The claims and statistics of this paper haven’t been checked yet.

Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.

A few free checks a day · papers already verified open instantly · results are public

Integrity signals

Registry

Crossref · 10.1016/j.dsr.2014.01.007

Cites

4 of 4 references verified0 citation errors · 0 not checkable

Statistics

Claims the paper makes

The claims and statistics of this paper haven’t been checked yet.

Run the check — free, no account needed. It reads the open-access text and checks the sources it cites.

A few free checks a day · papers already verified open instantly · results are public

Claims other papers make about this one

Each is checked against this paper’s own text: does it say what the citing paper says it does?

  • Cropper et al. (2014) found further evidence of increases in upwelling favorable winds during summer months from 1981 to 2012.

    “They found further evidence of increases in upwelling favorable winds (from oceanic stations; two out of four significant) during summer months from 1981 to 2012.”

    From Recent Trends in SST, Chl‐<i>a</i>, Productivity and Wind Stress in Upwelling and Open Ocean Areas in the Upper Eastern North Atlantic Subtropical Gyre (2021) · cites this paper as Cropper et al. (2014)

    The Discussion reports increased summer upwelling-favorable winds north of 21°N during 1981–2012, supporting the main claim. But the cited paper’s Results (§3.3.1) describe six coastal meteorological stations, with positive trends at four and a significant trend at only one; they do not support the citing sentence’s description of oceanic stations with two of four significant. (LLM, conf=0.84)

    Experimental — accuracy not yet measured
  • Cropper et al. (2014) and Taboada and Anadón (2012) reported general SST increases in the North Atlantic, with open ocean warming rates in the range of +0.1 to +0.3 °C dec-1.

    “Cropper et al. (2014) and Taboada and Anadón (2012) reported general SST increases in the North Atlantic, where warming rates in the open ocean lie in the range of +0.1-0.3°Cdec -1 .”

    From Recent Trends in SST, Chl‐<i>a</i>, Productivity and Wind Stress in Upwelling and Open Ocean Areas in the Upper Eastern North Atlantic Subtropical Gyre (2021) · cites this paper as Cropper et al. (2014)

    The ΔSST section reports statistically significant open-ocean warming around parts of the northwest African coast. It does not establish general SST increases across the North Atlantic or give the claimed open-ocean warming range of +0.1 to +0.3 °C per decade. (LLM, conf=0.86)

    Experimental — accuracy not yet measured
  • The Bakun Hypothesis was originally supported by emerging interregional patterns of observed sea-surface wind stress and has been periodically tested against time series of observed data in all four regional eastern boundary upwelling systems.

    “This idea was originally supported by emerging interregional patterns of observed sea-surface wind stress, and has been periodically tested against time series of observed data in all four regional EBUS [12,13].”

    From Anticipated Effects of Climate Change on Coastal Upwelling Ecosystems (2015) · cites this paper as [13]

    Split into 2 atoms — 1 confirmed, 1 partially supported, 0 disputed, 0 misattributed, 0 unverifiable. Expand the claim to see per-atom verdicts.

    Experimental — accuracy not yet measured
  • Cropper et al. computed the Trade Wind Index, which suggests an intensification of winds since 1973.

    “Moreover, they computed the Trade Wind Index (difference of sea level pressure from Azores and Cape Verde) which also suggests an intensification of winds since 1973.”

Self-check

Percentages, sums and reported differences re-computed from the paper’s own numbers.

The self-check needs the paper’s full text.

Cites

Flagged first, then by citations

Research works printed but not linked: 8

  1. Behringer, D.W., 2007. The global ocean data assimilation system at NCEP. In: Proceedings of the 11th Symposium on Integrated Observing and Assimilation Systems for Atmosphere, Oceans, and Land Surface, Am. Meteorol. Soc., San Antonio, Tex.
  2. Behringer, D.W., Xue, Y., 2004. Evaluation of the global ocean data assimilation system at NCEP: The Pacific Ocean. In: Proceedings of the Eighth Symposium on Integrated Observing and Assimilation Systems for Atmosphere, Oceans, and Land Surface, AMS 84th Annual Meeting, Washington State Convention and Trade Center, Seattle, Washington, pp. 11-15.
  3. Cropper T.E. and Hanna E., An analysis of the climate of Macaronesia, 1865-2012, Int. J. Climatol. Early View, http://dx.doi.org/10.1002/joc.3710, in press. · DOI
  4. Diffenbaugh, N.S., Snyder, M.A, Sloan, L.C., 2004. Could CO(2)-induced land-cover feedbacks alter near-shore upwelling regimes? Proc. Natl. Acad. Sci. USA 101, 27-32.
  5. Herbert, T.D., 2001. Review of alkenone calibrations (culture, water column, and sediments). Geochem. Geophys. Geosys 2 (2000GC000055).
  6. Nicholson, S.E., 2013. The West African Sahel: a review of recent studies on the rainfall regime and its interannual variability. ISRN Meteorol 2013, 453521.
  7. Uppala, S.M., Kållberg, P.W., Simmons, A.J., Andrae, U., Bechtold, V.D.C., Fiorino, M., Gibson, J.K., Haseler, J., Hernandez, A., Kelly, G.A., Li, X., Onogi, K., Saarinen, S., Sokka, N., Allan, R.P., Andersson, E., Arpe, K., Balmaseda, M.A., Beljaars, A.C.M., Berg, L.V-D., Bidlot, J., Bormann, N., Caires, S., Chevallier, F., Dethof, A., Dragosavac, M., Fisher, M., Fuentes, M., Hagemann, S., Hólm, E., Hoskins, B.J., Isaksen, L., Janssen, P.A.E.M., Jenne, R., Mcnally, A.P., Mahfouf, J.-F., Morcrette, J.- J., Rayner, N.A., Saunders, R.W., Simon, P., Sterl, A., Trenberth, K.E., Untch, A., Vasiljevic, D., Viterbo, P., Woollen, J., 2005. The ERA-40 re-analysis. Q. J. R. Meteorol. Soc., 131; , pp. 2961-3012.
  8. Wang, C., 2011. Atlantic multidecadal oscillation, in "State of the Climate in 2011". Bull. Am. Meteorol. Soc. 93 (7), S137-S138.

Cited by

Sorted by citations

Authors
Cropper, T. E., Hanna, E., & Bigg, G. R.
Affiliations
University of Sheffield (GB)
Corresponding author
Cropper, Thomas E.
Venue
Deep Sea Research Part I: Oceanographic Research Papers
Publisher
Elsevier BV
Published
2014-04
Volume
86
Pages
94-111
ISSN
0967-0637 (ISSN-L)
OpenAlex
W1964542801
Cited by
260
References
4
Citations by year
2026: 20 · 2025: 21 · 2024: 26 · 2023: 24 · 2022: 38 · 2021: 21 · 2020: 23 · 2019: 20 · 2018: 22 · 2017: 16 · 2016: 15 · 2015: 10 · 2014: 4
FWCI
10.82
Type
journal article
Language
en
Open access
Locations
  • Deep Sea Research Part I Oceanographic Research Papers (publishedVersion, cc-by)
  • Lincoln Repository (University of Lincoln) (acceptedVersion)
  • White Rose Research Online (University of Leeds, The University of Sheffield, University of York) (acceptedVersion)
  • ORCA Online Research @Cardiff (Cardiff University) (acceptedVersion)
  • NERC Open Research Archive (Natural Environment Research Council) (acceptedVersion)
  • Figshare (submittedVersion, cc-by)
Funders
  • NERC Doctoral Training (NE/I528618/1)
  • Department of Geography, University of Sheffield
Topics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
Keywords
coastal upwelling, North Atlantic Oscillation, East Atlantic pattern, interannual variability, sea surface temperature, Northwest African coast, ENSO, Atlantic Multidecadal Oscillation

About these checks

Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.

Statistics and arithmetic are recomputed, not judged.

Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.

What counts as a claim ›How we measure confidence ›How we check this ›

Are you an author, or do you see a problem with this page? Request a review