Cited by 134Oceanographic and Atmospheric ProcessesClimate variability and modelsMarine Plankton and Biogeochemistry

The DOI matches its Crossref record; 62 of the 64 references it cites were found in a registry or an index; 2 of the 11 sources its claims cite were checked for support.

Canary current upwelling: More or less?

Open access
Barton, E.D., Field, D.B., Roy, C.·2013·Progress in Oceanography

Abstract

It has been hypothesized that coastal upwelling in the four major eastern boundary current systems might be intensified as global warming could result in a greater land-sea temperature gradient and hence strengthen alongshore winds. Recent research has suggested a substantial increase of upwelling intensity off Northwest Africa. Evidence there is based on the derivation of a proxy for upper ocean temperatures from the alkenone unsaturation index (U37K') derived from two sediment cores recovered off Cape Ghir, Morocco. An accelerating decrease of over 1. °C during the last century was concluded for near surface temperature near the Cape. Support for this conclusion was found in an increase in Bakun's upwelling index for the same area. The evidence for a general intensification of upwelling within the whole Canary current upwelling system is examined here. Using available estimates of wind from PFEL, NCAR/NCEP, ECMWF, ICOADS and WASWind plus measured wind data from coastal meteorological stations, no evidence of a coherent intensification in winds at the regional scale off Northwest Africa is found. Moreover, sea surface temperature records from ships-of-opportunity (ICOADS data set) and also from the Pathfinder satellite AVHRR data set show a significant and correlated increase at all latitudes in the region, including in the area around Cape Ghir. It is concluded that there is no evidence for a general increase in upwelling intensity off Northwest Africa or Iberia. The apparent lowering of SST off Cape Ghir indicated by the alkenone unsaturation index can be explained by coccolithophorids (phytoplankton from which the U37K' signal is derived) living deeper in the water column. The distribution of most phytoplankton (including coccolithophorids) will deepen and have less overlap with mixed layer temperatures as the ocean warms, resulting in a near surface temperature estimate that is increasingly biased by subsurface temperatures and lower than the actual SST. © 2013 Elsevier Ltd.

Overview

AI snapshot

Written from the paper’s full text.

TL;DR

The paper tests the hypothesis that coastal upwelling in the Canary Current system has intensified, and finds no evidence of a coherent regional increase in upwelling-favourable winds off Northwest Africa or Iberia. It argues that the apparent alkenone-derived SST cooling off Cape Ghir is an artefact of coccolithophorids living deeper in the water column as the ocean warms.

Key findings

  • Using wind estimates from PFEL, NCAR/NCEP, ECMWF, ICOADS and WASWind plus measured wind data from coastal meteorological stations, "no evidence of a coherent intensification in winds at the regional scale off Northwest Africa is found."
  • Sea surface temperature records from ships-of-opportunity (ICOADS) and the Pathfinder satellite AVHRR data set "show a significant and correlated increase at all latitudes in the region, including in the area around Cape Ghir."
  • The authors conclude "there is no evidence for a general increase in upwelling intensity off Northwest Africa or Iberia," in direct contrast to earlier studies (e.g. McGregor et al. 2007, who reported a 1.2 °C SST reduction off Cape Ghir over the last century, and Narayan et al. 2010).
  • The apparent lowering of SST off Cape Ghir from the alkenone unsaturation index (U^K′_37) is explained by coccolithophorids living deeper in the water column; as the ocean warms, their distribution deepens and overlaps less with mixed-layer temperatures, biasing the near-surface temperature estimate low relative to actual SST.

Methods

  • Design: re-examination of the evidence for general intensification of upwelling across the whole Canary Current upwelling system, using publicly available wind and SST data sets for the North Atlantic upwelling region between Dakar, Senegal (15°N) and Galicia, Spain (43°N).
  • Data: wind from PFEL, NCAR/NCEP, ECMWF, ICOADS and WASWind, plus measured wind from coastal meteorological stations; SST from ICOADS ships-of-opportunity and Pathfinder AVHRR satellite data; sediment-core alkenone (U^K′_37) proxy records from two cores off Cape Ghir, Morocco (from McGregor et al.).
  • Analysis: documentation of temporal trends in atmospheric forcing and oceanic response, consideration of factors affecting reliability of the different wind and SST time series, and exploration of the SST–alkenone proxy temperature relationship.

Limitations

  • The paper states that "the evidence that wind velocity is increasing and SST decreasing in the NW African upwelling region as a whole has many uncertainties," and notes that different analyses give conflicting results (e.g. Pardo et al. found weakening, Narayan et al. found increasing upwelling intensity).
  • Evident from the supplied text: only the abstract, introduction and the start of the Data section (pages 1–3 of 42) are available, so the paper's detailed results, statistical tests and its own stated limitations section are not present in the provided fragment.

Model-written summary. Check it against the paper before relying on it.

Integrity signals

Registry

Crossref · 10.1016/j.pocean.2013.07.007

Cites

62 of 62 references verified0 citation errors · 0 not checkable

Statistics

Nothing to recompute.

Verification

Claims the paper makes

4 No full text of the sources · 3 Own interpretation · 2 Own result · 1 Supported · 1 Supported so far · 1 Not checked yet

  • Probably not a substantial claim. 4
  • It may state two separate claims as one. 2
6 of 6
  • The paper relies on this without support.

    The UK’37 alkenone unsaturation index signal is derived from coccolithophorids.

    “coccolithophorids (phytoplankton from which the View the MathML sourceU37K′ signal is derived)”
1 of 1

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?

Citations

Cites

Show all 64 references

Research works printed but not linked: 3

  1. Isemer, H.-J., 1995. Trends in marine surface winds speed: ocean weather stations versus voluntary observing ships. In: Proceedings of the International COADS Workshop, Kiel, Germany, NOAA Environmental Research Laboratories and Institut fur Meereskunde, pp. 68–84.
  2. Prahl, 2007, Biogeochemical assessment of alkenone export depth in the summertime euphotic zone of the Gulf of California, Extended Abstracts Presented at the ACS National Meeting, 47, 483
  3. Smith, 1968, Upwelling, Oceanography and Marine Biology, Annual Review, 6, 11

Cited by

Sorted by citations

See all 134

Metadata

Authors
Barton, E. D., Field, D. B., & Roy, C.
Affiliations
  • Instituto de Investigacións Mariñas (ES)
  • Hawaii Pacific University (US)
  • Centre National de la Recherche Scientifique (FR)
Corresponding author
Barton, E.D.
Venue
Progress in Oceanography
Publisher
Elsevier BV
Published
2013-09
Volume
116
Pages
167-178
ISSN
0079-6611 (ISSN-L)
OpenAlex
W2004932320
Cited by
134
References
64
Citations by year
2026: 7 · 2025: 5 · 2024: 13 · 2023: 10 · 2022: 19 · 2021: 11 · 2020: 14 · 2019: 10 · 2018: 11 · 2017: 8 · 2016: 8 · 2015: 11 · 2014: 4 · 2013: 3
FWCI
6.10
Type
journal article
Language
en
Open access
Locations
  • Progress In Oceanography (publishedVersion)
  • HAL (Le Centre pour la Communication Scientifique Directe) (submittedVersion)
  • DIGITAL.CSIC (Spanish National Research Council (CSIC)) (submittedVersion, other-oa)
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 Plankton and Biogeochemistry
Keywords
global warming, alkenone unsaturation index, sea surface temperature, coccolithophores, mixed layer temperature, alongshore winds, Maghreb, Iberia, eastern boundary currents

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.

A language model drew the claims from the paper on 2026-10-16, under version 3 of the claim definition (model deepseek-v4.1-flash, prompt extract-v3).

A second model labelled each claim on 2026-10-16 (model jev-1.13-20260917, definition revision gold-guideline-v0.2).

Cited sources are checked with a language model’s help (gpt-6-sol).

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