Changes in the partial pressure of carbon dioxide in the Mauritanian-Cap Vert upwelling region between 2005 and 2012

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Abstract

Coastal upwellings along the eastern margins of major ocean basins represent regions of large ecological and economic importance due to the high biological productivity. The role of these regions for the global carbon cycle makes them essential in addressing climate change. The physical forcing of upwelling processes that favor production in these areas are already being affected by global warming, which will modify the intensity of upwelling and, consequently, the carbon dioxide cycle. Here, we present monthly high-resolution surface experimental data for temperature and partial pressure of carbon dioxide in one of the four most important upwelling regions of the planet, the Mauritanian-Cap Vert upwelling region, from 2005 to 2012. This data set provides direct evidence of seasonal and interannual changes in the physical and biochemical processes. Specifically, we show an upwelling intensification and an increase of 0.6 Tg yr-1 in CO2 outgassing due to increased wind speed, despite increased primary productivity. This increase in CO2 outgassing together with the observed decrease in sea surface temperature at the location of the Mauritanian Cap Blanc, 21° N, produced a pH rate decrease of -0.003-0.001 yr-1.

Figures

  • Figure 1. Ship track (black line) in the area from 28◦ N (Gran Canaria, the Canary Islands) to 10◦ N. The locations of Cap Blanc and Cap Vert are indicated. Monthly OceanColor Web (https:// oceancolor.gsfc.nasa.gov/) data for average chlorophyll a concentration (mg m−3) were included in a MATLAB routine and annually averaged. The map has been generated using MATLAB 7.12 R2011a.
  • Figure 2. Time series of upwelling index (UI, × 10−3 m2 s−1) in the Mauritanian–Cap Vert upwelling region along the ship track computed following Nykjaer and Van Camp (1994). Blue colors are related to upwelling events and red colors to downwelling events.
  • Figure 3. In situ data of column (a) SST and column (b) SSS in the Mauritanian–Cap Vert coastal region grouped by seasons: winter (W; December, January, and February), spring (Sp; March, April, and May), summer (Sm; June, July, and August), and autumn (Au; September, October, and November). The averaged values for all cruises in Table S1 are shown in black for each season including the 95 % confidence limits. The color code for each cruise is indicated in Table S1.
  • Figure 4. Latitudinal distribution of the interannual trends for the upwelling index (UI) and for the four experimental variables along the QUIMA-VOS line integrated over every degree between 2005 and 2012. Panel (a) presents the trends for upwelling index (UI, × 10−3 m2 s−1, mean confidence interval of 9 m2 s−1), SST (◦C yr−1, confidence interval 0.13 ◦C), and SSS (yr−1, confidence interval 0.06) and (b) the trends for fCOsw2 and fCO atm 2 (confidence intervals 4.23 and 0.44 µatm).
  • Figure 5. Fugacity of CO2 data in the Mauritanian–Cap Vert coastal region grouped by seasons: winter (W; December, January, and February), spring (Sp; March, April, and May), summer (Sm; June, July, and August), and autumn (Au; September, October, and November). Column (a) fCOsw2 latitudinal distribution. Column (b), difference between measured and fCO sw 2 values normalized to a constant temperature of 22 ◦C. The averaged values for all cruises in Table S1 are shown in black for each season including the 95 % confidence limits. The color code for each cruise is indicated in Table S1.
  • Figure 6. pH of surface waters in total proton scale and at in situ SST computed from total alkalinity (based on regional correlations with SST and SSS; Lee et al., 2006) and fCO2 at 21± 0.25◦ N. The error bars represent the standard deviation of the computed data for each cruise for the selected latitude. The black curve shows the harmonic fitting of Eq. (4) for the data and the corresponding linear trend is also shown.
  • Figure 7. Latitudinal distributions of seasonal and annual CO2 fluxes (FCO2, mol m−2). Fluxes of CO2 were computed using Nightingale et al. (2000) parameterization and satellite winds with a resolution of 6 h. (a) Integrated year to year from 2005 to 2012 and (b) latitudinally integrated for 2005 to 2012 together with annual values for the North Atlantic Oscillation (NAO) index. Latitudinal distributions of FCO2 seasonally integrated from 2005 to 2012 are depicted for (c) winter (December, January, and February), (d) spring (March, April, and May), and (e) summer (June, July, and August).

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CITATION STYLE

APA

González-Dávila, M., Casiano, J. M. S., & Machín, F. (2017). Changes in the partial pressure of carbon dioxide in the Mauritanian-Cap Vert upwelling region between 2005 and 2012. Biogeosciences, 14(17), 3859–3871. https://doi.org/10.5194/bg-14-3859-2017

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