Abstract
The issue of long-term tendencies in the sea surface temperature (SST) in the Benguela upwelling region and their causes is examined using the daily satellite data of the SST for 1985–2017 and the near-surface wind for 1988–2017. It is shown that in the Benguela upwelling region there has been a significant intensification of offshore winds in the last 20 years. This is accompanied by a decrease in the thermal upwelling index (taking into account the sign of the index or an increase in its absolute values) in the southern part of the Benguela upwelling, but it practically does not influence this indicator in its northern part. The probable cause for this difference is the change in the wind-field structure, which results in opposite trends in the magnitude of the wind stress curl in different parts of the Benguela upwelling. In the southern part of the Benguela upwelling, both the coastal upwelling and the vertical velocities due to the vorticity of the near-water wind intensify, while in its northern part the corresponding trends have opposite signs. This leads to a partial compensation of these two effects in the northern part of the Benguela upwelling. The cause for the change in the wind-field structure is the displacement of the center of the Subtropical High to the southeast and the concomitant reversal of the near-surface wind vectors in the coastal zone.
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REFERENCES
Backeberg, B.C., Penven, P., and Rouault, M., Impact of intensified Indian Ocean winds on mesoscale variability in the Agulhas system, Nat. Clim. Change, 2012, vol. 2, no. 8, pp. 608–612. https://doi.org/10.1038/nclimate1587
Bakun, A., Global climate change and intensification of coastal ocean upwelling, Science, 1990, vol. 247, pp. 198–201. https://doi.org/10.1126/science.247.4939.198
Bakun, A., Field, D.B., Redondo-Rodriguez, A., and Weeks, S.J., Greenhouse gas, upwelling-favorable winds, and the future of coastal ocean upwelling ecosystems, Global Change Biol., 2010, vol. 16, no. 4, pp. 1213–1228. https://doi.org/10.1111/j.1365-2486.2009.02094.x
Belmadani, A., Echevin, V., Codron, F., Takahashi, K., and Junquas, C., What dynamics drive future wind scenarios for coastal upwelling off Peru and Chile?, Clim. Dyn., 2014, vol. 43, no. 7–8, pp. 1893–1914.
Carr, M.E., Estimation of potential productivity in Eastern Boundary Currents using remote sensing, Deep-Sea Res. II, 2002, vol. 49, no. 1–3, pp. 59–80.
Carr, M.E. and Kearns, E.J., Production regimes in four Eastern Boundary Current systems, Deep-Sea Res. II, 2002, vol. 50, no. 22–26, pp. 3199–3221.
Chavez, F.P. and Messie, M., A comparison of eastern boundary upwelling ecosystems, Prog. Oceanogr., 2009, vol. 83, no. 1–4, pp. 80–96. https://doi.org/10.1016/j.pocean.2009.07.032
Climate Change 2014: Synthesis Report. Contribution of Working Groups I, II and III to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Pachauri, R.K. and Meyer, L.A., Eds., Geneva: IPCC.
Demarq, H., Trends in primary production, sea surface temperature and wind in upwelling systems (1998–2007), Prog. Oceanogr., 2009, vol. 83, pp. 376–385.
Desbiollesa, F., Bentamya, A., Blanke, B., Roy, C., Mestas-Nunez, A.M., Grodsky, S.A., Herbette, S., Cambon, G., and Maes, C., Two decades (1992–2012) of surface wind analyses based on satellites scatterometer observations, J. Mar. Syst., 2017, no. 168, pp. 38–56.
Dufois, F. and Rouault, M., Sea surface temperature in False Bay (South Africa): towards a better understanding of its seasonal and inter-annual variability, Cont. Shelf Res., 2012, vol. 43, pp. 24–35.
Hartmann, D.L., Klein Tank, A.M.G., Rusticucci, M., Alexander, L.V., Bronnimann, S., Charabi, Y.A.R., and Zhai, P., Observations: atmosphere and surface in Climate Change 2013. The Physical Science Basis: Working Group I Contribution to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change, Cambridge: Cambridge University Press, 2013, vol. 9781107057999, pp. 159–254. https://doi.org/10.1017/CBO9781107415324.008.
Junker, T., Schmidt, M., and Mohrholz, V., The relation of wind stress curl and meridional transport in the Benguela upwelling system, J. Mar. Syst., 2015, vol. 143, pp. 1–6.
Lamont, T., Garcia-Reyes, M., Bograd, S.J., van der Lingen, C.D., and Sydeman, W.J., Upwelling indices for comparative ecosystem studies: variability in the Benguela upwelling system, J. Mar. Syst., 2018, vol. 188, pp. 3–16.
Narayan, N., Paul, A., Mulitza, S., and Schulz, M., Trends in coastal upwelling intensity during the late 20th century, Ocean Sci., 2010, vol. 6, pp. 815–823. https://doi.org/10.5194/os-6-815-2010
Polonskii, A.B. and Serebrennikov, A.N., Interannual and intramonth fluctuations of the wind field and ocean surface temperature in the West African upwelling zone using satellite data, Issled. Zemli Kosmosa, 2017, no. 5, pp. 14–19.
Polonskii, A.B. and Serebrennikov, A.N., Long-term trends in the temperature of the ocean surface in the Canary Upwelling zone and their causes, Issled. Zemli Kosmosa, 2018, no. 3, pp. 1–8.
Polonskii, A.B. and Serebrennikov, A.N., On the change in the temperature of the ocean surface in the Benguela upwelling zone. Part 1: seasonal cycle, Issled. Zemli Kosmosa, 2019, no. 3, pp. 33–44.
Serebrennikov, A.N., Improved method for determining coastal upwelling indices using satellite data, Sovr. Probl. Dist. Zond. Zemli Kosm., 2018, vol. 15, no. 5, pp. 44–51.
Strub, P.T., Mesias, J.M., Montecino, V., Rutllant, J., and Salinas, S., Coastal ocean circulation off western South America, The Sea, Robinson, A.R., and Brink, K.H., Eds., New York: John Wiley and Sons, 1988, vol. 11.
Tim, N., Zorita, E., and Hunicke, B., Decadal variability and trends of the Benguela upwelling system as simulated in a high ocean-only simulation, Ocean Sci., 2015, vol. 11, pp. 483–502
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Translated by L. Mukhortova
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Polonsky, A.B., Serebrennikov, A.N. On the Change in the Sea Surface Temperature in the Benguela Upwelling Region: Part II. Long-Term Tendencies. Izv. Atmos. Ocean. Phys. 56, 970–978 (2020). https://doi.org/10.1134/S0001433820090200
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DOI: https://doi.org/10.1134/S0001433820090200