On the causes of interannual variability of the wind field and ocean surface temperature in the area of the Canary upwelling

A.B. Polonsky1, T.V. Voznaya1, 2

1Institute of Natural and Technical Systems, RF, Sevastopol, Gogol St., 14

 E-mail: apolonsky5@mail.ru

2Sevastopol State University, Sevastopol, Universitetskaya St., 33

DOI: 10.33075/2220-5861-2025-3-14-23

UDC 551.465.6:588.16                             

EDN: https://elibrary.ru/cjqhqx

Abstract:

The purpose of this work is to check how significantly El Niño events affect the interannual variability of wind and ocean surface temperature fields in the Canary Upwelling region. Satellite data from several decades and the Pacific Nino3 index are used. It is shown that, on average, about 15% of the total variance of wind and ocean surface temperature fields in the Canary Upwelling region on an interannual scale is due to Pacific variability. The development of a warm anomaly in the equatorial zone of the Pacific Ocean is accompanied by an intensification of the Canary Upwelling. This intensification manifests itself in the strengthening of the wind-driven current off the northwestern coast of Africa and the lowering of the ocean surface temperature there, which are several months behind the changes in the ocean surface temperature in the Nino3 region. The maximum manifestations of ENSO in the Canary Upwelling region are observed during the mature phase of the event, when the Hadley cell intensifies as a result of the anomalous warming of the equatorial Pacific Ocean. During the most intense El Niño events, the dispersion of hydrometeorological characteristics in the Canary Upwelling region increases significantly due to Pacific variability.

Keywords: Canary Upwelling intensity and its interannual variability, El-Niño-Southern Oscillation events

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