Abstract

This study investigates circulation types (CTs) in Africa, south of the equator, that are related to wet and dry conditions in the Western Cape, the statistical relationship between the selected CTs and the Southern Annular Mode (SAM), and changes in the frequency of occurrence of the CTs related to the SAM under the ssp585 scenario. Obliquely rotated principal component analysis applied to sea level pressure (SLP) was used to classify CTs in Africa, south of the equator. Three CTs were found to have a high probability of being associated with wet days in the Western Cape, and four CTs were equally found to have a high probability of being associated with dry days in the Western Cape. Generally, the dry/wet CTs feature the southward/northward track of the mid-latitude cyclone, adjacent to South Africa; anti-cyclonic/cyclonic relative vorticity, and poleward/equatorward track of westerlies, south of South Africa. One of the selected wet CTs was significantly related to variations of the SAM. Years with an above-average SAM index correlated with the below-average frequency of occurrences of the wet CT. The results suggest that through the dynamics of the CT, the SAM might control the rainfall variability of the Western Cape. Under the ssp585 scenario, the analyzed climate models indicated a possible decrease in the frequency of occurrence of the aforementioned wet CT associated with cyclonic activity in the mid-latitudes, and an increase in the frequency of the occurrence of CT associated with enhanced SLP at mid-latitudes.

Highlights

  • The Southern Annular Mode (SAM) is a low-frequency mode of atmospheric variability of the southern hemisphere

  • The Climate Prediction Centre (CPC) dataset captured the annual cycle of rainfall in the Western Cape, it underestimated rainfall from austral autumn to early austral spring (September) relative to the analyzed station data

  • The relationship between CT5− and El Niño Southern Oscillation (ENSO) suggests that during El Niño events, the atmospheric Rossby waves generated by sea surface temperature (SST) anomalies in the central or eastern Pacific that modulate southeasterly moisture fluxes advected by the western branch of the Mascarene high might cause below-average austral summer rainfall in some eastern parts of the Western Cape [32,42,44]

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Summary

Introduction

The Southern Annular Mode (SAM) is a low-frequency mode of atmospheric variability of the southern hemisphere. The SAM is characterized by a zonally symmetric north–south movement of the westerly belt that encircles Antarctica [1]. Its positive phase features a southward shift of the westerly belt, enhanced mean sea level pressure (SLP) in the mid-latitudes, and lower SLP in the high latitudes; the opposite occurs during its negative phase. According to [2], the existence of the SAM is mostly due to internal atmospheric dynamics. North–south migration of storm tracks in the southern hemisphere, which is related to sea surface temperature (SST) variability [3] and mid-latitude precipitation variability [4], is associated with variations of the SAM [5]. According to [6], variations of the SAM can influence ocean circulation

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