Table 1 Key large scale forcing factors of the regional climate system and their impact on oceanic and atmospheric patterns.

From: Exploring steric sea level variability in the Eastern Tropical Atlantic Ocean: a three-decade study (1993–2022)

Climate index

Abbrev

Parameter

Location of high

Location of low

References

Effect

Atlantic multidecadal oscillation

AMO

North atlantic SST anomaly

Warmer waters in the North Atlantic

Cooler waters in the north atlantic

Enfield et al.28

Influences Atlantic SSTs and climate variability over multidecadal timescales

Indian ocean dipole mode index

DMI

Western—eastern tropical Indian ocean SST gradient

Positive phase: Warmer waters in the west, cooler waters in the east

Negative phase: Reversed temperature gradient

Saji et al.29; Liu et al.30

Affects monsoon patterns, rainfall in the Indian Ocean region (East Africa, Australia, and Southeast Asia.)

Niño3 index

Niño3 (150°W–90°W, 5°S–5°N)

Eastern tropical pacific SST anomaly

Eastern pacific

Eastern pacific

Trenberth and Stepaniak31

Key indicator of El Niño-Southern Oscillation (ENSO) events, affecting global atmospheric circulation and regional climates

Tropical atlantic SST index

TASI

Gradient of meridional SST anomalies in the tropical Atlantic

Tropical atlantic

Tropical atlantic

Chang et al.32

Influences Atlantic hurricane activity and West African monsoon. It is associated with a potential decadal 'dipole' mode of coupled variability in the tropical Atlantic

Tropical northern atlantic index

TNA (55°W–15°W, 5°N–25°N)

SST anomalies in the northern tropical atlantic ocean

Northern tropical atlantic

Northern tropical atlantic

Enfield et al.28

Affects Atlantic hurricane activity and rainfall over the Americas

Tropical southern atlantic index

TSA (30°W–10°E, 20°S–Eq)

SST anomalies in the southern tropical atlantic ocean

Southern tropical atlantic

Southern tropical atlantic

Enfield et al.28

Indicator of the surface temperatures in the GoG, the eastern tropical South Atlantic Ocean. Influences rainfall patterns in South America and Africa

Atlantic niño

ATL3 or EAUS (3°N–3°S, 0–20°W)

Eastern tropical atlantic SST anomaly

Eastern tropical atlantic

Eastern tropical atlantic

Chen et al.20; Liu et al.30

Influences West African summer monsoon, leading to reduced rainfall in the Sahel region and increased flooding in northeastern South America and the West African sub-Sahel countries bordering the GoG