Stable subtropical anticyclones (e.g., the South Pacific High, South Atlantic High, and Indian Ocean High) shift poleward during summer. Their influence brings hot, dry conditions to western coastal deserts (e.g., the Atacama, Namib) while directing moisture-laden trade winds toward eastern continental margins, producing summer-rainfall regimes in regions like southeastern Brazil, Mozambique, and eastern Australia.

[Generated AI] Date: April 14, 2026

Australian summer is notorious for extreme heat, bushfires (wildfires), and tropical cyclones in the north. The monsoon arrives over northern Australia (the “Wet”), while the south experiences dry, hot conditions influenced by blocking highs. Heatwaves, such as the infamous “Angry Summer” of 2012–2013, set temperature records (e.g., 49.6°C at Birdsville). The El Niño–Southern Oscillation (ENSO) strongly modulates summer rainfall: El Niño brings drought and fire risk; La Niña brings flooding.