Warming weakens Asian monsoon's reach into the Mediterranean

The South Asian summer monsoon has long been known to shape the Mediterranean climate thousands of kilometers away as part of a phenomenon known as the "monsoon–desert" mechanism. Through this mechanism, intense monsoon convection during the summer releases large amounts of heat into the atmosphere, triggering large-scale circulation changes that promote sinking air over the Mediterranean. This process suppresses clouds and rainfall and contributes to the Mediterranean region's hot, dry climate.