Why Southern Europe Is Warmer Than Northern Europe
The primary driver is latitude: Southern Europe lies closer to the equator, receiving more direct solar radiation. Additional factors amplify this warmth:
- Mediterranean Sea: Acts as a heat reservoir, absorbing daytime heat and releasing it slowly, moderating coastal climates.
- Atmospheric circulation: Prevailing winds from the south/southwest bring warm air from the Sahara Desert.
- Topography: The Alps and other northern mountain ranges block cold Arctic air, allowing warm air to pool in the south.
- Ocean currents: The Gulf Stream carries warm water to the coasts of Spain and Portugal.
- Urban heat islands: Large southern cities (Rome, Madrid, Athens) retain heat from buildings and pavement.
Together, these factors create the characteristic Mediterranean climate of hot, dry summers and mild, wet winters.