section_path: Geography/Climate
section_name: Climate
paragraph_text: Climate
  
  In general, Argentina has four main climate types: warm humid subtropical, moderate humid subtropical, arid and cold. all determined by the expanse across latitude, range in altitude, and relief features. Although the most populated areas are generally temperate, Argentina has an exceptional amount of climate diversity, ranging from subtropical in the north to polar in the far south. Consequently, there is a wide variety of biomes in the country, including Subtropical rainforests, semi-arid and arid regions, temperate plains in the Pampas, and cold subantarctic in the south. The average annual precipitation ranges from 150 millimetres (6 in) in the driest parts of Patagonia to over 2,000 millimetres (79 in) in the westernmost parts of Patagonia and the northeastern parts of the country. Mean annual temperatures range from 5 °C (41 °F) in the far south to 25 °C (77 °F) in the north.
  
  Major wind currents include the cool Pampero Winds blowing on the flat plains of Patagonia and the Pampas; following the cold front, warm currents blow from the north in middle and late winter, creating mild conditions. The Sudestada usually moderates cold temperatures but brings very heavy rains, rough seas and coastal flooding. It is most common in late autumn and winter along the central coast and in the Río de la Plata estuary. The Zonda, a hot dry wind, affects Cuyo and the central Pampas. Squeezed of all moisture during the 6,000 m (19,685 ft) descent from the Andes, Zonda winds can blow for hours with gusts up to 120 km/h (75 mph), fueling wildfires and causing damage; between June and November, when the Zonda blows, snowstorms and blizzard (viento blanco) conditions usually affect higher elevations.
  
  Climate change in Argentina is predicted to have significant effects on the living conditions in Argentina. The climate of Argentina is changing with regards to precipitation patterns and temperatures. The highest increases in precipitation (from the period 1960–2010) have occurred in the eastern parts of the country. The increase in precipitation has led to more variability in precipitation from year to year in the northern parts of the country, with a higher risk of prolonged droughts, disfavoring agriculture in these regions.