Río Negro is one of the five provinces that make up Argentine Patagonia (together with the most southern partido of Buenos Aires Province -
Patagones Partido). It is bounded to the north by the
Colorado River which separates it from
La Pampa Province, to the east by the
Atlantic Ocean and to the west by the
Andes and the
Limay River (serves as the natural border with
Neuquén Province).
Climate The climate of the province is temperate at low elevations, and very cold in the higher Andean peaks.
Temperature The mean annual temperatures in the province are relatively cold for its latitude owing to the marine currents to the east and higher altitude to the west. Mean annual temperatures in the province can vary, depending on altitude and distance from the sea. The northern parts of the province are the warmest, with a mean annual temperature of more than while the coldest areas are found in the Cordillera where the mean annual temperatures are less than . At the highest peaks, the mean annual temperature is less than freezing. Summer temperatures can exceed although the mean January temperatures range from . In contrast, the Andean region has milder summers with mean January temperatures of or less, depending on the altitude. In July, mean temperatures range from on the coast in the north to around in the central plateau.{{cite web |archive-url=https://web.archive.org/web/20141102083013/http://www.mineria.gob.ar/estudios/irn/rionegro/r-2.asp |archive-date=November 2, 2014|url= http://www.mineria.gob.ar/estudios/irn/rionegro/r-2.asp#m1
Humidity and precipitation . map for the province of Río Negro Relative humidity is lower in the central plateau where they average 50%. Along the coastal regions, humidity is higher with a mean annual humidity of 60% while the Andean region has the highest humidity with an average annual humidity exceeding 65% due to the lower temperatures there. In all locations, humidity is lower in the summer and higher in the winter owing to the higher temperatures in the summer. The Andes block most of the moisture from the
Pacific Ocean from coming in, causing it to release most of the precipitation on its western slopes and as such, most of the province is dry, with a mean annual precipitation around . Coastal areas and northern parts of the province receive a slightly higher precipitation, where it can average above a year. The Andean region receives the most precipitation with areas receiving a mean annual precipitation of in which the precipitation gradient is very strong and increases westwards. In some places, precipitation can exceed a year. Most of the Andean region has a rainfall pattern that is
Mediterranean like, similar to Central Chile in which most of the precipitation falls during the winter months and summers are dry.
Wind and sunshine near
Bariloche. One dominant characteristic of the climate is the strong winds that are observed throughout the province. Summers tend to be windier than winters. Winds coming from the west, southwest and northwest are common, occurring 50% of the time (60% if calm winds are not included). There is some tendency for the winds to come from the east, particularly on the coastal regions when sea breezes from the east can occur when westerly winds are weak, which can be felt up to from the coast. The mean wind speed throughout the province varies with the northern parts having the lowest wind speeds while the highest altitude areas being the windiest. Except for the northern parts of the province, mean annual wind speeds exceed . Cloud cover varies throughout the province, ranging from more than 60% in the Andean region to about 40% in the coastal areas. The central plateaus have intermediate amounts of cloud cover between these 2 regions. As such, the Andean region is cloudier than the rest of the province. Sunshine ranges from 10–11 hours of sunshine/day in January to about 5 hours of sunshine/day (less cloudier areas) to less than 3 hours of sunshine/day (more cloudier areas) in July. ==Demographics==