Climate
What is the name of the wind affecting west-central Argentina?
Argentina
Climate of Argentina Central Bank of Argentina Seferina Ñeembucú Department Wind speed
Climate_of_Argentina-Winter Central_Bank_of_Argentina-Abstract Seferina-Abstract Ñeembucú_Department-Borders Wind_speed-Factors_affecting_wind_speed
In winter (June to August) major winds include the cool Pampero blowing on the flat plains of Patagonia and the "Pampas" after a cold front; a warm wind that can blow from the north in mid and late winter creating mild conditions; and the Zonda, a hot and dry wind (see also foehn wind), affecting west-central Argentina. Argentina also gets some snow in many southern and central places of the country. 
The Central Bank of Argentina (, BCRA) is the central bank of Argentina.  
Seferina, or Zeferina, is a given name of Spanish origin, and from the Greek "Zephyra", meaning "west wind".  
To the west, Ñeembucú is limited by the Rio Paraguay and Argentina, to the south by the Rio Paraná and Argentina, to the north by the Central department, and to the east by the departments of Paraguarí and Misiones. 
Wind speed is affected by a number of factors and situations, operating on varying scales (from micro to macro scales). These include the pressure gradient, Rossby waves and jet streams, and local weather conditions. There are also links to be found between wind speed and wind direction, notably with the pressure gradient and surfaces over which the air is found. Pressure gradient is a term to describe the difference in air pressure between two points in the atmosphere or on the surface of the Earth. It is vital to wind speed, because the greater the difference in pressure, the faster the wind flows (from the high to low pressure) to balance out the variation. The pressure gradient, when combined with the Coriolis Effect and friction, also influences wind direction. Rossby waves are strong winds in the upper troposphere. These operate on a global scale and move from West to East (hence being known as Westerlies). The Rossby waves are themselves a different wind speed from what we experience in the lower troposphere. Local weather conditions play a key role in influencing wind speed, as the formation of hurricanes, monsoons and cyclones as freak weather conditions can drastically affect the velocity of the wind. 