Climatic map of the Province of La Pampa, Argentina
Climatic map of the Province of La Pampa, Argentina.
Being located in the Pampas, the province has a cool temperate climate. In general, the province is dominated by two different types of climates: a temperate one in the east and a semi-arid one in the west. Precipitation generally decreases from east to west and from north to south. Being characterized by large thermal amplitudes, the climate of the province has continental characteristics, particularly in the west where thermal amplitudes are much larger. The general atmospheric circulation is one of the most important factors that influence the climate on a regional scale. During summer, the South Atlantic High is displaced to the southeast, which brings hot and humid air masses from the north and northeast. The South Pacific High in summer is responsible for bringing cooler air masses from the southwest which when these two contrasting air masses meet lead to precipitation occurring. In contrast, winters are dry due the northward displacement of the South Atlantic high and the topographic barrier of the Andes north of 40oS which prevents frontal systems that bring precipitation from reaching the province. Any winds from the southwest during winter bring in cold and dry weather since most of the precipitation and humidity are released in the Andes. As such, most of the precipitation occurs during summer.
Being located in the Pampas, the province has a cool temperate climate. In general, the province is dominated by two different types of climates: a temperate one in the east and a semi-arid one in the west. Precipitation generally decreases from east to west and from north to south. Being characterized by large thermal amplitudes, the climate of the province has continental characteristics, particularly in the west where thermal amplitudes are much larger. The general atmospheric circulation is one of the most important factors that influence the climate on a regional scale. During summer, the South Atlantic High is displaced to the southeast, which brings hot and humid air masses from the north and northeast. The South Pacific High in summer is responsible for bringing cooler air masses from the southwest which when these two contrasting air masses meet lead to precipitation occurring. In contrast, winters are dry due the northward displacement of the South Atlantic high and the topographic barrier of the Andes north of 40oS which prevents frontal systems that bring precipitation from reaching the province. Any winds from the southwest during winter bring in cold and dry weather since most of the precipitation and humidity are released in the Andes. As such, most of the precipitation occurs during summer.
