What is mexicos climate

Northern Mexico gets very hot during summer with sudden violent heavy rain or hail storms, also an isolated tornado can occur within these storms. Seasonal variations in temperature are small, but May is the warmest month of the year, and January the coldest, when night frost is even possible. Mexico City experiences high average annual rainfall, most falling in summer. During hurricane season June - November , hurricanes are common in the coastal cities specially those near the Caribbean Sea and the Gulf of Mexico.

Similar to Central Australia and the Sahara Desert which typically means extremely hot summers and freezing cold winters. Outlook at Guanajuato, Mexico.

Similar to the Kenyan highlands which means mild temperatures, low humidity, and tons of rainfall during the summer season. States: Tamaulipas, Guanajuato , Hidalgo.

Similar to Southern Brazil and Uruguay, which means hot humid summers and mild winters, and rainfall throughout the year. The Border between Tijuana and California. Similar to European Mediterranean and Californian coast, this area in Mexico near TIajuana has dry summers and gets rainfall only during the winters.

Even with a summary of the 7 different climate zones in Mexico, there are hundreds of sub-genres of climates in each region. We love tropical weather with cool temperatures, and we live in a semi-arid climate in Mexico. Explore Mexico and decide for yourself! Daytime temperatures begin warming in March and reach an average high of 90 by May, but relatively low humidity keeps the climate somewhat comfortable during the hot season. The rest of the year the average high ranges from the mids to the low 80s and lows seldom drop below 45 F.

Almost two-thirds of the country consists of plateaux and high mountains with a climate that is warm-temperate; other parts have a tropical climate with temperature reduced by altitude. There are three important climatic influences which help to determine the character of the climate in Mexico and her different regions. The cold Californian current, which sweeps southwards on the Pacific coast, has the effect of lowering temperatures and reducing rainfall on the west coast as far south as the tip of the peninsula of Lower California.

This and the influence of the North Pacific anticyclone help to make much of northwestern Mexico desert or semi-desert; this is a continuation of the dry zone of the United States in southern California, New Mexico, and Arizona.

The warm waters of the Caribbean Sea, and the influence of the constant northeast trade winds, make the eastern coastal region a typical tropical coast with a marked single wet season in summer. The weather and climate of this region, particularly south of Tampico, have much in common with that of the Caribbean Islands. An important influence is the presence to the north of the great continental landmass of North America.

This area becomes very cold in winter — particularly when cold air sweeps down from the Canadian Arctic — and very warm in summer. The northern part of Mexico shares these extreme temperature conditions. Snow has fallen as far south as Tampico, which is within the tropics. The west coast is protected from such cold waves by the mountains and plateaux of central Mexico.

Only a very narrow coastal belt on the Pacific shore falls into the tierra caliente category, but there is a more extensive area on the Caribbean shore, including the whole Yucatan peninsula. The largest part of Mexico falls into tierra templada and tierra fria. This division takes little account of rainfall and is mainly on the basis of temperature.

The rainy season over the whole country is the period of high sun from May to October. The rest of the year is not completely rainless, but the amount and frequency of rain in the winter season is low. The wettest part of the country is the lowland on the Caribbean coast; the north coast of the Yucatan peninsula is relatively much drier than the east coast or the interior.

Rainfall is heaviest where the coast is backed by high mountains.