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Weather in USA
Temperatures in the continental United States vary seasonally. The greatest extremes occur in the vast north- central plains. The frost-free period decreases northward, from more than 240 days along the Gulf of Mexico, to less than 120 days along most of the country's Canadian border. The climate is generally milder along both oceanic coasts than in the interior.
Although the United States experiences wide climatic variation, the precipitation pattern may be depicted as two comparatively humid coasts separated by a progressively less humid interior. Rainfall generally declines westward from the humid eastern zone. The great plains are separated from the pacific coast by the arid landscape of the intermountain basins which receive less than 160mm of rain. Pacific Northwest is the wettest part of the country receiving 1800mm of rain annually. Both Alaska and Hawaii are very humid.
HAWAIIAN ISLANDS
The islands have a tropical oceanic climate with temperatures moderated both by altitude and by regular sea breezes at lower levels. Temperature ranges from 27 degrees centigrade in winter to 33 degrees centigrade in summer. The combination of temperature and humidity is rarely unpleasant due to the trade winds which act as natural air conditioning.
Some mountain slopes on the island of Hawaii are amongst the wettest regions in the world. The islands are occasionally affected by tropical cyclones during the period may to November.