Climate

Despite their tropical location, two moving currents affect the islands. The cold Humboldt Current produces the cool and dry garúa season from June to November and the warm marine Panama Current which produces the warm and wet season from December to May.

During the garúa season, cooler waters from the Humboldt Current are driven to the Galapagos by the southeast trade winds, with an average sea temperature of 71°F. As a result, there is warm tropical air passing over cool water. The moisture evaporating from the sea is concentrated in an inversion layer (300 to 600 m above sea level) and the higher parts of the islands, which intercept this layer, receive precipitation in the form of garúa (mist rain). While lowland areas remain dry though cool.

During the warm season the southeast trade winds diminish in strength and warmer waters from the Panama Basin flow through the islands. The average sea temperature rises to 77°F. Warmer waters cause the cool season inversion layer to break up, and Galapagos experience a more typical tropical climate with blue skies and occasionally heavy showers. In some years, the flow of warm water is much greater than normal, and an "El Niño" year results. Surface water temperatures are higher and rainfall can increase greatly. Life on land blossoms but seabirds and sea life, which depend on the more productive, cooler waters, may experience dramatic breeding failures.