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March is typically the warmest and wettest month, with temperatures as high as 30°C and as much as 80 mm of rainfall. [1] Temperature and rainfall vary with elevation, creating a range of microclimates on the higher islands. Average annual temperature declines an average of 0.9°C for every 100 meters of elevation, and rainfall increases.
The mean monthly temperature is 24 °C (75 °F) and the average monthly variation is 7.2 °C (13.0 °F). The daily average maximum temperature is 30 °C (86 °F) from February to April. The daily average minimum temperature is 18 °C (64 °F) in September. There are 2343 sunshine hours in an average year. [15]
Many fish, birds, and marine mammals depend on the phytoplankton. The bottom image shows sea surface temperature, cool up welling waters are coloured purple. Thriving phytoplankton populations are indicated by high chlorophyll concentrations (top image), coloured green and yellow. Images acquired on March 2, 2009.
At Charles Darwin Station, the precipitation during the month of March in the particularly wet year of 1969 was 249.0 mm (9.80 in), but during March 1970 the next year it was only 1.2 mm (0.047 in). There is also a large range in precipitation from one place to another and across the islands' two main seasons.
The ocean temperature plays a crucial role in the global climate system, ocean currents and for marine habitats. It varies depending on depth, geographical location and season. Not only does the temperature differ in seawater, so does the salinity. Warm surface water is generally saltier than the cooler deep or polar waters. [1]
GALÁPAGOS ISLANDS, Ecuador (AP) — Warm morning light reflects from the remains of a natural rock arch near Darwin Island, one of the most remote islands in the Galapagos. The 2021 collapse of ...
This is a list of countries and sovereign states by temperature. Average yearly temperature is calculated by averaging the minimum and maximum daily temperatures in the country, averaged for the years 1991 – 2020, from World Bank Group , derived from raw gridded climatologies from the Climatic Research Unit .
Every now and then, the surface water sloshes back across the ocean, bringing warm water temperatures along the eastern coasts of the Pacific. In non-El Niño years, the Cromwell Current is forced to the surface by underwater seamounts near the Galapagos islands (this is called upwelling.) However, during El Nino years the current does not ...