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  2. Climate change in Fiji - Wikipedia

    en.wikipedia.org/wiki/Climate_change_in_Fiji

    Similar to the majority of countries around the world, Fiji's temperature is rising as a result of climate change. The average maximum temperature of the country is rising at a rate of roughly 0.16 °C per year and has risen by almost 1.0 °C since 1950. [8]

  3. Ocean temperature - Wikipedia

    en.wikipedia.org/wiki/Ocean_temperature

    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]

  4. Baffin Bay - Wikipedia

    en.wikipedia.org/wiki/Baffin_Bay

    Average January temperatures are −20 °C (−4 °F) in the south and −28 °C (−18 °F) in the north. In July, the average temperature is 7 °C (45 °F). The annual precipitation is 100–250 mm (3.9–9.8 in) on the Greenland side and about twice as much near Baffin Island. [3]

  5. Fiji Water: So cool, so fresh, so bad for the environment?

    www.aol.com/news/2009-08-24-tale-of-fiji-water...

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  6. Suva - Wikipedia

    en.wikipedia.org/wiki/Suva

    Suva averages 3,000 mm (118 inches) of precipitation annually. Its driest month, July, averages 125 mm (4.92 in). As in many other cities with a tropical rainforest climate, temperatures are relatively constant throughout the year, with an average high of about 28 °C (82 °F) and an average low of about 22 °C (72 °F).

  7. Geography of Fiji - Wikipedia

    en.wikipedia.org/wiki/Geography_of_Fiji

    Fiji's location in Oceania Topography of Fiji. Fiji is a group of volcanic islands in the South Pacific, lying about 4,450 kilometres (2,765 mi) southwest of Honolulu and 1,770 km (1,100 mi) north of New Zealand. Of the 332 islands and 522 smaller islets making up the archipelago, about 106 are permanently inhabited. [1]

  8. Sea surface temperature - Wikipedia

    en.wikipedia.org/wiki/Sea_surface_temperature

    A wet-bulb temperature at 500 hPa in a tropical atmosphere of −13.2 °C (8.2 °F) is required to initiate convection if the water temperature is 26.5 °C (79.7 °F), and this temperature requirement increases or decreases proportionally by 1 °C in the sea surface temperature for each 1 °C change at 500 hpa.

  9. El Niño–Southern Oscillation - Wikipedia

    en.wikipedia.org/wiki/El_Niño–Southern...

    An especially strong Walker circulation causes La Niña, which is considered to be the cold oceanic and positive atmospheric phase of the broader El Niño–Southern Oscillation (ENSO) weather phenomenon, as well as the opposite of El Niño weather pattern, [19] where sea surface temperature across the eastern equatorial part of the central ...

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