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THE CLIMATE OF FIJI
Fiji enjoys a tropical maritime climate without great
extremes of heat or cold.
Winds
At all seasons the predominant winds over Fiji are the
trade winds from the east to south-east. On the coast of
both main islands Viti Levu and Vanua Levu, day time sea
breezes blow across with great regularity. In general,
the winds over Fiji are light or moderate; strong winds
are uncommon and are most likely to occur in the period June to
November when the trade winds are most persistent.
Temperatures
Temperatures at the lower levels around Fiji are fairly
uniform. In the leeward side of the mountains, however,
on the western and northern sides of the main islands
(including Taveuni), the day-time air temperatures often
rise 1°C to 2°C above those on the windward sides or
on the smaller islands. Also, the humidity on the
leeward side tends to be somewhat lower. Due to the
influence of the surrounding ocean, the changes in
the temperature from day to day and season to season
are relatively small. The average temperatures
change by only about 2°C to 4°C between the coolest months (July and
August) and the warmest months (January and February).
Around the coast, the average night-time air
temperatures can be as low as 18°C to 20°C and the
average day-time temperatures can be as high as 30°C to
32°C. South-eastern coastal areas and the high interior
often experience persistent cloudy humid weather.
Rainfall
Rainfall is highly variable and mainly orographic
(influenced by the island topography and the prevailing
south-east trades). The south-east trade winds are
saturated with moisture, any high land mass lying in
their path receives much of the precipitation. The
mountains of Viti Levu and Vanua Levu create wet
climatic zones on their windward sides and dry climatic
zones on their leeward sides, hence, the main islands
have pronounced dry and wet zones. Little climatic
differentiation occurs on the smaller islands having low
relief. Fiji experiences a distinct wet season (November
to April) and a dry season (May to October) that is
controlled largely by the north and south movements of
the South Pacific Convergence Zone which is the main
rainfall producing system for the region. Much of the
Fiji’s rain however falls in heavy brief local showers.
Rainfall is usually abundant during the wet season
(November to April), especially over the larger islands,
and it is often deficient during the rest of the year,
particularly in the ‘dry zone’ on the north western
sides of the main islands. In the drier half year, from
May to October, the heaviest rainfall occurs on the
windward (south-east) parts of the larger islands.
Annual rainfall in the dry zones averages around 2000mm,
whereas in the wet zones, it ranges from 3000mm around
the coast to 6000mm on the mountainous sites. The
smaller islands receive amounts intermediate between
those on the wet and dry sides of the larger islands.
The south-eastern parts of main islands, generally
receive monthly total rainfall of 150mm during the dry
season and 400mm during the wettest months. These parts
of the islands have rain on about six out of ten days
for the dry season and about eight out of ten days in
wet season. The north-western parts of these islands are
in the rain shadow and receive generally less than 100mm
per month during the dry period. The variation in the
monthly totals between the two zones during the wet
season is little. The wettest month is usually March and
the driest month is almost always July. During the wet
season, brief heavy afternoon showers and thunderstorms
are common. Fiji experiences prolonged dry spells quite
often, usually for three to four months duration, when
the north-western parts of the main islands receive
little or no rain. The ENSO (El Nino Southern
Oscillation) phenomenon appears to be a major
contribution to the fluctuations of climate, especially
rainfall in the South Pacific. It has been seen that
during most of the ENSO episodes, the rainfalls are
extremely low in the dry zones. Due to the great
variability of rainfall in the region, averages have
little value as indicators of what the rainfall is
likely to be in any particular month or season.
Tropical Cyclones
Fiji lies in the area occasionally traversed by tropical
cyclones. They are mostly confined to the period
November to April, with greatest frequency around
January and February. On average, some ten to twelve
cyclones per decade affect some part of Fiji, and two or
three causing severe damage. Specific locations may not
be directly affected for several years but the dominant
north-west tracks give some increased risk of damage in
the outlying north-west island groups.
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