2011 annual rainfall compared against historical rainfall records.
© Australian Bureau of Meteorology.
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The persistent rain of 2010 and 2011 was thanks to La Nina;
a shift in ocean currents and temperatures that alters weather patterns across the
Equatorial Pacific. Usually, there’s
warm water to the East of Indonesia and Australia, warming the air above, which
rises to produce clouds and rain. When La
Nina takes hold, though, sea temperatures are much warmer than normal, creating
more convection (rising warm air), and delivering much more rain.
The effects of La Nina extend much further than the Pacific;
the atmosphere’s global circulation is driven by convection at the equator, and
changes here can affect the rest of the globe: jet streams shift; patterns of
temperature and rainfall on other continents change; and the greatest impact is
in the Northern Hemisphere, not the South.
2011 annual mean temperatures compared against historical
temperature
records. © Australian Bureau of Meteorology.
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1: The thirty
year average is calculated between 1961-1990.
A few more statistics from the Australian Weather Bureau’s AnnualAustralian Climate Statement 2011:
Annual Average Rainfall:
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699mm
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234mm above the long term average, and the third wettest since
records began in 1900.
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Two Year (2010 & 2011) Average Rainfall Total:
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1402mm
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5mm less than the all-time two-year high, and the second wettest on
record.
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Average Mean Temperature:
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21.67oC
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0.14oC below the 30-year average (1961 – 1990) .
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Autumn Mean Temperature:
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1.15oC below average.
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Maximum Recorded Temperature:
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48.1oC
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An all-time record for central South
Australia (measured in Woomera). (Several other locations
measured close to 50oC in late December).
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Warmest year on record for the south-west of Western
Australia.
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1.16oC above average.
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Sea Surface Temperature Anomalies:
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+0.39oC - January
+0.43oC - November
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Second and third warmest Sea Surface Temperature Anomalies
on record.
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Statistics and graphs are the copyright of the Australian Government's Bureau of Meteorology. Presented with permission of the Bureau under the provision for Secondary Distribution of Bureau of Meteorology Information.
Copyright on the remainder of the text: Christopher Lee, 2012.
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