climate outlook – 2011/2012

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Climate Outlook – 2011/2012 Nadraki Weather www.nadraki.com [email protected]

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Climate Outlook – 2011/2012. Nadraki Weather www.nadraki.com [email protected]. El Nino / Southern Oscillation. Normal conditions. Southern Oscillation Index (SOI). - PowerPoint PPT Presentation

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Page 1: Climate Outlook – 2011/2012

Climate Outlook – 2011/2012

Nadraki [email protected]

Page 2: Climate Outlook – 2011/2012

El Nino / Southern Oscillation

Page 3: Climate Outlook – 2011/2012
Page 4: Climate Outlook – 2011/2012
Page 5: Climate Outlook – 2011/2012

Normal conditions

Page 6: Climate Outlook – 2011/2012

Southern Oscillation Index (SOI)

SOI is the standardised anomaly of the Mean Sea Level Pressure difference between Tahiti and Darwin. It is calculated as follows:

[ Pdiff - Pdiffav ] SOI = 10 -------------------

SD(Pdiff) where Pdiff   =   (average Tahiti MSLP for the month) - (average Darwin MSLP for the month),Pdiffav   =   long term average of Pdiff for the month in question, andSD(Pdiff)   =   long term standard deviation of Pdiff for the month in question.

 

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South Pacific Convergence Zone

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Neutral

Page 15: Climate Outlook – 2011/2012

El Nino

Page 16: Climate Outlook – 2011/2012

La Nina

Page 17: Climate Outlook – 2011/2012

References

NIWA Island Climate Update 132 - September 2011

Http://www.niwa.co.nz/node/102804

ENSO Observations www.bom.gov.au/climate/enso/

Fiji Climate Outlook http://www.met.gov.fj/aifs_prods/Outlook.

pdf

Page 18: Climate Outlook – 2011/2012

Climate is what you expect, weather is what

you get Day to day weather is highly variable in

the Pacific.

Large ocean areas and small landmass means minor movements of weather systems can have significant impacts.

It only takes one cyclone to ruin your day!