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The Bottom Line
SOI in Near Zero Phase at end of June.
Dave McRae, Qld Climate Change Centre of Excellence, 30/06/09.
The monthly value of the SOI for May was minus 4.9 and for June was
minus 2.8. This places the SOI in a Consistently Near Zero SOI phase.
Based on a Consistently Near Zero SOI phase at the end of June and
historical rainfall records there is a 30 to 40% chance of getting above
the long term median rainfall for July through to the end of September
across most of Queensland (or depending on how you look at things a 60
to 70% chance of getting below median rainfall).
The exception is for the region to the south east of the Gulf of
Carpentaria where there is a 50 to 70% chance of getting above median
rainfall for July to September. However median rainfall levels at this
time of year in that region are low. For example Normanton has a July to
September median rainfall of 1mm, Julia Creek has a July to September
median rainfall of 6mm and Richmond has a July to September median
rainfall of 8mm.
When using a climate forecast you should remember that the probability
or percent chance of something occurring is just that - a probability.
For example if there is a 70% chance of recording more than 100 mm there
is also a 30% chance of recording less than 100 mm i.e. 70-30; 30-70. It
does not mean that you will get 70% more than 100 mm or 100 mm plus
another 70%.
For those who like to follow the relationship between the SOI and
rainfall patterns in more detail have a look at what happened in your
area during July to September in the following years since 1950 that
have had a 'Consistently Near Zero' SOI phase at the end of June; 1954,
1960, 1961, 1969, 1976, 1979, 1980, 1991, 1995 and 1999.
For example at Kingaroy, below average rainfall for July to September in
those years was recorded 4 times, close to average rainfall was recorded
4 times and above average rainfall was recorded only 2 times. Therefore
rainfall at Kingaroy during July to September is more likely to be below
average to average than well above average. For more information on
historical rainfall data for your region try Rainman Streamflow or
www.longpaddock.qld.gov.au
It will be interesting to see if strongly negative SOI values develop
over coming months. If the 30 day average of the SOI where to fall into
strongly negative values and remain there, it would increase the chance
of a dry late winter/spring. You can receive a text message with the
latest SOI values sent to your mobile phone. To subscribe to this free
service, call me on (07) 4688 1459 or e-mail
david.mcrae@climatechange.qld.gov.au
The Full Story
Rainfall probabilities fall/increased risk of El Nino climate pattern.
Dave McRae, Qld Climate Change Centre of Excellence, 03/07/09
The monthly value of the SOI for May was minus 4.9 and for June was
minus 2.8. This places the SOI in a Consistently Near Zero SOI phase.
Based on a Consistently Near Zero SOI phase and historical rainfall
records there is a 30 to 40% chance of getting above the long term
median rainfall for July through to the end of September across most of
Queensland (or depending on how you look at things a 60 to 70% chance of
getting below median rainfall).
The exception is for the region to the south east of the Gulf of
Carpentaria where there is a 50 to 70% chance of getting above median
rainfall for July to September. However median rainfall levels at this
time of year in that region are low. For example Normanton has a July to
September median rainfall of 1mm, Julia Creek has a July to September
median rainfall of 6mm and Richmond has a July to September median
rainfall of 8mm.
When using a climate forecast you should remember that the probability
or percent chance of something occurring is just that - a probability.
For example if there is a 70% chance of recording more than 100 mm there
is also a 30% chance of recording less than 100 mm i.e. 70-30; 30-70. It
does not mean that you will get 70% more than 100 mm or 100 mm plus
another 70%.
For those who like to follow the relationship between the SOI and
rainfall patterns in more detail have a look at what happened in your
area during July to September in the following years since 1950 that
have had a 'Consistently Near Zero' SOI phase at the end of June; 1954,
1960, 1961, 1969, 1976, 1979, 1980, 1991, 1995 and 1999. For example at
Kingaroy, below average rainfall for July to September in those years
was recorded 4 times, close to average rainfall was recorded 4 times and
above average rainfall was recorded only 2 times. Therefore rainfall at
Kingaroy during July to September is more likely to be below average to
average than well above average. For more information on historical
rainfall data for your region try Rainman Streamflow or
www.longpaddock.qld.gov.au
It will be interesting to see if strongly negative SOI values develop
over coming months. If the 30 day average of the SOI where to fall into
strongly negative values and remain there, it would increase the chance
of a dry late winter/spring. You can receive a text message with the
latest SOI values sent to your mobile phone. To subscribe to this free
service, call me on (07) 4688 1459 or e-mail
david.mcrae@climatechange.qld.gov.au
According to the latest ENSO Wrap-up from the Bureau of Meteorology
www.bom.gov.au/climate/enso more evidence of a developing El Nino
climate pattern has emerged during the last few weeks. This is reflected
by central and eastern Pacific Ocean sea surface temperatures being
significantly warmer than the long-term average and a distinct warming
of sub-surface temperatures throughout the eastern Pacific during June.
This is a trend away from the La Nina like climate pattern that was a
feature of the last 9 months.
This trend is also consistent with the output of the surveyed
international climate models which all indicate the development of an El
Nino climate pattern later this year. None of the surveyed climate
models are forecasting any potential return of La Nina or La Nina like
conditions.
The message should not be "doom and gloom" another El Nino may be
approaching. Rather this is an opportunity to take a risk management
approach. Review your business, cropping, stocking, fodder, water use
plans for the coming winter and spring, assess the seasonal conditions
experienced in your area to date and the resources (soil moisture,
grass, water, money, equipment) you have available, monitor changes in
the seasonal climate outlook over coming months and adjust your plans if
and as necessary.
Typically during an El Nino event, there is a low chance of getting
above median rainfall during winter, spring and early summer throughout
Queensland. The impact of an El Nino around the state will vary
depending on the seasonal conditions experienced during summer (e.g.
water supply levels for urban and agriculture, sub-soil moisture profile
for cropping/horticulture/pasture/tree growth). As most of central and
northern Queensland recorded average to above average rainfall over the
summer rainfall season, the immediate impact of a potential El Nino
event this year on food production and water supply etc is likely to be
minimal.
This is in contrast however, to parts of southern Queensland such as the
Darling Downs and south west of the state where average to below average
rainfall was recorded over the summer rainfall season. This is following
on from a number of years of drought.
Also of some interest is the recent trend to positive values in the
Indian Ocean Dipole (IOD). If this trend is maintained (and if coupled
with an El Nino climate pattern) there is an increased risk of below
average winter rainfall especially throughout south-eastern Australian.
For more information try www.bom.gov.au/climate/IOD/
SOI influence on climate varies across Australia (greatest skill is for
eastern Australia) and between seasons (usually greatest skill is for
winter, spring and early summer). Therefore users of the SOI and any
other seasonal forecasts are urged to investigate skill level for their
location by using such tools as Rainman StreamFlow.
When I'm asked about how climate information can be used I refer to a
couple of key points developed from client feedback. Key points include
that management decisions should never be based entirely on one factor
such as a climate or weather forecast. As always, everything that could
impact of the outcome of a decision (soil moisture, pasture
type/availability, crop and commodity prices, machinery, finance, costs
etc) should be considered. For example, the level of soil moisture at
planting is the major factor influencing crop yield or success.
A simple cost benefit analysis when making a major decision may also be
useful. For example what will I gain if I get the desired outcome? What
will I lose (sleep, money, family relationships) if I do not get the
desired outcome and what other options (risk neutral) are there? A PART
OF THIS PROCESS IS TO HELP MANAGERS TO BE CAREFUL NOT TO CHANGE FROM
NORMAL RISK MANAGEMENT TO HIGH LEVEL RISK TAKING BASED ON A PIECE OF
INFORMATION (SUCH AS A CLIMATE FORECAST).
Forecasts as well do not always give a strong signal as to likely
conditions for your location. In assessing climate forecasts as a
management tool consider the level of signal for the key decision times
in your location. Rainman StreamFlow is a useful tool for this.
| what is:
"Seasonal Climate Outlook" ? |
| The term "Seasonal Climate" refers
to what the weather was, is, is-likely-to-be for a particular season. The
"Outlook" is based on the Southern
Oscillation Index (SOI), Sea-Surface
Temperature (SST) patterns in the Pacific Ocean are also important in
driving climate variability and are useful guides to potential climate patterns
in Australia (and other parts of the world too). One rainfall probability system used in Queensland is the "SOI
Phase System", the current "Outlook
Message" gives commentary on the seasonal outlook and additional information may be found at the Queensland Climate Change Centre of Excellence. You will also
find the "Winter
Crop Outlook" on the Department of Primary Industries web site. |
|