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Seasonal Climate Outlook: February - April 2011

Warmer than normal conditions likely to continue into autumn.

The equatorial Pacific remains in a strong La Niña state, which is expected to persist into the start of autumn 2011, says the NIWA National Climate Centre. Beyond this time, there is disagreement between the forecast models as to whether La Niña will continue into winter at a weaker level, or whether a transition to neutral conditions will occur.

Early autumn temperatures (February to April) are likely to be above average in all regions, except in the east of the both Islands where average or above average temperatures are equally likely.

Seasonal rainfall is likely to be normal or above normal in all North Island regions, and near normal in all South Island regions. Soil moisture levels and river flows during February–April are likely to be above normal in all North Island regions, normal or below normal on the east coast of the South Island, and near normal elsewhere in the South Island.

The seasonal outlook states that mean sea level pressures are likely to be below normal to the north of New Zealand, with weaker westerlies across the country.

Tropical cyclone activity is likely to be near- or above-normal this season (through to May 2011). The risk of an ex-tropical cyclone passing close to New Zealand is slightly above the long-term average. On average, at least one ex-tropical cyclone passes within 500km of New Zealand in 9 out of 10 cyclone seasons.

 


Overall Picture

Temperature:

On average for early autumn (February-April), temperatures are likely to be above average in all regions, except in the east of the North Island and the east of the South Island where average or above average temperatures are equally likely. Sea surface temperatures are presently slightly above normal around the North Island, and over the coming three months are expected to warm further above the normal for this time of year.

Rainfall, soil moisture, and river flows:

The National Climate Centre says that the expected lower pressures to the north of the country are likely to result in early autumn seasonal rainfall being normal or above normal across the North Island. Soil moisture levels and river flows are also likely to be above normal in all North Island regions. For the South Island, rainfall is likely to be near normal in all regions, whereas soil moisture levels and river flows are likely to be normal or below normal on the east coast of the South Island, and near normal elsewhere.

Regional predictions for the next three months:

Northland, Auckland, Waikato, Bay of Plenty:

Temperatures are likely to be above average.  Seasonal rainfall totals over February-April are equally likely to be near normal or above normal. Soil moisture levels and river flows are likely to be above normal.

Probabilities are assigned in three categories; above average, near average, and below average. The full probability breakdown is:

Temperature Rainfall Soil moisture River flows
Above average 55% 40% 45% 45%
Near average 30% 40% 35% 35%
Below average 15% 20% 20% 20%

Click these links to view the historic rainfall and temperature ranges for this region

Central North Island, Taranaki, Wanganui, Manawatu and Wellington:

Temperatures are likely to be above average. Seasonal rainfall totals over February-April are equally likely to be either near normal or above normal, whereas soil moisture levels and river flows are likely to be above normal.

Probabilities are assigned in three categories; above average, near average, and below average. The full probability breakdown is:

Temperature Rainfall Soil moisture River flows
Above average 55% 40% 45% 45%
Near average 30% 40% 35% 35%
Below average 15% 20% 20% 20%

Click these links to view the historic rainfall and temperature ranges for this region

Gisborne, Hawke’s Bay, Wairarapa:

Temperatures are equally likely to be near average or above average. Seasonal rainfall totals are equally likely to be in the near normal or above normal range. Soil moisture levels and river flows are likely to be above normal.

Probabilities are assigned in three categories; above normal, near normal, and below normal.The full probability breakdown is:

Temperature Rainfall Soil moisture River flows
Above average 40% 40% 45% 45%
Near average 40% 40% 35% 35%
Below average 20% 20% 20% 20%

Click these links to view the historic rainfall and temperature ranges for this region

Nelson, Marlborough, Buller:

Temperatures are likely to be in the above average range. Seasonal rainfall, soil moisture levels, and river flows are likely to be in the normal range.

Probabilities are assigned in three categories; above average, near average, and below average. The full probability breakdown is:

Temperature Rainfall Soil moisture River flows
Above average 50% 35% 35% 35%
Near average 30% 45% 45% 45%
Below average 20% 20% 20% 20%

Click these links to view the historic rainfall and temperature ranges for this region

West Coast, Alps and Foothills, Inland Otago, Southland:

Temperatures are very likely to be above average, for the three months as a whole. Seasonal rainfall, soil moisture levels, and river flows are likely to be in the normal range.

Probabilities are assigned in three categories; above average, near average, and below average. The full probability breakdown is:

       Temperature            Rainfall     Soil moisture River flows
Above average 60% 20% 30% 30%
Near average 30% 45% 40% 40%
Below average 10% 35% 30% 30%

Click these links to view the historic rainfall and temperature ranges for this region

Coastal Canterbury, East Otago:

Temperatures are equally likely to be in the near average or above average range. Seasonal rainfalls are likely to be near normal, whereas soil moisture levels and river flows are equally likely to be in the near normal or below normal range.

Probabilities are assigned in three categories; above average, near average, and below average. The full probability breakdown is:

Temperature Rainfall Soil moisture River flows
Above average 40% 30% 20% 20%
Near average 40% 45% 40% 40%
Below average 20% 25% 40% 40%

Click these links to view the historic rainfall and temperature ranges for this region

Background

The tropical Pacific is in a strong La Niña state, which is likely to persist into early autumn 2011. Beyond that time, the evolution of the El Niño/La Niña cycle is uncertain. The present event has persisted since August 2010, and atmospheric indicators show this episode to be one of the strongest of the last 100 years. Previous very intense La Niña events occurred in 1975/76, 1971, and in 1917 (probably the strongest historically according to atmospheric indicators in the tropical Pacific).

For comment, please contact:

Dr Brett Mullan, NIWA Principal Scientist, Climate Variability & Change

Tel (04) 386 0508

Dr James Renwick, NIWA Principal Scientist, Climate Variability & Change

Mobile (021) 178 5550, Tel (04) 386 0343 (office DDI)

© Copyright NIWA 2011. All rights reserved. Acknowledgement of NIWA as the source is required.


Notes to reporters & editors

1. NIWA’s outlooks indicate the likelihood of climate conditions being at, above, or below average for the season as a whole. They are not ‘weather forecasts’. It is not possible to forecast precise weather conditions three months ahead of time.

2. The outlooks are the result of the expert judgment of NIWA’s climate scientists. They take into account observations of atmospheric and ocean conditions and output from global and local climate models. The presence of El Niño or La Niña conditions and the sea surface temperatures around New Zealand can be a useful indicator of likely overall climate conditions for a season.

3. The outlooks state the probability for above average conditions, near average conditions, and below average conditions for rainfall, temperature, soil moisture, and river flows. For example, for winter (June-July-August) 2007, for all the North Island, we assigned the following probabilities for temperature:

· Above average: 60%

· Near average: 30%

· Below average: 10%

We therefore concluded that above average temperatures were very likely.

4. This three-way probability means that a random choice would only be correct 33% (or one-third) of the time. It would be like randomly throwing a dart at a board divided into 3 equal parts, or throwing a dice with three numbers on it. An analogy with coin tossing (a two-way probability) is not correct.

5. A 50% ‘hit rate’ is substantially better than guess-work, and comparable with the skill level of the best overseas climate outlooks. See, for example, analysis of global outlooks issued by the International Research Institute for Climate and Society based in the U.S. (http://iri.ldeo.columbia.edu/) published in the Bulletin of the American Meteorological Society (Goddard, L., A. G. Barnston, and S. J. Mason, 2003: Evaluation of the IRI's “net assessment” seasonal climate forecasts 1997-2001. Bull. Amer. Meteor. Soc., 84, 1761-1781).

6. Each month NIWA publishes an analysis of how well its outlooks perform. This is available on-line and is sent to about 3,500 recipients of NIWA’s newsletters, including many farmers. See The Climate Update: www.niwascience.co.nz/ncc

7. All outlooks are for the three months as a whole. There will inevitably be wet and dry days, hot and cold days, within a season. The exact range in temperature and rainfall within each of the three categories varies with location and season. However, as a guide, the “near average” or middle category for the temperature predictions includes deviations up to ±0.5°C from the long-term mean, whereas for rainfall the “near normal” category lies approximately between 80% and 115% of the long-term mean.

8. The seasonal climate outlooks are an output of a scientific research programme, supplemented by NIWA’s Capability Funding. NIWA does not have a government contract to produce these outlooks.