Southern NSW - Fast Break

Author: | Date: 04 Jan 2019

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You are reading the Fast Break for New South Wales

Volume 1 | Issue 1 | New South Wales | Published: 04 February 2019

Welcome to the first edition of our “Fast Break” newsletter for the Southern New South Wales grains industry. We have been constructing these summaries for the last 11 years in Victoria, and for the last year in South Australia and Tasmania as part of the GRDC funded “Using Seasonal Forecasts Project” project. If you like it, please consider passing it on through your networks and subscribing.

We are describing SNSW as a line south of Dubbo. In the predictions, I divide this region into quarters, hence N, S, E, W, NW, NE, SW, SE, defines zones in this southern half. If the models are more precise I might use terms such as coast, Riverina, central west, etc.

A weak El Niño like ocean appeared in November and December 2018. Despite the central Pacific Ocean and surface interested in the concept of El Niño the atmosphere above in terms of pressure, cloud and wind patterns weren’t having a bar of it. Consequently, the attempt rapidly collapsed to neutral over January. But, a risk still remains that it could come back properly this year.
Current indicators are neutral, or in the case of cloud and tradewinds weakly El Niño.
Similarly, to the same time in 2015, a large slug of warm water remains at depth in the western Pacific. Trade wind reversals to the east of PNG will need to be watched in coming months, as we don’t want to see westerly wind bursts force that warm water over to South America and kick off a more serious El Niño. Current model forecasts suggest a weak one can hang around over autumn but most think it will collapse in winter. Bare in mind, model skill at this time is poor as it will be essentially random weather around PNG that may or may not kick off a potential ElNiño.
The one climate indicator that has been active over summer, has been a positive phase of the Southern Annular Mode. This can increase rainfall in the SE of NSW over summer. This looks to have had some effect in December and January but providing average rainfall to this region rather than wetter.
Pressure position and strength have been generally behaving themselves. A persistent high pressure in the Tasman Sea has stopped the passage of fronts, but allowed some troughing of tropical moisture, particularly to the Central West and a lot of warm air down from the north, increasing temperatures.
Modelled rainfall predictions for SNSW are split between drier and average, but there is a strong model consensus for a continuation of warmer temperatures.

map of Southern NSW showing plant available moisture (%)
The BoM AWRA modelled soil moisture shows very little in the cropping areas of NSW. The exception is Dubbo which had some January rain. Our experience from moisture probes in other states suggest this data is the worst-case scenario if weeds have not been controlled over summer. The harvest rainfall in November and December could be expected to have left low to moderate amounts at depth.
Graphs showing the distribution of global model forecasts for February-April, with models split between drier/average rainfall with likely warmer temperatures
Graphs showing the distribution of global model forecasts for May-July, with models split between average/drier rainfall with likely warmer temperatures

Model consensus forecast for the next six months

Current outlook (28 January)

Current outlook (27 November)

Feb-Apr outlook

May-Jul outlook

Dec-Feb outlook

Feb-Apr outlook

Pacific Ocean

Weak El Niño/ slightly warm

Slightly warm

El Niño (Modoki)

El Niño (Modoki)

Indian Ocean

Slightly warm

Slightly warm

Neutral/slightly warm

Slightly warm

Rainfall

Slightly drier/ average

Average/slightly drier

NA

NA

Temperature

Slightly warmer

Slightly warmer

NA

NA

Equatorial Pacific Ocean Sea surface temperatures have cooled to neutral levels
Sea surface temperatures (SST) along the Equatorial Pacific through November and December were just at or above the El Niño level of 0.8oC. Temperatures have since cooled rapidly in January, such that NINO3 is at +0.38oC and NINO3.4 is +0.36oC (as of 3 Jan), both neutral temperatures. The Indian Ocean Dipole is neutral as is usual over summer. The Coral Sea is warmer than normal, but temperatures are a bit cooler off the NW coast.
Equatorial undersea temperatures in the Pacific remain in a neutral state with warm water in the west.
The Pacific Ocean Equatorial sub-surface temperatures peaked in October and were then on the decline. Support for the El Niño at the surface waned in December and dropped away in January. Currently two distinct pools exist, a cooler in the east and a warmer in the west. If there is reversed trade wind activity in the west, it could potentially push the warmer water under to South America, which doesn’t rule out a second attempt at an El Niño this year.
The SOI value is currently at -0.7
The SOI value is currently at -0.7. This indicates normal pressure patterns around the Equator as measured at Tahiti and Darwin. During summer the SOI is often affected by tropical weather and is a very unreliable indicator.
The Equatorial Pacific trade winds are slightly reversed in the western Pacific
The Equatorial Pacific Easterly Trade Winds are normal in the east and show some vague reversal activity in the west. Watch for strong trade wind reversals as this could indicate a potential reforming of the El Niño.
Cloud is slightly greater at the junction of the Equator with the Dateline
Cloud at the International Dateline (180oW) junction with the Equator is slightly greater (blue colour). This is usually a sign of El Niño but in this case the cloud intensifies to the west instead of to the east. This cloud is more in keeping with the warm Coral Sea. There is a lack of cloud in the Indian Ocean and I am not sure if it means anything over summer.
the SAM has spent most of Summer positive
The Southern Annular Mode (SAM) has been essentially positive since November. In summer, a +SAM can be beneficial to rainfall in the SE of NSW. NOAA predicts the SAM to remain moderately positive for the next fortnight.
the STR of high pressure has move further north than its normal position between Adelaide and Melbourne.
In the past 30 days, the Sub Tropical Ridge of High Pressure’s Position is marginally higher than its summer position of Melbourne. This is stopping some of the moisture from the north coming down. The real feature has been the persistent high in the Tasman Sea that has been allowing hot northerly winds to sweep down. It’s also meant a block to the normal movement of the frontal systems that cause cool changes, meaning that extended heat waves were experienced. There was one exception where a tropical burst of moisture fell on the Central West in January.
Pressure at Darwin and Tahiti are similar, while pressure over SE Australia has been lower.
The Sub Tropical Ridge of High Pressure’s Strength was normal to lower inland and higher along the coast of NSW. The very high blocking pressure in the Tasman Sea can be observed. Some of the northwards feed from that high has provided moisture on the seaward side of the Great Divide. Pressure at Darwin and Tahiti are normal which is why the SOI is neutral.
12 climate models show their predictions for the next six months for the Pacific Ocean, Indian Ocean, rainfall and temperature for SNSW
Download this table in word format here

Modelled Climate and Ocean Predictions for Southern NSW from January 2019 run models

12 climate models show their predictions for the next six months for the Pacific Ocean, Indian Ocean, rainfall and temperature for SNSW

Ocean-Atmosphere Coupled Models

Multi Model Ensembles

Statistical

System 5

ECMWF

Europe

ACCESS-S

BoM

Australia

SINTEX-F

JAMSTEC

Japan

CFSv2

NCEP

USA

GEOS-S2S

NASA

USA

EPS

JMA

Japan

CSM1.1m

BCC

China

GloSea5

UKMO

UK

NMME

USA

MME

APCC

Korea

EUROSIP

Europe

SOI phase

USQ/Qld

Australia

Month of Run

Jan

Jan

Jan

Jan

Jan

Jan

Jan

Jan

Jan

Jan

Jan

Jan

Forecast months

FMA

FMA

MAM

FMA

FMA

FMA

FMA

FMA

FMA

FMA

FMA

FMA

Rainfall Skill

Low

NA

NA

Low/Moderate

Low/Moderate

Low

NA

Moderate

Low/Moderate

NA

NA

NA

Summer Pacific Ocean NINO3.4

Warm

(El Niño)

Warm

(El Niño)

Warm

(weak El Niño)

Warm

(weak El Niño)

Slightly warm

Slightly warm (weak El Niño)

Slightly warm

Slightly warm

Slightly warm

Warm (weak El Niño)

Warm (weak El Niño Modoki)

Consistently near neutral

Summer Eastern

Indian Ocean

Slightly warm

Slightly warm

Slightly warm

Warm

Slightly warm

Neutral

Neutral

Slightly warm

Slightly warm

Slightly warm

Slightly warm

-

Summer Rainfall

Average, slightly drier CW

Average, slightly wetter coast, slightly drier Mallee

Slightly drier

Average

Average

Slightly drier

Slightly drier

Average

Average

Slightly drier, average coast

Average

Average

Summer Temperature

Slightly warmer

Slightly warmer

Slightly warmer

Slightly warmer

Slightly warmer

Slightly warmer

Average

Slightly warmer

Slightly warmer

Slightly warmer

Slightly warmer

-

Forecast months

MJJ

MJJ

JJA

MJJ

MJJ

-

MJJ

AMJ

MJJ

MJJ

AMJ

-

Autumn Pacific Ocean NINO3.4

Slightly warm

Warm

(weak El Niño)

Slightly warm

Warm

(El Niño Modoki)

Neutral

-

Neutral

Neutral

Slightly warm

Slightly warm

Warm (El Niño Modoki)

-

Autumn Eastern

Indian Ocean

Neutral

Slightly warm

Slightly cool (weak +IOD)

Warm

Neutral

-

Neutral/

slightly cool

Slightly warm

Slightly warm

Slightly warm

Slightly warm

-

Autumn Rainfall

Slightly drier

Slightly drier, average coast

Slightly drier

Average

Average

-

Average W, slightly drier E

Average

Slightly drier. average NE

Slightly drier, average coast, far W

Slightly drier E, average W

-

Autumn Temperature

Slightly warmer

Slightly warmer

Slightly warmer

Slightly warmer

Slightly warmer

-

Slightly warmer N,average S

Average

Slightly warmer

Slightly warmer

Slightly warmer

-

Notes

Operational

Operational

Experimental

Operational

Experimental

Experimental

Operational

Operational

Experimental

Summary of 4 dynamic models

Experimental

Summary of 8 dynamic models

Experimental

Summary of 5 dynamic models

5 phase system based on previous 2 months SOI

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