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Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research
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Page 1: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

Extreme oceanic events

David Griffin

CSIRO Marine and Atmospheric Research

Page 2: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

Special thanks to

• Madeleine Cahill• George Cresswell and Jason Middleton• John Wilkin and Alan Pearce• Peter Campbell, Jason Waring, • Kim Badcock (and the whole remote sensing group)• Jim Mansbridge• The Bluelink and IMOS communities (many great people)• Peter Thompson, referees and the panel

Page 3: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

1995 Mass Mortality of Pilchard –due to an extreme ocean event?

?

Page 4: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

• Event was extreme but not unprecedented• Shift focus to the virus• Exposed ill-preparedness for addressing urgent questions• Assembling data took too long• Available data were too few• Too hard to know ‘how anomalous’ various observations were• Nevertheless, I think we got it right• BTW, the next comparable upwelling was not til 2010:

Page 5: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

2010 upwelling event, similar to 1995:

Page 6: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

The cause: occasional summer wind pattern

Sea Surface Temperature

Sea level anomaly

High

wind

Page 7: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

Next, two Qld events. Ocean impact unnoticed?

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beautiful one day….(9 Feb 1997)

Sea level anomaly Sea Surface Temperature

Page 9: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

TC Andrew (25 March 1997) the next.

Sea level anomaly Sea Surface Temperature

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Month later: cold along NGBR

Sea level anomaly

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16 March 2010: TC ULUI

Sea level anomaly

L

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25 May (TC ULUI + 40d)

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30 June 2010 (TC ULUI + 110d)

Fast current,Possibleupwelling

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Tropical cyclones on NWS: hazard to oil and gas.TC Phil 31 Dec 1996, cat 3 but slow moving

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More recently (15 March 2012)

TC Lua

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20 March 2012 (TC Lua + 5d)

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Chlor-a for same day(new on IMOS OceanCurrent):

100km.100km.30m=60t chl-a

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Highest-ever sea level at Fremantle, 2pm WST:

3h period seiche (Molloy, 2001)

MSL

surge

tide

Leeuwin

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Two weeks before storm:

Cold core eddy

Leeuwin

0.4m

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ROAM sea level, 10-12 June 2012.

Sea level anomaly

N

E

Rottnest Is

Cockburn SoundLeeuwin

180km

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CSIRO Bluelink Relocatable Ocean Atmosphere Model sea level, 10 June 2012

200m1000m

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2pm WST 10 June 2012

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Cockburn Sound.Highest sea level: 2pm WST 10 June 2012:

Photo Credit: Steve Brooks, PerthWeatherLivePhoto: Steve Brooks, Perth Weather Live

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A few days later

Photo: Steve Brooks, Perth Weather Live

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Median energy flux of ocean currents

0 Median non-tidal current speed 0.8 (m/s)

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Median energy flux of ocean currents

0 Median non-tidal current speed 0.8 (m/s)

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Cyclonic Eddy(Low sealevel)

Is it real? Yes, see drifter.

Is it extraordinary?Lets look at some history

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Maximum (in 1994-2011) gridded altimetric (+ filtered tidegauge) sea level anomaly:

+1m

SLA

-1m

wide range:

0.3m

to

1.1m

Page 37: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

99th percentile anomaly (exceeded 1% of time) - the max is 30% higher than this

+1m

SLA

-1m

0.2m

0.7m

Page 38: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

1st percentile anomaly (exceeded 99% of time)

+1m

SLA

-1m

-0.7m

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Lowest sea level is 30% lower than 1st %-ile

-1m

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Maximum anomaly map again.highest highs are south of the lowest lows

+1m

SLA

-1m

Lowest low was here

Highest highIs here

Page 41: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

Median elevation (50th percentile)near zero – i.e. distribution is fairly symmetric

+1m

SSHA

-1m

Page 42: Extreme oceanic events David Griffin CSIRO Marine and Atmospheric Research.

Cyclonic Eddy(Low sealevel)

Is it real? Yes, see drifter.

Is it extraordinary?Lets use that history

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16 Jan 2011: Many extreme highs and lows

1.5m/s

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Back 4 days (to 12 Jan)

flood

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Back 4 days (to 8 Jan)

Pre flood:Sea level extreme

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Back 4 days (to 4 Jan)

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Back 4 days (to 31 Dec)

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Back 4 days (to 27 Dec)

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Back 4 days (to 23 Dec)

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That high sea level all along the Qld-NSW coast was not a ‘storm surge’

• Coastal sea level was very high. Anomaly of nearshore current was zero. Odd situation – still needs investigation.

• Lets now go back to 16 Jan then step forward.

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vanishing

growing

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Discussion

• Marine science has tended to focus on the ‘normal’ behaviour of the ocean

• But observing systems are now adequate for us to also focus on the rare occasions when something extreme happens

• Some events have obvious societal impacts, e.g. beach erosion, coastal flooding, coral bleaching, fish kills, oil rig failures

• Many do not – but may – e.g. chlor-a blooms and deserts• Extreme events pose a challenge to observing system

design, quality control of data, and data interpretation• I think the effort is warranted

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Thank you