Simulating the variability of Florida Current frontal eddies
Contents Agulhas Current Variability: A challenge across ... · the northern Agulhas Current in the...
Transcript of Contents Agulhas Current Variability: A challenge across ... · the northern Agulhas Current in the...
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Contents
Agulhas Current Variability:
A challenge across industry sectors
Marjolaine Krug
Ecosystem Earth Observations (CSIR-NRE)
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• Intense ship traffic
• Strong currents
• Intense and frequent of storms
• Intense Wave / Current interactions
which results in crossing seas and
rogue waves (up to half of ship
accidents due to bad weather occur
in crossing seas)
Image provided in Ocean-Volvo race
Damage caused by rogue wave and Ship wrecks
location
Ship traffic from AIS on 10 Jan 2016 (image
by Rory Meyer - Meraka)
Background
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Background
• Strongest western boundary current of the southern hemisphere and maybe of the
world (Bryden 2005)
• Driven by the anticyclonic wind circulation of the South-Indian subtropical gyre
• Starts around Ponto de Ouro (27oS, Mozambique) - Ends at the retroflection (40oS)
• Variability in the Mozambique Channel and south of Madagascar transmitted into
the northern Agulhas Current in the form of deep sea eddies, which can lead to the
formation of large cyclonic Agulhas Current meanders
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Mesoscale variability
Trajectories of surface drifters
reaching the Natal Bight
between 1992 and 2002
(Braby et al., 2016)
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Mesoscale variability
Sea surface temperature and
currents derived from sea
surface height show presence of
large Agulhas meander
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EO monitoring
Deriving index of variability from altimetry (method in Krug et al., 2014).
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EO monitoring
Year 2000
The year of the great Agulhas
Current Early Retroflection
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EO monitoring
Altimetry challenged by lack of
temporal and spatial coverage
when monitoring smaller
scales and / or rapidly evolving
structures.
Potential to exploit other
remote sensing products such
as SST for EO monitoring.
(Rouault and Penven 2011)
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EO monitoring
Daily changes in the position
of the Agulhas Current
northern wall derived from
merged Odyssea SST.
(Krug et al., submitted)
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Sub-mesoscale variability
Sub-mesoscale
variability at the Agulhas
Current northern wall.
Observations collected
during the Shelf Agulhas
Glider Experiment
(SAGE).
(Krug et al., submitted)
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Sub-mesoscale variability
Max ζ/f = 1.02
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Future plans
Exploiting new EO datasets
Increasing our in-situ observations
Improving our models