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Preliminary Results of the CASCADE Cruise (Gulf of Lions)
R/V l’Atalante, 01 - 23 March 2011CEFREM, ICM-CSIC, UB, UPM, IFREMER, LA, HCMR, LOV, LMGEM, LOMIC, UA
CASCADE: CAscading, Storm, Convection, Advection and Downwelling Events
Cascading : Down-slope cascade of dense water formed along the coast
Wind-driven mixing and cooling of the upper layer of the ocean during winter
Open-Sea convection : Deepening of the mixed layer thickness in the open ocean
Situation for the Gulf of Lions
Marin
Quantification of the export of dissolved and particulate organic and inorganic matter, as well as microorganisms (free and attached bacteria, phytoplankton)
=> validation of coupled models
Open-sea convection event
02 Feb - Chlorophylle
05 Mar - Chlorophylle
Radiale L
Rad
iale
M
Difference phases of open-sea convectionPreconditionning
General circulation and winds combine to predispose some part of a gyre to locally overturn
Mixing
Heat loss associated with the wind exceed some critical level and initiates convection
Sinking
Sinking and restratification of the water column, once the surface forcing decline
Spreading
Dispersion of newly formed deep mixed water
Transfer and sequestration of organic matter in the deep basin Response of deep ecosystems
Aft
er
He
len
Jo
hn
s (h
ttp:/
/puddle
.mit
.edu/~
hele
n/o
odc.
htm
l)
Hints of pelagic ecosystem response to convection
Bursts of deep (near-bottom) bio-luminescence measured by photomultiplier following convection events
Both mechanical stimulation (current-induced)
and
spontaneous stimulation (bacterial growth due to nutrients inputs from surface and sediment)
103
102
10
13.3
13.2
40
30
10
0
20
Jan 2008 Jul 2008 Jan 2009 Jul 2009 Jan 2010
13.1
13.0
12.9
104
Pot. temperature (deg. C)
Current speed (cm/s)
Number of photon per seconds
Jul 2010
Aft
er
Ta
mb
urin
i et
al (
su
bm
itte
d t
o S
cie
nce
)
De
pth
(m
)
Potential temperature (°C) Chlorophylle (µg/L)
0
500
1000
1500
2000
250012.90 13.25 0 0.15
4 march8 march
Sinking and spreading
Rapid shift from a convective (homogenized) to a stratified regime within few days
Levantine Intermediate water
Old deep water
Mixed layer depth
New deep water
Capping of newly formed deep water by Levantine intermediate water
Export of dissolved and particulate, organic and inorganic matter and
bacterial activity (preserving in situ hyperbaric conditions) during and outside convective periods in old and new deep waters
10 March - Turbidity
18 March - Turbidity
Storm, Downwelling and Cascading Event
(cm/s)
Suspended sediment concentration (mg/l)
Simulation of bottom currents for March 13, 2011(peak of the 1st storm)
Monitoring of the storm
In the Cap de Creus Canyon
Moorings
CTD station and transect
2 days of fixed CTD YoYo-ing during the stormTransect after the stormContinuous recording with moorings
Current, turbidity, and particle fluxes
ADCP Echo amplitude
(count)
ADCP current speed (cm/s)
1st storm 2nd storm
Sediment traps samples (36h interval)
Large current (up to 90 cm/s), turbidity(up to 25 mg/l), and particles fluxes
Export of dissolved and particulate organic and inorganic matter, as well as microorganisms (free and attached bacteria, phytoplankton) on water, trap samples, and sediment
Signature of dense water plume
Turbidity
Temperature
Salinity
Oxygene
Transect performed after the 1st storm (March 14, 2011)
2011 : warm and wet winter with weak formation of dense shelf water.
Export of existing dense water possible due to the occurrence of E-SE storms that flushed the shelf