osse and bio-argo · bio-argo floats measurements o par, ed(380), ed(412), ed(490) o b bp (700):...
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![Page 1: OSSE and Bio-Argo · Bio-Argo Floats Measurements o PAR, Ed(380), Ed(412), Ed(490) o b bp (700): POC proxy o Chla fluorescence: Chla concentration proxy o O2 o NO3 o pH, pCO2, passive](https://reader035.vdocuments.us/reader035/viewer/2022081522/5fc4b9967d8b4053b12f0223/html5/thumbnails/1.jpg)
OSSE and Bio-Argo
North Atlantic Sub-polar Gyre
South Atlantic sub-tropical Gyre
Questions to be addressed
Existing data
Future deployment plans
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Bio-Argo Floats
Measurements
o PAR, Ed(380), Ed(412), Ed(490)
o bbp(700): POC proxy
o Chla fluorescence: Chla concentration proxy
o O2
o NO3o pH, pCO2, passive acoustic, video
Missions
o Temporal resolution configurable: from diel
cycle to Argo 10 day cycling mode: adaptative
sampling strategy
o Vertical configuration configurable: up to 0.1m
resolution
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Sub-polar gyre
• ~3000 profiles over the last 2.5
years
• 7 new floats recently deployed by
US colleagues
• NO3 not well resolved
http://remocean.eu
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Sub-polar gyre
Magnitude of the CO2 sink of biologicalorigin
– Phytoplankton bloom• Timing
• magnitude
• main phytoplankton groups involved (?)
– Export• « Classical » export: sinking of particulate material
when bloom collapses. Sinking rate vsremineralisation rates
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03/01/2016Name of the meeetingLacour et al., GRL, 2015
Bloom Timing and magnitude in the Labrador
Sea: climatological / bioregionalisation
approach
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Sequence of bloom export : one
example in the Labrador Sea
~ 30 time series like
this (but with
nuances…) over
the last two years
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03/01/2016Name of the meeeting
The importance of meso-and sub-
mesoscale in production and export
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Some exemples of
« unclassical way » of
particulate matter export
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Sub-polar gyre
Magnitude of the CO2 sink of biological origin
– Phytoplankton bloom• Timing
• magnitude
• main phytoplankton groups involved (?)
– Export• « Classical » export: sinking of particulate material
when bloom collapses. Sinking rate vs remineralisationrates
• Mixed-layer pump (when re-stratification occurs)
• Eddy-driven pump
• => small-scale regions of intense carbon export?
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Sub-tropical gyre
• ~400 profiles over the
last 2.5 years
• NO3 /O2 well resolved
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Sub-tropical gyre
Balance between oxygen production and
respiration (Net community production):
– From O2 floats time series in North and South
Pacific subtropical Gyre, NCP > 0
• To be adressed in the South Atlantic
– Combined role of nitracline location / avialable
irradiance in driving production at the level of
the Deep Chlorophyll Maximum (DCM): a
seasonal problem.
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From Mignot et al, Global Biogeochemical Cycles 2014
Sub-tropical gyre
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Example of (on-going) time serie in the
South Atlantic subtropical gyre
Name of the meeeting
T S s
Chla bbp/POC
O2 NO3
Ed380 Ed412 Ed490 PAR
CDOM
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AtlantOs Bio-Argo deployment plan
• 7 Bio-Argo floats: where?
– PAR, Ed(380), Ed(412), Ed(490)
– bbp(700): POC proxy
– Chla fluorescence: Chla concentration proxy
– O2
– NO3
• 7 deep O2-Argo : where?
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Planning a global BioGeoChemical-Argo network
Villefranche-sur-mer, January 11-13, 2016
• Science questions
• Sizing the array
– OSSE
– Regionalization approach