submesoscale ncp and gpp rates from underway o 2 / ar and triple oxygen isotope measurements

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Submesoscale NCP and GPP rates from Underway O 2 /Ar and Triple Oxygen Isotope Measurements Rachel H. R. Stanley Rachel H. R. Stanley Woods Hole Oceanographic Woods Hole Oceanographic Institution Institution

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Submesoscale NCP and GPP rates from Underway O 2 / Ar and Triple Oxygen Isotope Measurements. Rachel H. R. Stanley Woods Hole Oceanographic Institution. Primer on Biological Production. NCP = Net Community Production = Net amount of C taken up by ecosystem, should equal export production - PowerPoint PPT Presentation

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Page 1: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

Submesoscale NCP and GPP rates from Underway O2/Ar and Triple Oxygen Isotope Measurements

Rachel H. R. StanleyRachel H. R. Stanley Woods Hole Oceanographic InstitutionWoods Hole Oceanographic Institution

Page 2: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

• NCP = Net Community Production = Net amount of C taken up by ecosystem, should equal export production

• NPP = Net Primary Production = autotrophic component of NCP only• GPP = Gross Primary Production = total photosynthesis

Primer on Biological Production

Page 3: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

• ADVANTAGES– In situ techniques– Integrate over one to two weeks – “Easy” to make measurements so high resolution possible– Includes contribution from DOC– Can be done in underway mode but need some depth info

• PROBLEMS– Rely on gas exchange estimate– What exact time/spatial scale are you measuring?– Have to account for mixing, entrainment, etc.– Doesn’t work well in upwelling regions

Gas Tracers for Measuring PP

Page 4: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

Method: NCP from O2 and Ar• Oxygen produced by photosynthesis, consumed by

respiration, but also affected by physics

• Ar is abiotic analogue for O2 because similar physiochemical properties

Page 5: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

EIMS for Continuous Measurements• Recent advance: continuous at-sea measurements of O2 and

Ar using an Equilibrator Inlet Mass Spectrometer (EIMS) yield thousands of data points of NCP

Page 6: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

EIMS for Continuous Measurements• Recent advance: continuous at-sea measurements of O2 and

Ar using an Equilibrator Inlet Mass Spectrometer (EIMS) yield thousands of data points of NCP

OceanMixed Layer

Wet Lab (at-sea)

EquilibratorCartridge

Quadrupole Mass Spectrometer (QMS)

Measure O2 and Ar

gasfrom

headspace

UnderwayWater

Page 7: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

EIMS for Continuous Measurements• Recent advance: continuous at-sea measurements of O2 and

Ar using an Equilibrator Inlet Mass Spectrometer (EIMS) yield thousands of data points of NCP

Page 8: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

Two Datasets from the Pacific

From Stanley et al, GBC, 2010

WEP

STP

Page 9: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

• Not many variables measured at high enough resolution for comparison with NCP

• Temperature is a measure of physical variability and frontal instabilities

• Correlation analysis is not enough – sections with positive and negative correlation, lags, etc.

NCP and Temperature

From Stanley et al, GBC, 2010WEP

Page 10: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

• Power spectra for temperature and O2/Ar similar at low frequency, but differ at high frequency

Power Spectra

Page 11: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

• PDF=power density function

• Temperature and O2/Ar differ at scales close to 4 km, similar at scales >10 km

Scales of Variability

Page 12: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

• PDF=power density function

• Temperature and O2/Ar differ at scales close to 4 km, similar at scales >10 km

Scales of Variability

Page 13: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

Similar variability between NCP and physics

• Kurtosis -- at scales ranging from 8 to 50 km -- shows similar variability of temperature and O2/Ar (and thus NCP)

• Suggests that processes are related physics is “priming the pump” for biology

But to examine link, really need Process Studies!

Page 14: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

• GPP = Gross Primary Production = total photosynthetic flux• Mass independent fractionation results in atmospheric 17

different than photosynthetic 17.• Sampled discretely while underway or from niskins

GPP from Triple Oyxgen Isotopes

Page 15: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

GPP and NPP• “STP” cruise• GPP and NPP

similar pattern• GPP/NPP ratio

equals 3 to 5 • BUT there are

differences autotrophic respiration (RA), Mehler reaction, or photo-respiration

NPP=GPP-RA

Page 16: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

GPP, NPP and NCP• Do I want any text?

NCP=GPP-RA-RH

Page 17: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

Energy Flow Diagrams• Diagrams drawn

to scale

• Differences in regions: total amount of energy & its distribution between boxes

• Caveats: measurement uncertainty, VGPM NPP

Page 18: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

• NCP can be measured continuously from underway system from O2/Ar ratios

• Submesoscale variability in NCP similar to that in physics

• GPP can be measured discretely from underway water or Niskins

• Combination of GPP, NCP and NPP describe energy flow variations in autotrophic respiration may be important

• NEED some CTD cast samples to correct for entrainment (Nicholson et al, submitted)

Conclusions

Page 19: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements

Collaborators:– Raf Ferrari (MIT), Michael Bender (Princeton), John

Kirkpatrick (UW)– Captain and crew of R/V Kilo Moana and NOAA ship

Kai’imomoana•Funding Sources:

– NSF Chemical Oceanography– WHOI Penzance Fund for Assistant Scientists

Acknowledgements

Page 20: Submesoscale  NCP and GPP rates from Underway O 2 / Ar  and Triple Oxygen Isotope Measurements