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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.

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Presentation on theme: "Submesoscale NCP and GPP rates from Underway O 2 /Ar and Triple Oxygen Isotope Measurements Rachel H. R. Stanley Woods Hole Oceanographic Institution."— Presentation transcript:

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

2 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

3 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

4 Method: NCP from O 2 and Ar Oxygen produced by photosynthesis, consumed by respiration, but also affected by physics Ar is abiotic analogue for O 2 because similar physiochemical properties

5 EIMS for Continuous Measurements Recent advance: continuous at-sea measurements of O 2 and Ar using an Equilibrator Inlet Mass Spectrometer (EIMS) yield thousands of data points of NCP

6 EIMS for Continuous Measurements Recent advance: continuous at-sea measurements of O 2 and Ar using an Equilibrator Inlet Mass Spectrometer (EIMS) yield thousands of data points of NCP Ocean Mixed Layer Wet Lab (at-sea) Equilibrator Cartridge Quadrupole Mass Spectrometer (QMS) Measure O 2 and Ar gas from headspace Underway Water

7 EIMS for Continuous Measurements Recent advance: continuous at-sea measurements of O 2 and Ar using an Equilibrator Inlet Mass Spectrometer (EIMS) yield thousands of data points of NCP

8 Two Datasets from the Pacific From Stanley et al, GBC, 2010 WEP STP

9 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, 2010 WEP

10 Power spectra for temperature and O 2 /Ar similar at low frequency, but differ at high frequency Power Spectra

11 PDF=power density function Temperature and O 2 /Ar differ at scales close to 4 km, similar at scales >10 km Scales of Variability

12 PDF=power density function Temperature and O 2 /Ar differ at scales close to 4 km, similar at scales >10 km Scales of Variability

13 Similar variability between NCP and physics Kurtosis -- at scales ranging from 8 to 50 km -- shows similar variability of temperature and O 2 /Ar (and thus NCP) Suggests that processes are related  physics is “priming the pump” for biology But to examine link, really need Process Studies!

14 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

15 GPP and NPP “STP” cruise GPP and NPP similar pattern GPP/NPP ratio equals 3 to 5 BUT there are differences  autotrophic respiration (R A ), Mehler reaction, or photo- respiration NPP=GPP-R A

16 GPP, NPP and NCP Do I want any text? NCP=GPP-R A -R H

17 Energy Flow Diagrams Diagrams drawn to scale Differences in regions: total amount of energy & its distribution between boxes Caveats: measurement uncertainty, VGPM  NPP

18 NCP can be measured continuously from underway system from O 2 /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

19 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

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