1 / 18

Quantifying the Mechanisms Governing Interannual Variability in Air-sea CO 2 Flux

Study on factors influencing CO2 flux using ocean hindcast simulations from 1958-2004, focusing on wind, temperature, alkalinity, freshwater, and biology interactions. Results show regional effects and non-linear dust-climate interactions.

ldoggett
Download Presentation

Quantifying the Mechanisms Governing Interannual Variability in Air-sea CO 2 Flux

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Quantifying the Mechanisms Governing Interannual Variability in Air-sea CO2 Flux S. Doney & Ivan Lima (WHOI), K. Lindsay & N. Mahowald (NCAR), K. Moore (UCI) & Matt Maltrud (LANL) Global Ocean Hindcast Simulations (1958-2004) -Upper ocean multi-functional group, multi-nutrient ecosystem model (Moore et al., 2004) -Coupled to full-depth ocean BGC model (CCSM-POP) -Surface forcing (1957-2004) from NCEP reanalysis and satellite products -Fixed pre-industrial atmospheric CO2 (~280 ppm) & transient anthropogenic CO2 simulations

  2. Winds, Heat & Freshwater Fluxes Dust/iron CO2 O2 Light Net Community Prod. Circulation Regenerated Prod. Winter mixed layer Nutrient/ DIC Supply Export Remineralization Physical & Biological Controls pCO2 = f(Temp., Salinity, DIC, Alkalinity) + (+) +- Biology only one factor on surface pCO2 & air-sea CO2 flux;

  3. Ocean Model Hindcast (1957-2004)

  4. Factors driving interannual pCO2 anomalies: Wind Speed

  5. 1:1 nDIC Temp Alk Freshwater W. Eq. Pacific

  6. Dissolved Inorganic Carbon Regression of surface pCO2 anomalies on forcing terms ~1 driving term 0 minor term <0 compensating term Masked in areas of low pCO2’ and low correlation Temperature

  7. Alkalinity Regression of surface pCO2 anomalies on forcing terms ~1 driving term 0 minor term <0 compensating term Masked in areas of low pCO2’ and low correlation Freshwater

  8. Annual inventory change & flux anomalies X’: I/t = Q’ srf. flux + A’ horz. advection + E’ eddies + V’ vert. adv. + P’ net comm. prod. + other Q’ 0 A’ E’ I 100 P’ V’

  9. Physics Only Dust Only Dust Only Physics Only

  10. SeaWiFS Dust r=0.82 Physics r=0.11 Dust & Physics r=0.48 Smoothed w/ annual filter

  11. Monthly Annual

  12. -Models as tools for identifying ocean biogeochemical mechanisms • -Regional partitioning of factors driving air-sea CO2 flux • Southern Ocean wind speed variability • Subtropics thermal • Tropics/high latitude biology and circulation on nDIC • Tropical Indo-Pacific freshwater • -Non-linear interactions of dust and climate variability

  13. Model Obs Is low dust deposition downwind of Australia in 1997/1998 realistic? Tentative answer: yes Chen et al. precip slightly above average for 1997 and 1998 Low dep due to low source Two met stations close to source area: 946720 and 944820 have fewer dust events than average in 1997 and 1998 Low dep due to high precip All values are anomalies from climatological mean (1979-2004): black monthly: Yellow line: 0: blue line: annual mean

  14. Physics r=0.56 SeaWiFS Dust r=0.71 Dust & Physics r=0.60 Monthly anomalies

More Related