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Nature Doesn’t Yield Her Secrets Easily Mark Battle (Bowdoin College) Michael Bender (Princeton) Ralph Keeling (Scripps Institute of Oceanography) Pieter Tans (NOAA/CMDL) Jesse Bastide, Carrie Simonds, Blake Sturtevant, Becca Perry EdFest Rochester 8/7/2004 Funding from: NSF, EPA, NOAA GCRP, BP-Amoco, Bowdoin College
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Organizing Principle: 1 topic superficially
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Organizing Principle: 1 topic superficially Many topics with vanishing content
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1988-1994: PhD in HEP experiment 1994-1997: Post Doc. at URI-GSO (Oceanography) 1997-1999: Research Scientist at Princeton (Geosciences) 2000 - ? : Asst. Prof. Bowdoin College (Physics) My tortuous path
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Where does anthropogenic CO 2 end up?
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Measurements of O 2 and CO 2 O2 = Land biota + Industry CO2 = Land biota + Industry + Ocean
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Measurements of O 2 and CO 2 real time collections
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The Princeton cooperative flask sampling network
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Ships of opportunity
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Automated sample collection systems
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O 2 /N 2 changes are small O 2 /N 2 per meg (O 2 /N 2sa – O 2 /N 2st )/(O 2 /N 2st ) x10 6 1 per meg = 0.0001% 1 GtC from FF 3.2 per meg O2/N2
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1991 – 1997 Land sink = 1.4 ± 0.8 GtC/yr Ocean sink = 2.0 ± 0.6 GtC/yr Battle et al. Science 2000 (2467-2470)
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Measurements of O 2 and CO 2 real time collections average land/ocean carbon partition 1991 present
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Measurements of O 2 and CO 2 O2 = Land biota + Industry CO2 = Land biota + Industry + Ocean
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Measurements of O 2 and CO 2 O2 = Land biota + Industry CO2 = Land biota + Industry + Ocean
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Measurements of O 2 and CO 2 O2 = Land biota + Industry CO2 = Land biota + Industry + Ocean
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Determining the O 2 :CO 2 stoichiometry for the land biota
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Measurements of O 2 and CO 2 real time collections air archives average land/ocean carbon partition 1991 present measure land O 2 :CO 2 stoichiometry
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Firn (snowpack) as an air archive Ice Surface Firn ~120m
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Influences of firn air composition Overlying atmosphere (Fick’s laws)
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Influences of firn air composition Overlying atmosphere (Fick’s laws) Selective exclusion at bubble close-off (Knudsen regime) Gravitational settling (barometric equation) Thermal fractionation (kinetic theory) Wind pumping/bulk flow (Bernard convection?)
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The forward problem… 1.Posit an atmospheric history 2.Use the history to drive the model forward in time 3.Compare model predictions with observations
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The inverse problem… 1.Start with a set of observations 2.What atmospheric history led to those data?
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The mechanistic inverse problem… 1.Start with a set of observations 2.What atmospheric history led to those data? Trial history (land sink) + (fossil source)+ (exclusion flux) Battle et al., Nature 1996 (231-235) Land sink: 0.4 ± 0.4 GtC/yr for 1977-1985
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The phenomenological inverse problem… 1.Start with a set of observations 2.What atmospheric history led to those data? Trial history f t Montzka et al., Geophys. Res. Lett., In press
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Measurements of O 2 and CO 2 real time collections air archives average land/ocean carbon partition 1991 present average land/ocean carbon partition 1977 1985 histories of other species ~1900 present measure land O 2 :CO 2 stoichiometry
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Full circle… Bowdoin teaching: Physics of the Environment (Physics 81): Spring '02, ‘05 Introductory Physics I (Physics 103): Fall, '02 Introductory Physics II (Physics 104): Spring '01, Fall '01 E & M Laboratory (Physics 223L): Fall ‘04 Statistical Mechanics (Physics 229): Spring '00, '01, '02, '03, ‘05 Acoustics (Physics 250): Fall '00 Physical Oceanography (Physics 255): Fall '00, '02 Atmospheric Physics (Physics 256): Fall '01, Fall ‘04 Physics of Particles and Nuclei (Physics 280): Spring '03
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