314
Air Pollution and Turbulence: Modeling and Applications
P. D. Quay, B. Tilbrook, and C. S. Wong. Oceanic uptake of fossil fuel CO 2 : Carbon-13 evidence. Science, 256:74–79, 1992.
J. T. Randerson, I. G. Enting, E.A.G. Schuur, K. Caldeira, and I. Y. Fung. Seasonal and latitudinal variability of tropospheric Δ 14 CO 2 : Post bomb contributions from fossil fuels,
oceans and the stratosphere, and the terrestrial biosphere. Glob. Biogeochem. Cycles,
16:1112, doi:10:1029/2002GB001876, 2002.
M. R. Raupach, P. J. Rayner, D. J. Barrett, R. S. DeFries, M. Heimann, D. S. Ojima, S. Quegan,
and C. C. Schmullius. Model-data synthesis in terrestrial carbon observation: Methods,
data requirements and data uncertainty specifi cations. Glob. Change Biol., 11:378–397,
2005, doi:10.1111/j.1365–2486.2005.00917.x.
P. J. Rayner. Flying leap becomes C4MIP. Res. GAIM, 4:2 (winter 2001):8, 2001.
P. J. Rayner. Optimizing CO 2 observing networks in the presence of model error: Results from
TransCom 3. Atmos. Chem. Phys., 4:413–421, 2004.
P. J. Rayner and R. M. Law. A comparison of modelled responses to prescribed CO 2 sources.
CRC-SHM Technical Paper no. 1, 1995 (and CSIRO Division of Atmospheric Research
Technical Paper no. 36) (CSIRO: Australia).
P. J. Rayner and D. O’Brien. The utility of remotely sensed CO 2 concentration data in surface
source inversions. Geophys. Res. Lett., 28:175–178, 2001a.
P. J. Rayner and D. M. O’Brien. Correction to ‘The utility of remotely sensed CO 2 concentration data in surface source inversions’. Geophys. Res. Lett., 28:2429, 2001b.
P. J. Rayner, I. G. Enting, and C. M. Trudinger. Optimizing the CO 2 observing network for
constraining sources and sinks. Tellus, 48B:433–444, 1996.
P. J. Rayner, I. G. Enting, R. J. Francey, and R. Langenfelds. Reconstructing the recent carbon cycle from atmospheric CO 2 , δ 13 C and O 2 /N 2 observations. Tellus, 51B:213–232,
1999a.
P. J. Rayner, R. M. Law, and R. Dargaville. The relationship between tropical CO 2 fl uxes and
the El Niño-Southern Oscillation. Geophys. Res. Lett., 26:493–496, 1999b.
P. J. Rayner, M. Scholze, W. Knorr, T. Kaminski, R. Giering, and H. Widmann. Two decades of
terrestrial carbon fl uxes from a carbon cycle data assimilation system (CCDAS). Glob.
Biogeochem. Cycles, 19:GB2026, 2005, doi: 10.1029/2004GB002254.
J. E. Robertson and A. J. Watson. Thermal skin effect on the surface ocean and its implications
for CO 2 uptake. Nature, 358:738–740, 1992.
C. Rödenbeck, S. Houwerling, M. Gloor, and M. Heimann. CO 2 fl ux history 1982–2001
inferred from atmospheric data using a global inversion of atmospheric transport. Atmos
Chem. Phys. Discuss., 3:2575–2659, 2003.
T. Roy, P. Rayner, R. Matear, and R. Francey. Southern hemisphere ocean CO 2 uptake:
Reconciling atmospheric and oceanic estimates. Tellus, 55B:701–710, 2003.
J. L. Sarmiento and E. T. Sundquist. Revised budget for the oceanic uptake of anthropogenic
carbon dioxide. Nature, 356:589–593, 1992.
B. A. Shaby and C. B. Field. Regression tools for CO 2 inversions: Application of a shrinkage
estimator to process attribution. Tellus, 58B:279–292, 2006.
U. Siegenthaler and H. Oeschger. Biospheric CO 2 emissions during the past 200 years reconstructed by deconvolution of ice core data. Tellus, 39B:140–154, 1987.
P. Suntharalingam, J. T. Randerson, N. Krakaeur, D. J. Jacob, and J. A. Logan. Infl uence
of reduced carbon emissions and oxidation on the distribution of atmospheric CO 2 :
Implications for inversion analyses. Glob. Biogeochem. Cycles, 19:GB4003, 2005,
doi:10.1029/2005GB002493.
P. P. Tans, T. J. Conway, and T. Nakazawa. Latitudinal distribution of the sources and sinks
of atmospheric carbon dioxide derived from surface observations and an atmospheric
transport model. J. Geophys. Res., 94D:5151–5172, 1989.
P. P. Tans, I. Y. Fung, and T. Takahashi. Observational constraints on the global atmospheric
CO 2 budget. Science, 247:1431–1438, 1990.
© 2010 by Taylor and Francis Group, LLC
Air Pollution and Turbulence: Modeling and Applications
P. D. Quay, B. Tilbrook, and C. S. Wong. Oceanic uptake of fossil fuel CO 2 : Carbon-13 evidence. Science, 256:74–79, 1992.
J. T. Randerson, I. G. Enting, E.A.G. Schuur, K. Caldeira, and I. Y. Fung. Seasonal and latitudinal variability of tropospheric Δ 14 CO 2 : Post bomb contributions from fossil fuels,
oceans and the stratosphere, and the terrestrial biosphere. Glob. Biogeochem. Cycles,
16:1112, doi:10:1029/2002GB001876, 2002.
M. R. Raupach, P. J. Rayner, D. J. Barrett, R. S. DeFries, M. Heimann, D. S. Ojima, S. Quegan,
and C. C. Schmullius. Model-data synthesis in terrestrial carbon observation: Methods,
data requirements and data uncertainty specifi cations. Glob. Change Biol., 11:378–397,
2005, doi:10.1111/j.1365–2486.2005.00917.x.
P. J. Rayner. Flying leap becomes C4MIP. Res. GAIM, 4:2 (winter 2001):8, 2001.
P. J. Rayner. Optimizing CO 2 observing networks in the presence of model error: Results from
TransCom 3. Atmos. Chem. Phys., 4:413–421, 2004.
P. J. Rayner and R. M. Law. A comparison of modelled responses to prescribed CO 2 sources.
CRC-SHM Technical Paper no. 1, 1995 (and CSIRO Division of Atmospheric Research
Technical Paper no. 36) (CSIRO: Australia).
P. J. Rayner and D. O’Brien. The utility of remotely sensed CO 2 concentration data in surface
source inversions. Geophys. Res. Lett., 28:175–178, 2001a.
P. J. Rayner and D. M. O’Brien. Correction to ‘The utility of remotely sensed CO 2 concentration data in surface source inversions’. Geophys. Res. Lett., 28:2429, 2001b.
P. J. Rayner, I. G. Enting, and C. M. Trudinger. Optimizing the CO 2 observing network for
constraining sources and sinks. Tellus, 48B:433–444, 1996.
P. J. Rayner, I. G. Enting, R. J. Francey, and R. Langenfelds. Reconstructing the recent carbon cycle from atmospheric CO 2 , δ 13 C and O 2 /N 2 observations. Tellus, 51B:213–232,
1999a.
P. J. Rayner, R. M. Law, and R. Dargaville. The relationship between tropical CO 2 fl uxes and
the El Niño-Southern Oscillation. Geophys. Res. Lett., 26:493–496, 1999b.
P. J. Rayner, M. Scholze, W. Knorr, T. Kaminski, R. Giering, and H. Widmann. Two decades of
terrestrial carbon fl uxes from a carbon cycle data assimilation system (CCDAS). Glob.
Biogeochem. Cycles, 19:GB2026, 2005, doi: 10.1029/2004GB002254.
J. E. Robertson and A. J. Watson. Thermal skin effect on the surface ocean and its implications
for CO 2 uptake. Nature, 358:738–740, 1992.
C. Rödenbeck, S. Houwerling, M. Gloor, and M. Heimann. CO 2 fl ux history 1982–2001
inferred from atmospheric data using a global inversion of atmospheric transport. Atmos
Chem. Phys. Discuss., 3:2575–2659, 2003.
T. Roy, P. Rayner, R. Matear, and R. Francey. Southern hemisphere ocean CO 2 uptake:
Reconciling atmospheric and oceanic estimates. Tellus, 55B:701–710, 2003.
J. L. Sarmiento and E. T. Sundquist. Revised budget for the oceanic uptake of anthropogenic
carbon dioxide. Nature, 356:589–593, 1992.
B. A. Shaby and C. B. Field. Regression tools for CO 2 inversions: Application of a shrinkage
estimator to process attribution. Tellus, 58B:279–292, 2006.
U. Siegenthaler and H. Oeschger. Biospheric CO 2 emissions during the past 200 years reconstructed by deconvolution of ice core data. Tellus, 39B:140–154, 1987.
P. Suntharalingam, J. T. Randerson, N. Krakaeur, D. J. Jacob, and J. A. Logan. Infl uence
of reduced carbon emissions and oxidation on the distribution of atmospheric CO 2 :
Implications for inversion analyses. Glob. Biogeochem. Cycles, 19:GB4003, 2005,
doi:10.1029/2005GB002493.
P. P. Tans, T. J. Conway, and T. Nakazawa. Latitudinal distribution of the sources and sinks
of atmospheric carbon dioxide derived from surface observations and an atmospheric
transport model. J. Geophys. Res., 94D:5151–5172, 1989.
P. P. Tans, I. Y. Fung, and T. Takahashi. Observational constraints on the global atmospheric
CO 2 budget. Science, 247:1431–1438, 1990.
© 2010 by Taylor and Francis Group, LLC