Abstract
We have developed a new observational screening technique for inverse model. This technique was applied to our transport models with re-analysed meteorological data and the inverse model to estimate the global distribution of CO{sub 2} concentrations and fluxes. During the 1990s, we estimated a total CO{sub 2} uptake by the biosphere of 1.4-1.5 PgC yr-1 and a total CO{sub 2} uptake by the oceans of 1.7-1.8 PgC yr-1. The uncertainty of global CO{sub 2} flux estimation is about 0.3 PgC yr-1. We also obtained monthly surface CO{sub 2} concentrations in the marine boundary layer to precisions of 0.5-1.0 ppm. To utilize non-processed (statistical monthly mean) observational data in our analysis, we developed a quality control procedure for such observational data including a repetition of inversion. This technique is suitable for other inversion setups. Observational data by ships were placed into grids and used in our analysis to add to the available data from fixed stations. The estimated global distributions are updated and extended every year
Maki, T. (Atmospheric Environment and Applied Meteorology Research Dept., Meteorological Research Institute, Japan Meteorological Agency (Japan)), e-mail: tmaki@mri-jma.go.jp;
Fujita, T;
Hirahara, T;
Yamada, K;
Suda, K;
[1]
Mori, K;
[2]
Takeuchi, A;
[3]
Tsutsumi, Y;
[4]
Conway, T J
[5]
- Global Environment and Marine Dept., Japan Meteorological Agency (Japan)
- Kobe Marine Observatory, Japan Meteorological Agency (Japan)
- Meteorological Satellite Center, Japan Meteorological Agency (Japan)
- Mito Local Meteorological Observatory, Japan Meteorological Agency (Japan)
- Global Monitoring Division, Earth System Research Laboratory, National Oceanic and Atmospheric Administration (United States)
Citation Formats
Maki, T. (Atmospheric Environment and Applied Meteorology Research Dept., Meteorological Research Institute, Japan Meteorological Agency (Japan)), e-mail: tmaki@mri-jma.go.jp, Fujita, T, Hirahara, T, Yamada, K, Suda, K, Mori, K, Takeuchi, A, Tsutsumi, Y, and Conway, T J.
New technique to analyse global distributions of CO{sub 2} concentrations and fluxes from non-processed observational data.
Sweden: N. p.,
2010.
Web.
doi:10.1111/J.1600-0889.2010.00488.X.
Maki, T. (Atmospheric Environment and Applied Meteorology Research Dept., Meteorological Research Institute, Japan Meteorological Agency (Japan)), e-mail: tmaki@mri-jma.go.jp, Fujita, T, Hirahara, T, Yamada, K, Suda, K, Mori, K, Takeuchi, A, Tsutsumi, Y, & Conway, T J.
New technique to analyse global distributions of CO{sub 2} concentrations and fluxes from non-processed observational data.
Sweden.
https://doi.org/10.1111/J.1600-0889.2010.00488.X
Maki, T. (Atmospheric Environment and Applied Meteorology Research Dept., Meteorological Research Institute, Japan Meteorological Agency (Japan)), e-mail: tmaki@mri-jma.go.jp, Fujita, T, Hirahara, T, Yamada, K, Suda, K, Mori, K, Takeuchi, A, Tsutsumi, Y, and Conway, T J.
2010.
"New technique to analyse global distributions of CO{sub 2} concentrations and fluxes from non-processed observational data."
Sweden.
https://doi.org/10.1111/J.1600-0889.2010.00488.X.
@misc{etde_1010793,
title = {New technique to analyse global distributions of CO{sub 2} concentrations and fluxes from non-processed observational data}
author = {Maki, T. (Atmospheric Environment and Applied Meteorology Research Dept., Meteorological Research Institute, Japan Meteorological Agency (Japan)), e-mail: tmaki@mri-jma.go.jp, Fujita, T, Hirahara, T, Yamada, K, Suda, K, Mori, K, Takeuchi, A, Tsutsumi, Y, and Conway, T J}
abstractNote = {We have developed a new observational screening technique for inverse model. This technique was applied to our transport models with re-analysed meteorological data and the inverse model to estimate the global distribution of CO{sub 2} concentrations and fluxes. During the 1990s, we estimated a total CO{sub 2} uptake by the biosphere of 1.4-1.5 PgC yr-1 and a total CO{sub 2} uptake by the oceans of 1.7-1.8 PgC yr-1. The uncertainty of global CO{sub 2} flux estimation is about 0.3 PgC yr-1. We also obtained monthly surface CO{sub 2} concentrations in the marine boundary layer to precisions of 0.5-1.0 ppm. To utilize non-processed (statistical monthly mean) observational data in our analysis, we developed a quality control procedure for such observational data including a repetition of inversion. This technique is suitable for other inversion setups. Observational data by ships were placed into grids and used in our analysis to add to the available data from fixed stations. The estimated global distributions are updated and extended every year}
doi = {10.1111/J.1600-0889.2010.00488.X}
journal = []
issue = {5}
volume = {62B}
place = {Sweden}
year = {2010}
month = {Nov}
}
title = {New technique to analyse global distributions of CO{sub 2} concentrations and fluxes from non-processed observational data}
author = {Maki, T. (Atmospheric Environment and Applied Meteorology Research Dept., Meteorological Research Institute, Japan Meteorological Agency (Japan)), e-mail: tmaki@mri-jma.go.jp, Fujita, T, Hirahara, T, Yamada, K, Suda, K, Mori, K, Takeuchi, A, Tsutsumi, Y, and Conway, T J}
abstractNote = {We have developed a new observational screening technique for inverse model. This technique was applied to our transport models with re-analysed meteorological data and the inverse model to estimate the global distribution of CO{sub 2} concentrations and fluxes. During the 1990s, we estimated a total CO{sub 2} uptake by the biosphere of 1.4-1.5 PgC yr-1 and a total CO{sub 2} uptake by the oceans of 1.7-1.8 PgC yr-1. The uncertainty of global CO{sub 2} flux estimation is about 0.3 PgC yr-1. We also obtained monthly surface CO{sub 2} concentrations in the marine boundary layer to precisions of 0.5-1.0 ppm. To utilize non-processed (statistical monthly mean) observational data in our analysis, we developed a quality control procedure for such observational data including a repetition of inversion. This technique is suitable for other inversion setups. Observational data by ships were placed into grids and used in our analysis to add to the available data from fixed stations. The estimated global distributions are updated and extended every year}
doi = {10.1111/J.1600-0889.2010.00488.X}
journal = []
issue = {5}
volume = {62B}
place = {Sweden}
year = {2010}
month = {Nov}
}