New technique to analyse global distributions of CO2 concentrations and fluxes from non-processed observational data

被引:37
作者
Maki, T. [1 ]
Ikegami, M. [2 ]
Fujita, T. [2 ]
Hirahara, T. [2 ]
Yamada, K. [2 ]
Mori, K. [3 ]
Takeuchi, A. [4 ]
Tsutsumi, Y. [5 ]
Suda, K. [2 ]
Conway, T. J.
机构
[1] Japan Meteorol Agcy, Meteorol Res Inst, Atmospher Environm & Appl Meteorol Res Dept, Tokyo, Japan
[2] Japan Meteorol Agcy, Global Environm & Marine Dept, Tokyo, Japan
[3] Japan Meteorol Agcy, Kobe Marine Observ, Tokyo, Japan
[4] Japan Meteorol Agcy, Meteorol Satellite Ctr, Tokyo, Japan
[5] Japan Meteorol Agcy, Mito Local Meteorol Observ, Tokyo, Japan
来源
TELLUS SERIES B-CHEMICAL AND PHYSICAL METEOROLOGY | 2010年 / 62卷 / 05期
基金
美国国家科学基金会; 美国海洋和大气管理局;
关键词
CARBON-DIOXIDE; ATMOSPHERIC CO2; STATION; TRANSPORT; NORTHERN; EXCHANGE; SCALE; SINKS; CYCLE;
D O I
10.1111/j.1600-0889.2010.00488.x
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
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 CO2 concentrations and fluxes. During the 1990s, we estimated a total CO2 uptake by the biosphere of 1.4-1.5 PgC yr-1 and a total CO2 uptake by the oceans of 1.7-1.8 PgC yr-1. The uncertainty of global CO2 flux estimation is about 0.3 PgC yr-1. We also obtained monthly surface CO2 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.
引用
收藏
页码:797 / 809
页数:13
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