Meso-scale mapping of terrestrial carbon dioxide source/sink intensity using inverse analysis of atmospheric concentration change by GA
Meso-scale mapping of terrestrial carbon dioxide source/sink intensity using inverse analysis of atmospheric concentration change by GA
批准号:
15380180
负责人:
MACHIMURA Takashi
金额:
$5.82万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (B)
财政年份:
2003
资助国家:
日本
项目状态:
已结题
起止时间:
2003 至 2005
中文摘要
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英文摘要
This study aimed to develop a new technique mapping terrestrial carbon dioxide source/sink intensity using an inverse model. The technique consists of the continuous atmospheric carbon dioxide concentration at one observatory, the wind field and gas diffusion simulation using a meso-scale meteorological model and the inverse analysis of source/sink intensity distribution using the genetic algorithm (GA). An atmosphere sampling system including an IRGA and an automated calibration system was developed and carbon dioxide concentration was measured continuously between December 2004 and January 2006 at Suita, Osaka. Before applying the new technique to real problems, a numerical simulation of the virtual source/sink distribution was examined in order to validate performance of the inverse analysis using GA. 4 or 16 fixed source/sinks were placed randomly in a target area of 126 km x 126 km and atmospheric concentration at a observatory was calculated using the meso-scale meteorological mo … More del (MM5) and the meso-scale objective analysis data. The inverse model using GA was capable to estimate the given source/sink distribution from calculated time series of the atmospheric concentration excepting a few parts of which source/sink had little influence on atmospheric concentration at the observatory. This suggested that the source/sink intensity of land use categories but its spatial distribution is more adequate as the problem to be solved. Therefore, the source sink intensity of each land use was estimated in the real problems. Carbon dioxide source intensity was the strongest in urban area among all land use and the vegetated land showed relatively small source both in winter and summer, however the absolute intensities were not accurate. The possible reasons were error in the atmospheric concentration measurement and the inadequate background concentration value. Relative source/sink intensity of the land uses and its seasonal change could be estimated reasonably by the new technique. Less
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