大气科学学报
大氣科學學報
대기과학학보
JOURNAL OF NANJING INSTITUTE OF METEOROLOGY
2009年
5期
595-603
,共9页
银燕%崔振雷%张华%辛金元%王莉莉
銀燕%崔振雷%張華%辛金元%王莉莉
은연%최진뢰%장화%신금원%왕리리
硫酸盐%黑碳%沙尘%CSHNET观测网%气溶胶光学厚度%大气化学传输模式%浓度分布
硫痠鹽%黑碳%沙塵%CSHNET觀測網%氣溶膠光學厚度%大氣化學傳輸模式%濃度分佈
류산염%흑탄%사진%CSHNET관측망%기용효광학후도%대기화학전수모식%농도분포
sulfate%black carbon%soil dust%CSHNET%AOD%concentration distribution%MATCH
结合2006年最新的气溶胶排放源资料,以NCEP/NCAR再分析资料为气象场,驱动大气化学传输模式MATCH(Model of Atmospheric Transport and Chemistry),模拟了2006年中国地区硫酸盐、黑碳和沙尘气溶胶的质量浓度分布及其季节变化.模拟的气溶胶光学厚度(AOD)结果与CSHNET观测网数据比较分析后发现,基于21个观测站的61组月平均数据与相应模拟结果的相关系数为0.63.模拟结果表明:2006年中国地区硫酸盐气溶胶高值区主要分布在中国的四川盆_地、华北及长江流域等工业较发达地区,而且具有明显的季节变化,四川盆地及长江以南地区.硫酸盐气溶胶1月份浓度高于7月份,长江以北的大部分地区,7月份浓度高于1月份;黑碳气溶胶主要分布在黄河、长江中下游地区及华南等地区,1月份浓度高于7月份;沙尘气溶胶主要分布在内蒙古中部沙漠地区,4月份浓度最高,7月份次之,其他月份较少.
結閤2006年最新的氣溶膠排放源資料,以NCEP/NCAR再分析資料為氣象場,驅動大氣化學傳輸模式MATCH(Model of Atmospheric Transport and Chemistry),模擬瞭2006年中國地區硫痠鹽、黑碳和沙塵氣溶膠的質量濃度分佈及其季節變化.模擬的氣溶膠光學厚度(AOD)結果與CSHNET觀測網數據比較分析後髮現,基于21箇觀測站的61組月平均數據與相應模擬結果的相關繫數為0.63.模擬結果錶明:2006年中國地區硫痠鹽氣溶膠高值區主要分佈在中國的四川盆_地、華北及長江流域等工業較髮達地區,而且具有明顯的季節變化,四川盆地及長江以南地區.硫痠鹽氣溶膠1月份濃度高于7月份,長江以北的大部分地區,7月份濃度高于1月份;黑碳氣溶膠主要分佈在黃河、長江中下遊地區及華南等地區,1月份濃度高于7月份;沙塵氣溶膠主要分佈在內矇古中部沙漠地區,4月份濃度最高,7月份次之,其他月份較少.
결합2006년최신적기용효배방원자료,이NCEP/NCAR재분석자료위기상장,구동대기화학전수모식MATCH(Model of Atmospheric Transport and Chemistry),모의료2006년중국지구류산염、흑탄화사진기용효적질량농도분포급기계절변화.모의적기용효광학후도(AOD)결과여CSHNET관측망수거비교분석후발현,기우21개관측참적61조월평균수거여상응모의결과적상관계수위0.63.모의결과표명:2006년중국지구류산염기용효고치구주요분포재중국적사천분_지、화북급장강류역등공업교발체지구,이차구유명현적계절변화,사천분지급장강이남지구.류산염기용효1월빈농도고우7월빈,장강이북적대부분지구,7월빈농도고우1월빈;흑탄기용효주요분포재황하、장강중하유지구급화남등지구,1월빈농도고우7월빈;사진기용효주요분포재내몽고중부사막지구,4월빈농도최고,7월빈차지,기타월빈교소.
The Model of Atmospheric Transport and Chemistry(MATCH)is used to simulate the distri-bution and seasonal variation of aerosols over China in 2006,by taking the latest source emission data and NCEP/NCAR reanalysis data as its initial conditions. The aerosol optical depth (AOD) obtained by MATCH is compared wim the CSHNET(the Chinese Sun Hazemeter Network)observational data.The =0.000 1).The results indicate that the high concentrations of sulfate are mainly located in Sichuan Basin,North China and the middle and lower reaches of the Yangtze River,and that sulfate loading is higher in July than in January in the north part of China and is opposite in the south part of China.The results also show that higher concentrations of black carbon aerosol appear in the middle and lower tea-ches of the Yangtze River and the Yellow River and the maximum values are higher in January than in July. The center with high concentration of dust aerosol is located in Inner Mongolia of China.The highest concentration of dust aerosols appears in April, with the secondary maximum value in July.