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中国南极科学考察第24航次大气CO_2遥感算法及其在第26航次中的应用分析

ATMOSPHERIC CO_2 ALGORITHM BASED ON THE 24TH CRUISE OF CHINARE AND ITS APPLICATION TO THE 26TH CRUISE
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摘要 利用中国南极科学考察第24航次采集的大气CO2浓度与AIRS的大气红外辐亮度进行统计回归,获取两者间的拟合关系。与该航次随机选取的60°S附近验证点比较,平均相对偏差为1.09%。同时,将拟合函数应用于对应第26航次同位置、近时间点的AIRS大气辐射值,其结果和第26航次走航数据进行比对,平均相对偏差为2.12%。对比同纬度下第24航次的精度,其精度有明显的下降,结果表明,利用统计回归的计算方式具有一定的局限性。 An algorithm was constructed by statistical regression using along-track atmospheric CO2 data collected during the 24th Chinese National Antarctic Research Expedition ( CHINARE ; Chinese National Arctic and Antarctic Administration) and Atmospheric Infrared Sounder (AIRS) radiance. Verification points around latitude 60° S were used, and the average error was 1.09%. AIRS radiance data with locations and times near those of the 26th CHIN- ARE cruise were input to the algorithm. Average error was 2.12%. It is demonstrated that the algorithm based on regression statistics has some limitations.
出处 《极地研究》 CAS CSCD 北大核心 2013年第3期278-283,共6页 Chinese Journal of Polar Research
基金 卫星海洋环境动力学国家重点实验室开放研究基金(SOED1204) 海洋赤潮灾害立体监测技术与应用国家海洋局重点实验室开放研究基金资助课题(MATHAB200903) 国家海洋局青年基金(2012443) 国家海洋局第三海洋研究所基本科研业务费资助项目(海三科2009048) 国家自然科学基金重点项目:"南大洋N2O源汇格局:驱动机制及其对海洋N2O收支的影响"(41230529) 国家高技术研究发展计划(863计划)计划重大项目极区大气环境遥感监测技术(2008AA121703) 国家海洋局极地考察办公室对外合作支持项目(IC2010013 IC2011114 IC201201) 国家极地专项"南北极环境综合考察与评估"资助
关键词 南大洋 二氧化碳 统计回归 大气红外探测器 中国南极科学考察 Southern Ocean, carbon dioxide, statistical regression, atmospheric infrared sounder, Chinese Ant-arctic Scientific Expedition
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参考文献14

  • 1IPCC,Climate Change 2007. The Physical Science Basis. Cambridge : Cambridge University Press, 2007.
  • 2Metzl N, Brunet C, Jabaud-Jan A, et al. Summer and winter air-sea C02 fluxes in the Southern Ocean. Deep-Sea Research Part I,2006, 53(9):1548-1563.
  • 3Chen L Q, Xu S Q, Gao Z Y, et al. Estimation of monthly air-sea C02 flux in the Southern atlantic and Indian Ocean using In-situ and remotelysensed data. Remote Sensing of Environment, 2011,115(8) : 1935-1941, doi:10. 1016/j. rse. 2011.03.016.
  • 4Chahine M T, Bamet C, Olsen E T, et al. On the determination of atmospheric minor gases by the method of vanishing partialderivatives with appli-cation to C02. Geophysical Research Letters, 2005 , 32(22) , L22803 , doi:10. 1029/2005GL024165.
  • 5Buchwitz M, Rozanov V V,Burrows J P. A near-infrared optimized DOAS method for the fast global retrieval of atmospheric CH4,CO, C02 , H20,and N20 total column amounts from SCIAMACHY Envisat-1 nadir radiances. Journal of Geophysical Research, 2000,105 ( D12) : 15231-15245.
  • 6Buchwitz M,de Beek R, Burrows J P, et al. Atmospheric methane and carbon dioxide from SCIAMACHY satellite data: initial comparison withchemistry and transport model. Atmospheric Chemistry Physics, 2005 , 5:941-962.
  • 7Barkley M P,Monks P S,Engelen R J. Comparison of SCIAMACHY and AIRS measurement over North America during the summer and autumn of2003. Geophysical Research Letters, 2006, 33 (22),L20805 , doi : 10. 1029/2006GL026807.
  • 8Yokota T, Yoshida Y, Eguchi N, et al. Global concentrations of C02 and CH4 retrieved from GOSAT : First preliminary results. Scientific OnlineLetters on the Atmosphere, 2009,5 : 160-163.
  • 9Hungershoefer K, Breon F M, Peylin P, et al. Evaluation of various observing systems for the global monitoring of C02 surface fluxes. AtmosphericChemistry and Physics, 2010, 10(21) : 10503-10520, doi: 10. 5194/acp-10-10503-2010.
  • 10National Institute for Environmental Studies. Public Release of Concentration Data ( Carbon Dioxide and Methane) Analyzed from GOSAT Observa-tional Data, 2010.

二级参考文献31

  • 1张华,石广玉,刘毅.两种逐线积分辐射模式大气吸收的比较研究[J].大气科学,2005,29(4):581-593. 被引量:18
  • 2程洁,柳钦火,李小文.星载高光谱红外传感器反演大气痕量气体综述[J].遥感信息,2007,29(2):90-97. 被引量:12
  • 3[1]IPCC.Climate Change 2007:The Physical Science Basis[M].Cambridge:Cambridge University Press,2007.
  • 4[2]Engelen R J,Denning A,Gurney K R,et al.Global observations of the carbon budget 1.Expected satellite capabilities for emission spectroscopy in the EOS and NPOESS eras[J].J Geophys Res,2001,106(D17):20055-20068.
  • 5[3]CMDL.See the NOAA Earth System Research Laboratory(ESRL) cooperative sampling network sites[EB/OL].[2007-11-15].http://www.esrl.noaa.gov/gmd/,2007.
  • 6[4]Fan S,Gloor M,Mahlman J,et al.A large terrestrial carbon sink in North America implied by atmospheric and oceanic carbon dioxide data and models[J].Science,1998,282:442-446.
  • 7[7]Rodgers C.Inverse Methods for Atmospheric Sounding:Theory and Practice[M].Singapore:World Scientific,2000.
  • 8[8]Cheruy F,Scott N A,Armante R,et al.Contribution to the development of radiative transfer models for high spectral resolution observations in the infrared[J].J Quant Spectrosc Radiat Transfer,1995,53(6):597-611.
  • 9[9]Liou K N.大气辐射导论[M].2版.北京:气象出版社,2004.
  • 10[12]Lacis A A,Oinas V.A description of the correlated k distribution method for modeling nongray gaseous absorption thermal emission and multiple scattering in vertically inhomogeneous atmospheres[J].J Geophys Res,1991,96(D5):9027-9063.

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