[ 1 ] 王涛,陈广庭,钱正安,等. 中国北方沙尘暴现状及对策 [ J ]. 中国沙漠, 2001, 21 (4) : 322 - 327.
[ 2 ] 王明星,张仁健. 大气气溶胶研究的前沿问题 [ J ]. 气候与环境研究, 2001, 6 (1) : 119 - 124.
[ 3 ] Ridgwell A J. Feedback in the earth system: the biogeochemical linking of land, air and sea [ J ]. IGBP Global Change Newsletter,
2002, 360: 2905 - 2924.
[ 4 ] Martin J H. Glacial - interglacial CO2 change: The iron hypothesis [ J ]. Paleoceanography, 1990, 199 (5) : 1 - 13.
[ 5 ] Duce R A, Unni C K, Ray B J, et al. Long range atmospheric transport of soil dust from Asia to the trop icalNorth Pacific: temporal variability [ J ]. Science, 1980, 209: 1522 - 1524.
[ 6 ] Coale K H, Johnson K S, Fitzwater S E, et al. A massive phytop lankton bloom induced by an ecosystem - scale iron fertilization experiment in the equatorial Pacific Ocean [ J ]. Nature, 1996, 383:495 - 501.
[ 7 ] 方小敏,韩永翔,马金辉,等. 青藏高原沙尘特征与高原黄土堆积———以2003 - 3 - 4拉萨沙尘天气过程为例 [ J ]. 科学通报,2004, 49 (11) : 1084 - 1090.
[ 8 ] 钱云,符淙斌,王淑瑜. 沙尘气溶胶与气候变化 [ J ]. 地球科学进展, 1999, 14 (4) : 391 - 394.
[ 9 ] Li X, Maring H, Savoie D, et al. Dominance of mineral dust in aerosol light scattering in the North Atlantic tradewinds [ J ]. Nature,
1996, 380: 416 - 419.
[ 10 ] Aoki T, Tanaka T Y, Uchiyama A, et al. Sensitivity Experiments of Direct Radiative Forcing Caused byMineral Dust Simulated with a
Chemical TransportModel [ J ]. Journal of theMeteorological Society of Japan, 2005, 83A: 315 - 331.
[ 11 ] Shi G Y, Wang H, Wang B, et al. Sensitivity Experiments on the Effects of Op tical Properties of Dust Aerosols on Their Radiative
Forcing under Clear Sky Condition [ J ]. Journal of theMeteorological Society of Japan, 2005, 83A: 333 - 346.
[ 12 ] 王宏,石广玉, Aoki T, 等. 2001年春季东亚—北太平洋地区沙尘气溶胶的辐射强迫 [ J ]. 科学通报, 2004, 49 ( 19 ) : 1993 -2000.
[ 13 ] Takemura T, Uno I, Nakajima T, et al. Single - Scattering albedo and radiative forcing of various aerosol species with a global Three
- Dimensionalmodel [ J ]. Journal of Climate, 2002, 15 (D4) : 333- 352.
[ 14 ] GunnarM, Grini A, JamesM Haywood, et al . Modeling the radiative impact of mineral dust during the Saharan Dust Experiment
( SHADE) campaign [ J ]. J Geophys Res, 2003, 108 (D18 ) :8579 - 8592.
[ 15 ] Haywood J M, Shine K P. The effect of anthropogenic sulfate and soot aerosol on the clear sky p lanetary radiation budget [ J ]. Geophys Res Lett, 1995, 22: 603 - 606.
[ 16 ] Hansen J, Sato M, Ruedy R. Radiative forcing and climate response [ J ]. J Geophys Res, 1997, 102: 6831 - 6864.
[ 17 ] CarlsonT N, Benjamin S. Radiative heating rates for Saharan dust [ J ]. Atmos Sci, 1980, 37: 193 - 197.
[ 18 ] Tegen I, Lacis A A. The influence on climate forcing of mineral aerosols from disturbed soils [ J ]. Nature, 1996, 380: 419 - 422.
[ 19 ] 孙景群,张海福. 激光遥测大气气溶胶的尺度谱分布 [ J ]. 气象学报, 1982, 40 (4) : 483 - 489.
[ 20 ] 孙景群,张海福. 激光遥测大气尘埃质量浓度的理论分析 [ J ].环境科学学报, 1982, 2 (1) : 36 - 43.
[ 21 ] PapayannisA, BalisD, AmiridisV, et al. Measurements of Saha ran dust aerosols over the EasternMediterranean using elastic backscatter - Raman lidar, spectrophotometric and satellite observations in the frame of the EARL INET p roject [ J ]. Atmos Chem Phys,2005, 5: 2065 - 2079.
[ 22 ] Tao ZM, Zhang Y C, Liu X Q, et al. Iteration method for the inversion of simulated multiwavelength lidar signals to determine
aerosol size distribution [ J ]. Chinese Physics, 2004, 13 ( 3) : 409 -412.
[ 23 ] 陶宗明,张寅超,张改霞. 气溶胶粒子消光效率因子的特性研究及尺度谱的拟合 [ J ]. 量子电子学报, 2004, 21 (1) : 103 - 109.
[ 24 ] Pu Q, Nakane H, Sasano Y, et al. Numerical simulation of the retrieval of aerosol size distribution from multiwavelength laser radar
measurement [ J ]. App lied Op tics, 1989, 28 (24) : 5259 - 5265.
[ 25 ] 辛金元,张文煜,袁九毅,等. 消光法反演腾格里沙漠地区沙尘气溶胶谱分布 [ J ]. 高原气象, 2004, 23 (5) : 654 - 659.
[ 26 ] 刘吉,陈长和. 兰州地区冬季大气气溶胶粒子谱的反演研究 [ J ]. 高原气象, 2004, 23 (1) : 103 - 109.
[ 27 ] Reagan J A, Herman B M. Bistatic lidar investigations of atmospheric aerosols. 14 th RadarMeteorology Conference. AmerMeteor Soc, 1970.
[ 28 ] Herman BM, Browning S R, Reagan J A. Determination of aerosol size distributions from lidar measurements [ J ]. J Atmos Sci, 1971,
28 (5) : 763 - 771.
[ 29 ] Reagan J A. Determination of the comp lex refractive index and size distribution of atmospheric particulates from bistatic - monostatic lidar and solar radiometermeasurements [ J ]. J Geophys Res, 1980,85 (C3) : 1591 - 1599.
[ 30 ] Parameswaran K, Rose KO, MuthyB V K. Aerosol characteristics from bistatic lidar observations [ J ]. J Geophys Res, 1984, 89(D2) : 2541 - 2552.
[ 31 ] 孙景群. 激光探测大气污染 [M ]. 北京:科学出版社, 1992. 101- 107.
[ 32 ] 杜萍. 利用卫星资料反演沙尘气溶胶光学厚度 [D ]. 兰州:兰州大学博士学位论文, 2002, 52 - 58.
[ 33 ] 胡波,张婕,张武,等. 应用积分浑浊度仪研究兰州城市冬季大气气溶胶 [ J ]. 兰州大学学报(自然科学版) , 2005, 41 ( 3) : 19 -25.
[ 34 ] 胡波,张武,张镭,等. 兰州市西固区冬季大气气溶胶粒子的散射特征 [ J ]. 高原气象, 2003, 22 (4) : 354 - 360.
[ 35 ] ZhangW, Hu B, Chen C H, et al. Scattering p roperties of atmospheric aerosols overLanzhou City and app lications using an integrating nephelometer [ J ]. Advances in Atmospheric Sciences, 2004,21 (6) : 848 - 856.
[ 36 ] Yu H , Kaufman Y J, ChinM, et al. A review ofmeasurement -based assessments of the aerosol direct radiative effect and forcing
[ J ]. Atmos Chem Phys, 2006, 6: 613 - 666.
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