[1]张德二.我国历史时期以来降尘的天气气候初步分析[J].中国科学(B辑), 1984,(3):278-287. [2]石广玉,赵思雄. 沙尘暴研究中的若干科学问题[J]. 大气科学,2003,27(4):591-603. [3]Hankin E H. On dust raising wind sad descending currents[J]. J. India. Met. Memoirs,1921,22:PartVI. [4]Idso S R, Ingram R S,Pritchard J M. An American hoboob[J]. Bull,AMS.,1972,50:930-935. [5]Jeseph P V,Raipal D K,Deka S N. “Andhi”,the convective dust storms of Northwest India[J].J.Mausam,1980,31:431-442. [6]周秀骥,徐祥德,颜鹏,等. 2000年春季沙尘暴动力学特征[J]. 中国科学(D辑),2002,32(4):327-334. [7]周自江,章国材,中国北方的典型强沙尘暴事件(1954\_2002)[J]. 科学通报,2003,48(1):1224-1228. [8]Zhuang G, Yi Z, Duce R A. Chemistry of iron in marine aerosols[J]. Glob. Biogeochem. Cyc.,1992, 6:161-173. [9]孙东怀,安芷生,苏瑞侠,等.最近2.6 Ma中国北方季风环流与西风环流演变的风尘沉积记录[J]. 中国科学(D辑),2003,33(6): 497-504. [10]Petit J R,Mounier L, Jouzel J,et al. Climate and atmospheric history of past 420 000 years from the Vostok ice core[J]. Antarctica Nature,1999,399:429-436. [11]王涛. 走向世界的中国沙漠防治与实践[J].中国沙漠,2001,21(1):1-3. [12]李耀辉.近年来我国沙尘暴研究的新进展[J].中国沙漠,2004,24(5):616-622. [13]Martin J H. Glacial-interglacial CO2 change:The iron hypothesis[J]. Paleoceanography,1990, 5: 1-13. [14]Coale K H, Johnson K S, Fitzwater S E, et al. A massive phytoplankton bloom induced by an ecosystem-scale iron fertilization experiment in the equatorial Pacific Ocean[J]. Nature, 1996,383: 495-501. [15]Watson A J, Bakker D C E, Ridgwell A J, et al. Effect of iron supply on Southern Ocean CO2 uptake and implications for glacial atmospheric CO2[J]. Nature, 2000, 407: 730-733. [16]Gong S L, Zhang X Y,Zhao T L, et al. Characterization of soil dust aerosol in China and its transport/distribution during 2001 ACE-Asia 2.Model Simulation and Validation[J]. J.Geophys. Res., 2003,108, (D9): 4262. doi:10.1029/2002JD002633. [17]Zhang X Y, Gong S L, Shen Z X, Characterization of soil dust aerosol in China and its transport and distribution during 2001 ACE-Asia: 1. Network observations[J]. J. Geophys. Res.,2003, 108(D9):8032-8039. [18]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2003-03-04拉萨沙尘天气过程为例[J].科学通报,2004,49(11):1082-1090. [19]韩永翔,奚晓霞,宋连春,等.青藏高原沙尘及其可能的气候意义[J].中国沙漠,2004,24(5):588-592. [20]钱正安,宋敏红,李万元.近50年来中国北方沙尘暴的分布及变化趋势分析[J].中国沙漠,2002,22(2):106-111. [21]张小曳.亚洲粉尘的源区分布、释放、输送、沉降与黄土堆积[J].第四纪研究,2001,21(1):29-40. [22]Duce R A, Unni C K, Ray B J, et al. Long-range atmospheric transport of soil dust from Asia to the tropical North Pacific: Temporal variability[J]. Science, 1980,209: 1522-1524. [23]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. [24]吕连清,方小敏,鹿化煜,等,青藏高原末次冰期千年尺度的粒度记录[J].科学通报, 2004,49(11):480-486. [25]黄美元,王自发.东亚地区黄沙长距离输送模式的设计[J].大气科学,1998,22(6):625-637. [26]刘毅,任丽新,周乐义,等.一次黄沙输送过程的数值模拟研究[J].大气科学,1998,22(6):905-912. [27]康凤琴,李耀辉,吕世华. 2001年4月8日强沙尘暴的数值模拟研究[J].中国沙漠,2003,23(1):681-685. [28]GaoY, Arimoto R, Zhou M Y, et al. Relationships between the dust concentrations over eastern Asia and the remote North Pacific[J]. J. Geophys. Res., 1992,97: 9867-9872. [29]Toshiyuki M, Nobuo S, Uno I, et al. Ground-based network observation of Asian dust events of April 1998 in East Asia[J]. J. Geophys Res., 2001,106(16):18345-18359. [30]Liu M, Westphal D L, Wang S, et al. A high-resolution numerical study of the Asian dust storms of April 2001[J]. J. Geophys Res., 2003, 108, 8653,doi:10.1029/2002JD003178. [31]Holzer M, McKendry I G, Jaffe D A. Springtime trans-Pacific atmospheric transport from east Asia: A transit-time probability density function approach[J]. J. Geophys Res., 2003,108, 4708,doi:10.1029/2003JD003558. [32]Zhao T L, Gong S L, Zhang X Y, et al. Modeled size-segregated wet and dry deposition budgets of soil dust aerosol during ACE-Asia, 2001: Implications for trans-Pacific transport[J]. J. Geophys. Res., 2003. 108(D23), 8665, doi:10.1029/2002JD003363. [33]韩永翔,赵天良,宋连春,等.北太平洋地区春季粉尘的空间分布特征\_\_观测及模拟研究[J].中国环境科学,2005,25(3):257-261. [34]Crutzen P J, Ramanathan V. The parasol perasol effect on climate[J].Science,2003,302:1679-1681. [35]Yin Y, Levin Z, Reisin T G,et al. The effects of giant cloud condensation nuclei on the development of precipitation in convective clouds—a numerical study[J]. Atmos. Res.,2000,53:91-116. [36]Rosenfold D,Rudich Y,Lahav R. Desert dust suppressing precipitation:A possible desertification feedback loop[J]. Proceeding of National Academy Science,2001,98(11):5975-5980. [37]Bishop J K B, Davis R E, Sherman J T. Robotic Observations of Dust Storm enhancement of Carbon Biomass in the North Pacific[J]. Science, 2002, 298:817-821. [38]韩永翔,奚晓霞,方小敏,等.亚洲大陆沙尘过程与北太平洋地区生物环境效应[J].科学通报,2005,50(24):2698-2705. [39]刘东生. 黄土与环境[M].北京:科学出版社,1985. [40]Perkins S. Dust, the Thermostat:How tiny airborne particles manipulate global climate[J]. Science News Online,2001,160(13):200. [41]董光荣.中国沙漠形成演化气候变化与沙漠化研究[M].北京:海洋出版社,2002. [42]董光荣,董玉祥,金炯,等. 西藏“一江两河”中部流域地区土地沙漠化的成因与发展趋势[J].中国沙漠,1994, 14(2):9-17. [43]宋豫秦, 张力小. 历史时期我国沙尘暴东渐的原因分析[J] . 中国沙漠, 2002, 22(6): 632-635. [44]黄宁, 郑晓静, 陈广庭, 等. 沙尘暴对无线电波传播影响的研究[J] . 中国沙漠, 1998, 18(4): 350-353. [45]杨民, 蔡玉琴, 王式功, 等. 2000 年春季中国北方沙尘暴天气气候成因研究[J] . 中国沙漠, 2001, 21 (Suppl.): 6-11. [46]Wang Z, Akiemoto H, Uno I. Neutralization of soil aerosol and its impact on the distribution of acid rain over Esat Asia:observations and model results[J]. J. Geophys. Res.,2002,107,doi:10.1029/2001JI001040. |