LATEST ADVANCES IN AEROSOL ABSORPTION AND ITS CLIMATE EFFECTS
Received date: 2002-11-08
Revised date: 2003-11-03
Online published: 2004-08-01
It's not enough to focus only on Top of Atomospheric (TOA) aerosol direct radiative forcing, especially for absorptive aerosol types such as smoke and dust aerosols. It's shown by INDOEX experiment that absorptive aerosol (mainly from anthropogenic productions) surface radiative forcing in magnitude is nearly 3 times more than that at TOA, the difference between them is the heating of atmosphere that contains absorptive aerosol. Combined with the heating of the atmospheric and reducing in earth's surface radiation due to aerosol absorption, evaporation and atmospheric stability may be affected and it is possible to influence hydrological cycle. Additionally, aborptive aerosol may produce cloud “burning effect”, then result in decreased cloud amount. Aerosol absorption has become the hot topic concerning aerosol's effects on climate. It's valuable to study aerosol absorption, since that there are large uncertainties and some inconsistency results have been obtained concerning aerosol absorption and its effects on climate. It's absolutely necessary to strengthen experiment and theory studies on aerosol absorption in China due to high occurrences of dust storms in north China and high concentration of black carbon (BC) in east China. The high concentration of BC is partly resulted by our energy consumption structure and relatively low energy consumption efficiency. It's shown by data and model analyses that aerosol absorption probably plays an important role in unique climate change in China with comparsion of in other region or globe. It's of significance to deepen our knowledge of aerosol radiative forcing and climate effects in China with the help of global or region climate model, at the same time, it's also helpful to estimate the environment and climate effects of pollution control measures taken by our country in recent years.
Key words: Absorption; Radiative forcing; Climate effect.
XIA Xiang-ao , WANG Ming-xing . LATEST ADVANCES IN AEROSOL ABSORPTION AND ITS CLIMATE EFFECTS[J]. Advances in Earth Science, 2004 , 19(4) : 630 -635 . DOI: 10.11867/j.issn.1001-8166.2004.04.0630
[1]IPCC. Radiative forcing of climate change[A]. In: Climate change 2001[C]. Cambridge University Press, 2001.
[2]Charlson R J, Langner J, Rodhe H, et al. Perturbation of the Northern hemisphere radiative balance by back-scattering from anthrpogenic aerosol[J].Tellus, 1991,43AB: 152-163.
[3]Kiehl J T, Briegleb B P. The relative roles of sulfate aerosols and greenhouse gases in climate forcing[J]. Science, 1993, 260: 311-314.
[4]Hobbs P V, Reid J S, Kotchenruther R A, et al. Direct radiative forcing by smoke from biomass burning[J]. Science, 1997, 275: 1776-1778.
[5]Li X, Maring H, Savoie D, et al. Dominance of mineral dust in aerosol light scattering in the North Atlantic trade winds[J]. Nature,1996,380: 416-419.
[6]Tegen I, Hollrig P, Chin M, et al. Contribution of different aerosol species to the global aerosol extinction optical thickness: Estimates from model results[J].Journal Geophysical Research, 1997, 102:23 895-23 915.
[7]Tegen I, Lacis A A, Fung I. The influence on climate forcing of mineral aerosols from disturbed soils[J]. Nature, 1996, 380: 419-422.
[8]Satheesh S K, Ramanathan V. Large differences in tropical aerosol forcing at the top of the atmosphere and earth's surface[J]. Nature, 2000, 405: 60-63.
[9]Ramanathan V, Crutzen P J, Kiehl J T, et al. Aerosol, climate, and hydrological cycle[J]. Science, 2001, 294: 2 119-2 124.
[10]Satheesh S K. Aerosol radiative forcing over land: Effect of surface and cloud reflection[J].Annales Geophysicae, 2002, 20: 1-5.
[11]Ackerman A S, Toon O B, Stevens D E, et al. Reduction of tropical cloudiness by soot[J]. Science, 2000, 288: 1 042-1 047.
[12]Norris J R. Has Northern Indian ocean cloud cover changed due to increasing anthropogenic aerosols?[J]. Geophysical Research Letters, 2001, 28: 3 271-3 274.
[13]Charney J. Drought in the Sahara: A biogeophysical feedback mechanism[J].Science, 1975,187:434-435.
[14]Brooks N,Legrand M. Dust variability over northern Africa and rainfall in the Sahel[A]. In: McLaren S J, Kniveton D R,eds. Linking Climate Change to Land Surface Change[C]. Kluwer Academic Publishers, 1999.125.
[15]Zhang Renjian(张仁健), Wang Mingxing(王明星), Zhang Wen(张文), et al. Physical and chemical characteristics of dust storms in spring, 2000[J]. Climatic and Environmental research(气候与环境研究), 2000, 5: 259-266(in Chinese).
[16]Zhang G, Yi Z, Duce R A, et al. Chemistry of iron in marine aerosols[J].Global Biogeochemical Cycles, 1992,6:161-173.
[17]Ye Duzheng(叶笃正), Chou Jifan(丑纪范), Liu Jiyuan(刘纪远), et al. Causes of sand-stormy weather in Northern China and control measurements[J]. Acta Geographica Sinica(地理学报), 2000, 55:513-521(in Chinese).
[18]Zhou Xiuji(周秀骥), Xu Xiangde(徐祥德), Yan Peng(颜鹏), et al. Dynamic characteristics of dust storms in spring,2000[J].Science in China)D(中国科学D辑), 2002,32:327-334(in Chinese).
[19]Zhang Xiaozhuai(张小曳). Source distributions, emission, transportation, deposition of Asia dust and loess accumulation[J].Quaternary Sciences(第四纪研究), 2001,21:29-40(in Chinese).
[20]Shen Zhibao(沈志宝), Wei Li(魏丽). The influences of atmospheric dust on the radiative heating in the earth atmosphere system and atmosphere in the north western China[J]. Plateau Meteorology(高原气象), 1999,18:425-435(in Chinese).
[21]Shen Zhibao(沈志宝), Wei Li(魏丽). The influence of atmospheric dust on the surface radiative energy budget in Heihe region[J].Plateau Meteorology(高原气象), 1999, 18:1-8(in Chinese).
[22]Qiu Jinheng(邱金桓), Sun Jinhui(孙金辉). Optical remote sensing and analysis of dust storml [J]. Chinese Journal of Atmospheric Science(大气科学),1994, 18:1-10(in Chinese).
[23]Qiu Jinheng(邱金桓). Determine atmospheric aerosol optical depth using multi-waved solar direct radiation observation data. I: Theory[J]. Chinese Journal of Atmospheric Science(大气科学), 1995, 19:385-394(in Chinese).
[24]Luo Yunfeng(罗云峰), Lü Daren(吕达仁), Li Weiliang(李维亮), et al. The characteristics of atmospheric aerosol optical epth variation over China in recent 30 years[J]. Chinese Science Bulletins(科学通报), 2000, 45:549-554(in Chinese).
[25]Andreae M O. The dark side of aerosols[J]. Nature, 409: 671-672.
[26]Jacobson M Z. Strong radiative heating due to the mixing state of black carbon in atmospheric aerosols[J]. Nature, 2001, 409: 695-697.
[27]Hansen J, Sato M, Lacis A, et al. Perspective: Climate forcings in the industrial era[J]. Proceedings of the National Academy of Sciences, 1998, 22:12 753-12 758.
[28]Smith S J, Wigley T M L, Edmonds J. A new route toward limiting climate change?[J]. Science, 2000, 290: 1 109-1 110.
[29]Li X W, Zhou X J, Li W L. The cooling of Sichuan province in recent 40 years and its probable mechanism[J]. Acta Meteorologica Sinica, 1995, 9: 57-68.
[30]Luo Y F Zhou X J, Li W L. A numerical study of the atmospheric aerosol climate forcing in China[J]. Chinese Journal of Atmospheric Science, 1999, 23: 1-12.
[31]Qian Yun(钱云), Fu Congbin(符淙斌), Wang Zifa(王自发). The influence of industrial SO2 on temperature in East Asia and China[J]. Climatic and Environmental Research(环境和气候研究), 1996,2:143-149(in Chinese).
[32]Yu S C, Saxena V K, Zhao Z C. A comparison of signals of regional aerosol-induced forcing in eastern China and the southeastern United States[J].Geophysical Research Letters, 2001, 28: 713716.
[33]Krishnan R, Ramanathan V. Evidence of surface cooling from absorbing aerosols[J]. Geophysical Research Letters, 2002, 29:10.1029/2002GL014687.
[34]Kaiser D P. Analysis of total cloud amount over China[J]. Geophysical Research Letters, 1998, 25: 3 599-3 602.
[35]Xu Q. Abrupt change of the mid-summer climate in central east China by the influence of atmospheric pollution[J]. Atmospheric Environment, 2001, 35: 5 029-5 040.
[36]Menon S, Hansen J, Nazarenko L, et al. Climate effects of black carbon aerosols in China and India[J]. Science, 2002, 297: 2 250-2 253.
[37]Rosenfeld D. Suppression of rain and snow by urban and industrial air pollution[J]. Science, 2000, 287: 1 793-1 796.
[38]Lohmann U. Interactions between anthropogenic aerosols and hydrologic cycles[J]. IGACtivities, 2002,26:3-7.
[39]Streets D G, Jiang K J, Hu X L, et al. Recent reductions in China's greenhouse gas emissions[J]. Science, 2001, 294: 1 835-1 836.
[40]Chameides W L, Hu H, Liu S, et al. Case study of the effects of atmospheric aerosols and reagional haze on agriculture: An opportunity to enhance crop yields in China through emission controls? [J]. Proceedings of the National Academy of Sciences, 1999, 26: 13 626-13 633.
[41]Chameides WL, Li X, Tang X, et al. Is ozone pollution affecting crop yields in China?[J]. Geophysical Research Letters, 1999, 26: 867-870.
/
〈 |
|
〉 |