Abstract
The effect of anthropogenic aerosols on the spring persistent rain (SPR) over eastern China is investigated by using a high-resolution Community Atmosphere Model version 5.1 (CAM5.1). The results show that the SPR starts later due to anthropogenic aerosols, with a shortened duration and reduced rainfall amount. A reduction in air temperature over the low latitudes in East Asia is linked to anthropogenic aerosols; so is a weakened southwesterly on the north side of the subtropical high. Meanwhile, air temperature increases significantly over the high latitudes. This north-south asymmetrical thermal effect acts to reduce the meridional temperature gradient, weakening the upper-level westerly jet over East Asia and the vertical motion over southeastern China. As a result, the SPR is reduced and has a much shorter duration. The indirect effect of anthropogenic aerosols also plays an important role in changing the SPR. Cloud droplet number concentration increases due to anthropogenic aerosols acting as cloud condensation nuclei, leading to a reduction in cloud effective radius over eastern China and a reduced precipitation efficiency there.
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References
Albrecht, B. A., 1989: Aerosols, cloud microphysics, and fractional cloudiness. Science, 245, 1227–1230.
Bréon, F. M., D. Tanré, and S. Generoso, 2002: Aerosol effect on cloud droplet size monitored from satellite. Science, 295, 834–838.
Chung, C. E., S. Nigam, and J. T. Kiehl, 2002: Effects of the South Asian absorbing haze on the northeast monsoon and surface-air heat exchange. J. Climate, 15, 2462–2476.
Chung, S. H., and J. H. Seinfeld, 2005: Climate response of direct radiative forcing of anthropogenic black carbon. J. Geophys. Res., 110, D11102, doi: 10.1029/2004JD005441.
Cowan, T., and W. Cai, 2011: The impact of Asian and non-Asian anthropogenic aerosols on the 20th century Asian summer monsoon. Geophys. Res. Lett., 38, L11703, doi: 10.1029/2011GL047268.
Dee, D. P., S. M. Uppala, A. J. Simmons, et al., 2011: The ERA-Interim reanalysis: Configuration and performance of the data assimilation system. Quart. J. Roy. Meteor. Soc., 137, 553–597.
Deng Jiechun, Xu Haiming, Ma Hongyun, et al., 2014a: The effects of anthropogenic aerosols over eastern China on East Asian monsoons in a high resolution CAM5.1 model. J. Trop. Meteor., 30, in press. (in Chinese)
—, —, —, et al., 2014b: A numerical study of the effect of anthropogenic aerosols over eastern China on East Asian summer monsoon onset and its northward advancement. J. Trop. Meteor., 30, in press. (in Chinese)
Gettelman, A., X. Liu, S. J. Ghan, et al., 2010: Global simulations of ice nucleation and ice supersaturation with an improved cloud scheme in the Community Atmosphere Model. J. Geophys. Res., 115, D18126, doi: 10.1029/2009JD013797.
Gu, Y., K. N. Liou, Y. Xue, et al., 2006: Climatic effects of different aerosol types in China simulated by the University of California, Los Angeles atmospheric general circulation model. J. Geophys. Res., 111, doi: 10.1029/2005JD006312.
Han, Q., W. B. Rossow, and A. A. Lacis, 1994: Nearglobal survey of effective cloud droplet radii in liquid water clouds using ISCCP data. J. Climate, 7, 465–497.
Hu Haibo, Liu Chao, Zhang Yuan, et al., 2011: The effects of aerosols in CAM3.0 on climate in East Asia during boreal spring. Scientia Meteor. Sinica, 31, 466–474. (in Chinese)
Hu, N., and X. Liu, 2013: Modeling study of the effect of anthropogenic aerosols on late spring drought in South China. Acta Meteor. Sinica, 27, 701–715.
Hurrell, J. W., J. J. Hack, D. Shea, et al., 2008: A new sea surface temperature and sea ice boundary dataset for the Community Atmosphere Model. J. Climate, 21, 5145–5153.
Jiang Pinping and Zhao Ping, 2012: The interanuual variability of spring rainy belt over southern China and the associated atmospheric circulation anomalies. Acta Meteor. Sinica, 70, 681–689. (in Chinese)
Jiang, Y., X. Liu, X. Q. Yang, et al., 2013: A numerical study of the effect of different aerosol types on East Asian summer clouds and precipitation. Atmos. Environ., 70, 51–63.
Kim, M. K., K. M. Lau, M. Chin, et al., 2006: Atmospheric teleconnection over Eurasia induced by aerosol radiative forcing during boreal spring. J. Climate, 19, 4700–4718.
Lamarque, J. F., T. C. Bond, V. Eyring, et al., 2010: Historical (1850–2000) gridded anthropogenic and biomass burning emissions of reactive gases and aerosols: Methodology and application. Atmos. Chem. Phys., 10, 7017–7039.
Lau, K. M., and K. M. Kim, 2006a: Observational relationships between aerosol and Asian monsoon rainfall, and circulation. Geophys. Res. Lett., 33, L21810, doi: 10.1029/2006GL027546.
—, M. K. Kim, and K. M. Kim, 2006b: Asian summer monsoon anomalies induced by aerosol direct forcing: The role of the Tibetan Plateau. Climate Dyn., 26, 855–864.
Li Chao, Xu Haiming, Zhu Suxing, et al., 2010: Numerical analysis on formation mechanism of spring persistent rain. Plateau Meteor., 29, 99–108. (in Chinese)
Li, Z., K. Lee, Y. Wang, et al., 2010: First observationbased estimates of cloud-free aerosol radiative forcing across China. J. Geophys. Res., 115, doi: 10.1029/2009JD013306.
Liu, X., R. C. Easter, S. J. Ghan, et al., 2012: Toward a minimal representation of aerosols in climate models: Description and evaluation in the Community Atmosphere Model CAM5. Geosci. Model Dev., 5, 709–739.
Liu, Y., J. Sun, and B. Yang, 2009: The effects of black carbon and sulfate aerosols in China regions on East Asian monsoons. Tellus(B), 61, 642–656.
Menon, S., J. Hansen, L. Nazarenko, et al., 2002: Climate effects of black carbon aerosols in China and India. Science, 297, 2250–2253.
Ming, Y., and V. Ramaswamy, 2009: Nonlinear climate and hydrological response to aerosol effects. J. Climate, 22, 1329–1339.
Neale, R. B., A. Gettelman, S. Park, et al., 2010: Description of the NCAR Community Atmosphere Model (CAM5.0). NCAR Technical Note NCAR/TN-486+STR: 7–8.
Pwlowska, H., and J. L. Brenguier, 2000: Microphysical properties of stratocumulus clouds during ACE-2. Tellus, 52B, 868–887.
Qi, L., J. He, Z. Zhang, et al., 2008: Seasonal cycle of the zonal land-sea thermal contrast and East Asian subtropical monsoon circulation. Chinese Sci. Bull., 53, 131–136.
Tian, S. F., and T. Yasunari, 1998: Climatological aspects and mechanism of spring persistent rains over central China. J. Meteor. Soc. Japan, 76, 57–71.
Twomey, S., 1997: The influence of pollution on the short-wave albedo of clouds. J. Atmos. Sci., 34, 1149–1152.
Wan Rijin and Wu Guoxiong, 2006: Mechanism of the spring persistent rains over southeastern China. Sci. China (Earth Science), 50, 130–144. (in Chinese)
— and —, 2008a: Temporal and spatial distribution of the spring persistent rains over southeastern China. Acta Meteor. Sinica, 66, 310–319. (in Chinese)
—, Wang Tongmei, and Wu Guoxiong, 2008b: Temporal variations of the spring persistent rains and SCS subtropical high and their correlations to the circulation and precipitation of the East Asian summer monsoon. Acta Meteor. Sinica, 66, 800–807. (in Chinese)
—, Zhao Bingke, and Hou Yiling, 2008c: Interanuual variability of spring persistent rain over southeastern China and its effect factor. Plateau Meteor., 27, 118–123. (in Chinese)
Wang, B., Q. Ding, X. Fu, et al., 2005: Fundamental challenge in simulation and prediction of summer monsoon rainfall. Geophys. Res. Lett., 32, L15711, doi: 10.1029/2005GL022734.
Wang, Z., H. Zhang, J. N. Li, et al., 2013: Radiative forcing and climate response due to the presence of black carbon in cloud droplets. J. Geophys. Res., 118, 3662–3675.
Wang Zhili, Guo Pinwen, and Zhang Hua, 2009a: A numerical study of direct radiative forcing due to black carbon and its effects on the summer precipitation in China. Climatic Environ. Res., 14, 161–171. (in Chinese)
—, Zhang Hua, and Guo Pinwen, 2009b: Effects of black carbon aerosol in South Asia on Asian summer monsoon. Plateau Meteor., 28, 419–424. (in Chinese)
Wetzel, M. A., and L. L. Stowe, 1999: Satelliteobserved patterns in stratus microphysics, aerosol optical thickness, and shortwave radiative forcing. J. Geophys. Res., 104, 31287–31299, doi: 1011029/1999JD900922.
Xie, P., and P. A. Arkin, 1997: Global precipitation: A 17-year monthly analysis based on gauge observations, satellite estimates, and numerical model outputs. Bull. Amer. Meteor. Soc., 78, 2539–2558.
Yang Huiling, Xiao Hui, and Hong Yanchao, 2011: Progress in impacts of aerosol on cloud properties and precipitation. Climatic Environ. Res., 16, 525–542. (in Chinese)
Zhang Bo, Zhong Shanshan, Zhao Bin, et al., 2011: The influence of the subtropical sea surface temperature over the western Pacific Ocean on spring persistent rains. J. Appl. Meteor. Sci., 22, 57–65. (in Chinese)
Zhang, H., Z. Wang, P. Guo, et al., 2009: A modeling study of the effects of direct radiative forcing due to carbonaceous aerosol on the climate in East Asia. Adv. Atmos. Sci., 26, 1–10.
—, —, Z. Wang, et al., 2012: Simulation of direct radiative forcing of aerosols and their effects on East Asian climate using an interactive AGCM-aerosol coupled system. Climate Dyn., 38, 1675–1693.
Zhang Jie, Zhou Tianjun, Yu Rucong, et al., 2009: Atmospheric water vapor transport and corresponding typical anomalous spring rainfall patterns in China. Chinese J. Atmos. Sci., 33, 121–134. (in Chinese)
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Supported by the National Basic Research and Development (973) Program of China (2010CB428505), National Natural Science Foundation of China (41275094), Priority Academic Program Development of Jiangsu Higher Education Institutions (PAPD), and Jiangsu Provincial Qinglan Project.
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Deng, J., Xu, H., Ma, H. et al. Numerical study of the effect of anthropogenic aerosols on spring persistent rain over Eastern China. J Meteorol Res 28, 341–353 (2014). https://doi.org/10.1007/s13351-014-3198-0
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DOI: https://doi.org/10.1007/s13351-014-3198-0