Abstract
Based on the CALIPSO (Cloud–Aerosol Lidar and Infrared Pathfinder Satellite Observation) Version 4.10 products released on 8 November 2016, the Level 2 (L2) aerosol product over the Tibetan Plateau (TP) is evaluated and the aerosol radiative effect is also estimated in this study. As there are still some missing aerosol data points in the daytime CALIPSO Version 4.10 L2 product, this study re-calculated the aerosol extinction coefficient to explore the aerosol radiative effect over the TP based on the CALIPSO Level 1 (L1) and CloudSat 2B-CLDCLASS-LIDAR products. The energy budget estimation obtained by using the AODs (aerosol optical depths) from calculated aerosol extinction coefficient as an input to a radiative transfer model shows better agreement with the Earth’s Radiant Energy System (CERES) and CloudSat 2B-FLXHR-LIDAR observations than that with the input of AODs from aerosol extinction coefficient from CALIPSO Version 4.10 L2 product. The radiative effect and heating rate of aerosols over the TP are further simulated by using the calculated aerosol extinction coefficient. The dust aerosols may heat the atmosphere by retaining the energy in the layer. The instantaneous heating rate can be as high as 5.5 K day–1 depending on the density of the dust layers. Overall, the dust aerosols significantly affect the radiative energy budget and thermodynamic structure of the air over the TP, mainly by altering the shortwave radiation budget. The significant influence of dust aerosols over the TP on the radiation budget may have important implications for investigating the atmospheric circulation and future regional and global climate.
Similar content being viewed by others
References
Ackerman, A. S., O. B. Toon, D. E. Stevens, et al.,2000: Reduction of tropical cloudiness by soot. Science, 288, 1042–1047, doi: 10.1126/science.288.5468.1042.
Adams, A. M., J. M. Prospero, and C. D. Zhang, 2012: CALIPSOderived three-dimensional structure of aerosol over the Atlantic basin and adjacent continents. J. Climate, 25, 6862–6879, doi: 10.1175/JCLI-D-11-00672.1.
Albrecht, B. A., 1989: Aerosols, cloud microphysics, and fractional cloudiness. Science, 245, 1227–1230, doi: 10.1126/science. 245.4923.1227.
Charlson, R. J., S. E. Schwartz, J. M. Hales, et al.,1992: Climate forcing by anthropogenic aerosols. Science, 255, 423–430, doi: 10.1126/science.255.5043.423.
Chen, B., J. Huang, P. Minnis, et al.,2010: Detection of dust aerosol by combining CALIPSO active lidar and passive IIR measurements. Atmos. Chem. Phys., 10, 4241–4251, doi: 10.5194/acp-10-4241-2010.
Chen, B., P. Zhang, B. D. Zhang, et al.,2014: An overview of passive and active dust detection methods using satellite measurements. J. Meteor. Res., 28, 1029–1040, doi: 10.1007/s13351-014-4032-4.
Chen, S. Y., J. P. Huang, C. Zhao, et al.,2013: Modeling the transport and radiative forcing of Taklimakan dust over the Tibetan Plateau: A case study in the summer of 2006. J. Geophys. Res. Atmos., 118, 797–812, doi: 10.1002/jgrd.50122.
Choi, I. J., T. Iguchi, S. W. Kim, et al.,2014: The effect of aerosol representation on cloud microphysical properties in Northeast Asia. Meteor. Atmos. Phys., 123, 181–194, doi: 10.1007/s00703-013-0288-y.
D'Almeida, G. A., P. Koepke, and E. P. Shettle, 2005: Atmospheric aerosols: Global climatology and radiative characteristics. J. Med. Microbiol., 54, 55–61.
Fu, Q., and K. N. Liou, 1992: On the correlated k-distribution method for radiative transfer in nonhomogeneous atmospheres. J. Atmos. Sci., 49, 2139–2156, doi: 10.1175/1520-0469(1992)049<2139:OTCDMF>2.0.CO;2.
Fu, Q., and K. N. Liou, 1993: Parameterization of the radiative properties of cirrus clouds. J. Atmos. Sci., 50, 2008–2025, doi: 10.1175/1520-0469(1993)050<2008:POTRPO>2.0.CO;2.
Garnier, A., J. Pelon, M. A. Vaughan, et al.,2015: Lidar multiple scattering factors inferred from CALIPSO lidar and IIR retrievals of semi-transparent cirrus cloud optical depths over oceans. Atmos. Meas. Tech., 8, 2759–2774, doi: 10.5194/amt-8-2759-2015.
Ge, J. M., J. P. Huang, C. P. Xu, et al.,2014: Characteristics of Taklimakan dust emission and distribution: A satellite and reanalysis field perspective. J. Geophys. Res. Atmos., 119, 11772–11783, doi: 10.1002/2014JD022280.
Guo, J. P., X. Y. Zhang, Y. R. Wu, et al.,2011: Spatiotemporal variation trends of satellite-based aerosol optical depth in China during 1980–2008. Atmos. Environ., 45, 6802–6811, doi: 10.1016/j.atmosenv.2011.03.068.
Guo, J. P., H. Liu, F. Wang, et al.,2016: Three-dimensional structure of aerosol in China: A perspective from multi-satellite observations. Atmos. Res., 178–179, 580–589, doi: 10.1016/j.atmosres.2016.05.010.
Henderson, D. S., T. L’Ecuyer, G. Stephens, et al.,2013: A multisensor perspective on the radiative impacts of clouds and aerosols. J. Appl. Meteor. Climatol., 52, 853–871, doi: 10.1175/JAMC-D-12-025.1.
Hess, M., P. Koepke, and I. Schult, 1998: Optical properties of aerosols and clouds: The software package OPAC. Bull. Amer. Meteor. Soc., 79, 831–844, doi: 10.1175/1520-0477(1998)079 <0831:OPOAAC>2.0.CO;2.
Huang, J., Q. Fu, J. Su, et al.,2009: Taklimakan dust aerosol radiative heating derived from CALIPSO observations using the Fu–Liou radiation model with CERES constraints. Atmos. Chem. Phys., 9, 4011–4021, doi: 10.5194/acp-9-4011-2009.
Huang, J. P., P. Minnis, Y. H. Yi, et al.,2007: Summer dust aerosols detected from CALIPSO over the Tibetan Plateau. Geophys. Res. Lett., 34, L18805, doi: 10.1029/2007GL029938.
Huang, J. P., P. Minnis, B. Chen, et al.,2008: Long-range transport and vertical structure of Asian dust from CALIPSO and surface measurements during PACDEX. J. Geophys. Res. Atmos., 113, D23212, doi: 10.1029/2008JD010620.
Huang, J. P., T. H. Wang, W. C. Wang, et al.,2014: Climate effects of dust aerosols over East Asian arid and semiarid regions. J. Geophys. Res. Atmos., 119, 11398–11416, doi: 10.1002/2014JD021796.
Jia, R., Y. Z. Liu, B. Chen, et al.,2015: Source and transportation of summer dust over the Tibetan Plateau. Atmos. Environ., 123, 210–219, doi: 10.1016/j.atmosenv.2015.10.038.
Kim, D.-H., B. J. Sohn, T. Nakajima, et al.,2005: Aerosol radiative forcing over East Asia determined from ground-based solar radiation measurements. J. Geophys. Res. Atmos., 110, D10S22, doi: 10.1029/2004JD004678.
Kovalev, V. A., W. M. Hao, and C. Wold, 2007: Determination of the particulate extinction-coefficient profile and the columnintegrated lidar ratios using the backscatter-coefficient and optical-depth profiles. Appl. Opt., 46, 8627–8634, doi: 10.1364/AO.46.008627.
Kuang, Y., C. S. Zhao, J. C. Tao, et al.,2015: Diurnal variations of aerosol optical properties in the North China Plain and their influences on the estimates of direct aerosol radiative effect. Atmos. Chem. Phys., 15, 5761–5772, doi: 10.5194/acp-15-5761-2015.
Kuhlmann, J., and J. Quaas, 2010: How can aerosols affect the Asian summer monsoon? Assessment during three consecutive pre-monsoon seasons from CALIPSO satellite data. Atmos. Chem. Phys., 10, 4673–4688, doi: 10.5194/acp-10-4673-2010.
Lau, K. M., M. K. Kim, and K. M. Kim, 2006: Asian summer monsoon anomalies induced by aerosol direct forcing: The role of the Tibetan Plateau. Climate Dyn., 26, 855–864, doi: 10.1007/s00382-006-0114-z.
Lau, W. K. M., 2016: The aerosol–monsoon climate system of Asia: A new paradigm. J. Meteor. Res., 30, 1–11, doi: 10.1007/s13351-015-5999-1.
Lau, W. K. M., and K.-M. Kim, 2010: Fingerprinting the impacts of aerosols on long-term trends of the Indian summer monsoon regional rainfall. Geophys. Res. Lett., 37, L16705, doi: 10.1029/2010GL043255.
Lau, W. K. M., M.-K. Kim, K.-M. Kim, et al.,2010: Enhanced surface warming and accelerated snow melt in the Himalayas and Tibetan Plateau induced by absorbing aerosols. Environ. Res. Lett., 5, 025204, doi: 10.1088/1748-9326/5/2/025204.
L’Ecuyer, T. S., N. B. Wood, T. Haladay, et al.,2008: Impact of clouds on atmospheric heating based on the R04 CloudSat fluxes and heating rates data set. J. Geophys. Res. Atmos., 113, D00A15, doi: 10.1029/2008JD009951.
Li, H. J., W. Zheng, and Q. Gong, 2013: An analysis on detection of a sand–dust weather event over Taklimakan Desert based on polarization micro-pulse lidar. Desert Oasis Meteor., 7, 1–5. (in Chinese)
Li, Z. Q., J. P. Guo, A. J. Ding, et al.,2017: Aerosol and boundary-layer interactions and impact on air quality. Natl. Sci. Rev., 4, 810–833, doi: 10.1093/nsr/nwx117.
Liu, Y., Y. Sato, R. Jia, et al.,2015: Modeling study on the transport of summer dust and anthropogenic aerosols over the Tibetan Plateau. Atmos. Chem. Phys., 15, 12581–12594, doi: 10.5194/acp-15-12581-2015.
Liu, Z. Y., D. Liu, J. P. Huang, et al.,2008a: Airborne dust distributions over the Tibetan Plateau and surrounding areas derived from the first year of CALIPSO lidar observations. Atmos. Chem. Phys., 8, 5045–5060, doi: 10.5194/acp-8-5045-2008.
Liu, Z. Y., A. Omar, M. Vaughan, et al.,2008b: CALIPSO lidar observations of the optical properties of Saharan dust: A case study of long-range transport. J. Geophys. Res. Atmos., 113, D07207, doi: 10.1029/2007JD008878.
Müller, D., K. Franke, A. Ansmann, et al.,2003: Indo-Asian pollution during INDOEX: Microphysical particle properties and single-scattering albedo inferred from multiwavelength lidar observations. J. Geophys. Res. Atmos., 108, 4600, doi: 10.1029/2003JD003538.
Mukai, M., T. Nakajima, and T. Takemura, 2008: A study of anthropogenic impacts of the radiation budget and the cloud field in East Asia based on model simulations with GCM. J. Geophys. Res. Atmos., 113, D12211, doi: 10.1029/2007JD 009325.
Nakajima, T., S. C. Yoon, V. Ramanathan, et al.,2007: Overview of the Atmospheric Brown Cloud East Asian Regional Experiment 2005 and a study of the aerosol direct radiative forcing in East Asia. J. Geophys. Res. Atmos., 112, D24S91, doi: 10.1029/2007JD009009.
Omar, A. H., D. M. Winker, M. A. Vaughan, et al.,2009: The CALIPSO automated aerosol classification and lidar ratio selection algorithm. J. Atmos. Oceanic Technol., 26, 1994–2014, doi: 10.1175/2009JTECHA1231.1.
Omar, A. H., J. L. Tackett, M. A. Vaughan, et al.,2016: Enhancements to the CALIOP aerosol subtyping and lidar ratio selection algorithms for level II Version 4. AGU Fall Meeting, San Francisco, 12–1. December, American Geophysical Union.
Qian, Y., M. G. Flanner, L. R. Leung, et al.,2011: Sensitivity studies on the impacts of Tibetan Plateau snowpack pollution on the Asian hydrological cycle and monsoon climate. Atmos. Chem. Phys., 11, 1929–1948, doi: 10.5194/acp-11-1929-2011.
Qian, Y. F., Y. Zhang, Y. Y. Huang, et al.,2004: The effects of the thermal anomalies over the Tibetan Plateau and its vicinities on climate variability in China. Adv. Atmos. Sci., 21, 369–381, doi: 10.1007/BF02915565.
Ramanathan, V., M. V. Ramana, G. Roberts, et al.,2007: Warming trends in Asia amplified by brown cloud solar absorption. Nature, 448, 575–578, doi: 10.1038/nature06019.
Rose, F. G., and T. P. Charlock, 2002: New Fu–Liou code tested with ARM Raman lidar and CERES in pre-CALIPSO sensitivity study. 11th Conference on Atmospheric Radiation, Ogden, Utah, USA, 7 June, Amer. Meteor. Soc.
Rosenfeld, D., S. Sherwood, R. Wood, et al.,2014: Climate effects of aerosol–cloud interactions. Science, 343, 379–380, doi: 10.1126/science.1247490.
Sassen, K., 1991: The polarization lidar technique for cloud research: A review and current assessment. Bull. Amer. Meteor. Soc., 72, 1848–1866, doi: 10.1175/1520-0477(1991)2.0. co;2.
Satheesh, S. K., V. Ramanathan, X. Li-Jones, et al.,1999: A model for the natural and anthropogenic aerosols over the tropical Indian Ocean derived from Indian Ocean Experiment data. J. Geophys. Res. Atmos., 104, 27421–27440, doi: 10.1029/1999JD900478.
Satheesh, S. K., V. Vinoj, S. S. Babu, et al.,2009: Vertical distribution of aerosols over the east coast of India inferred from airborne LIDAR measurements. Ann. Geophys., 27, 4157–4169, doi: 10.5194/angeo-27-4157-2009.
Seiki, T., and T. Nakajima, 2014: Aerosol effects of the condensation process on a convective cloud simulation. J. Atmos. Sci., 71, 833–853, doi: 10.1175/JAS-D-12-0195.1.
Sekiguchi, M., T. Nakajima, K. Suzuki, et al.,2003: A study of the direct and indirect effects of aerosols using global satellite data sets of aerosol and cloud parameters. J. Geophys. Res. Atmos., 108, 4699, doi: 10.1029/2002JD003359.
Shen, L. L., L. F. Sheng, and J. J. Chen, 2010: Preliminary analysis of the spatial distribution of the dust aerosol in a heavy dust storm. J. Desert Res., 30, 1483–1490. (in Chinese)
Su, J., J. P. Huang, Q. Fu, et al.,2008: Estimation of Asian dust aerosol effect on cloud radiation forcing using Fu–Liou radiative model and CERES measurements. Atmos. Chem. Phys., 8, 2763–2771, doi: 10.5194/acp-8-2763-2008.
Takamura, T., N. Sugimoto, A. Shimizu, et al.,2007: Aerosol radiative characteristics at Gosan, Korea, during the Atmospheric Brown Cloud East Asian Regional Experiment 2005. J. Geophys. Res. Atmos., 112, D22S36, doi: 10.1029/2007JD008506.
Tegen, I., A. A. Lacis, and I. Fung, 1996: The influence on climate forcing of mineral aerosols from disturbed soils. Nature, 380, 419–422, doi: 10.1038/380419a0.
Toth, T. D., J. L. Zhang, J. R. Campbell, et al.,2016: Temporal variability of aerosol optical thickness vertical distribution observed from CALIOP. J. Geophys. Res. Atmos., 121, 9117–9139, doi: 10.1002/2015JD024668.
Twomey, S., 1977: The influence of pollution on the shortwave albedo of clouds. J. Atmos. Sci., 34, 1149–1152, doi: 10.1175/1520-0469(1977)034<1149:TIOPOT>2.0.CO;2.
Uno, I., H. Amano, S. Emori, et al.,2001: Trans-Pacific yellow sand transport observed in April 1998. A numerical simulation. J. Geophys. Res. Atmos., 106, 18331–18344, doi: 10.1029/2000JD900748.
Wang, W. C., J. P. Huang, T. Zhou, et al.,2013: Estimation of radiative effect of a heavy dust storm over northwest China using Fu–Liou model and ground measurements. J. Quant. Spectrosc. Radiat. Transf., 122, 114–126, doi: 10.1016/j.jqsrt.2012.10.018.
Winker, D. M., M. A. Vaughan, A. Omar, et al.,2009: Overview of the CALIPSO mission and CALIOP data processing algorithms. J. Atmos. Oceanic Technol., 26, 2310–2323, doi: 10.1175/2009jtecha1281.1.
Wonsick, M. M., R. T. Pinker, and Y. Ma, 2014: Investigation of the “elevated heat pump” hypothesis of the Asian monsoon using satellite observations. Atmos. Chem. Phys., 14, 8749–8761, doi: 10.5194/acp-14-8749-2014.
Wu, G. X., X. Liu, Q. Zhang, et al.,2002: Progresses in the study of the climate impacts of the elevated heating over the Tibetan Plateau. Climatic Environ. Res., 7, 184–201. (in Chinese)
Wu, G. X., J. Y. Mao, A. M. Duan, et al.,2006: Current progresses in study of impacts of the Tibetan Plateau on Asian summer climate. Acta Meteor. Sinica, 20, 144–158.
Xia, X. G., P. C. Wang, Y. S. Wang, et al.,2008: Aerosol optical depth over the Tibetan Plateau and its relation to aerosols over the Taklimakan Desert. Geophys. Res. Lett., 35, L16804, doi: 10.1029/2008GL034981.
Yang, K., Y.-Y. Chen, and J. Qin, 2009: Some practical notes on the land surface modeling in the Tibetan Plateau. Hydrol. Earth Syst. Sci., 13, 687–701, doi: 10.5194/hess-13-687-2009.
Yang, W. Y., D. Z. Ye, and G. X. Wu, 1992: The influence of the Tibetan Plateau on the thermal and circulation fields over East Asia in summer. II: Main features of the local circulation fields and the large-scale vertical circulation fields. Chinese J. Atmos. Sci., 16, 287–301. (in Chinese)
Yasunari, T. J., P. Bonasoni, P. Laj, et al.,2010: Estimated impact of black carbon deposition during pre-monsoon season from Nepal Climate Observatory-Pyramid data and snow albedo changes over Himalayan glaciers. Atmos. Chem. Phys., 10, 6603–6615, doi: 10.5194/acp-10-6603-2010.
Young, S. A., and M. A. Vaughan, 2009: The retrieval of profiles of particulate extinction from Cloud–Aerosol Lidar Infrared Pathfinder Satellite Observations (CALIPSO) data: Algorithm description. J. Atmos. Oceanic Technol., 26, 1105–1119, doi: 10.1175/2008JTECHA1221.1.
Zhang, H., J. H. Ma, and Y. F. Zheng, 2010: Modeling study of the global distribution of radiative forcing by dust aerosol. Acta Meteor. Sinica, 24, 558–570.
Zhou, L. B., J. H. Zhu, H. Zou, et al.,2013: Atmospheric moisture distribution and transport over the Tibetan Plateau and the impacts of the South Asian summer monsoon. Acta Meteor. Sinica, 27, 819–831, doi: 10.1007/s13351-013-0603-z.
Zhu, Y. X., Y. H. Ding, and H. G. Xu, 2008: Decadal relationship between atmospheric heat source and winter–spring snow cover over the Tibetan Plateau and rainfall in East China. Acta. Meteor. Sinica, 22, 303–316.
Acknowledgements
The CALIPSO, CloudSat, and CERES data were obtained from the NASA Langley Research Center Atmospheric Sciences Data Center, and the authors gratefully acknowledge their efforts in making these data available online. We also gratefully acknowledge Q. Fu and K. N. Liou for providing the Fu–Liou model.
Author information
Authors and Affiliations
Corresponding author
Additional information
Supported by the Strategic Priority Research Program of Chinese Academy of Sciences (XDA2006010301), National Natural Science Foundation of China (91737101, 41475095, and 41405010), Fundamental Research Funds for Central Universities (lzujbky-2017-63), and China 111 Project (B13045).
Rights and permissions
About this article
Cite this article
Jia, R., Liu, Y., Hua, S. et al. Estimation of the Aerosol Radiative Effect over the Tibetan Plateau Based on the Latest CALIPSO Product. J Meteorol Res 32, 707–722 (2018). https://doi.org/10.1007/s13351-018-8060-3
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s13351-018-8060-3