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[1] Liu X.D. and B.D. Chen, Climatic warming in the Tibetan Plateau during recent decades. International Journal of Climatology, 2000, 20 (14), 1729-1742.
[2] Liu X.D. and Z.-Y. Yin, Spatial and temporal variation of the summer precipitation over the eastern Tibetan Plateau and the Northern Atlantic Oscillation. Journal of Climate, 2001, 14(13), 2896-2909.
[3] Liu X.D. and M. Yanai, Relationship between the Indian monsoon precipitation and the tropospheric temperature over the Eurasian continent. Quarterly Journal of the Royal Meteorological Society, 2001, 127(573), 909-937.
[4] Liu X.D. and Z.-Y. Yin, Sensitivity of East Asian monsoon climate to the Tibetan Plateau uplift. Palaeogeography, Palaeoclimatology, Palaeoecology, 2002, 183, 223-245.
[5] Liu X.D. and M. Yanai, Influence of Eurasian spring snow cover on Asian summer. International Journal of Climatology, 2002, 22(9), 1075-1089.
[6] Liu X.D., J.E. Kutzbach, Z. Liu, Z.S. An and L. Li, The Tibetan Plateau as amplifier of orbital-scale variability of the East Asian monsoon. Geophysical Research Letters, 2003, 30(16), 1839, doi:10.1029/2003GL017510.
[7] Liu X.D., Z.-Y. Yin, X.Y. Zhang and X.C. Yang, Analyses of the spring dust storm frequency of northern China in relation to antecedent and concurrent wind, precipitation, vegetation, and soil moisture conditions. J. Geophys. Res., 2004, 109, D16210, doi:10.1029/2004JD004615.
[8] Liu X.D., Z. Liu, J.E. Kutzbach, S.C. Clemens and W.L. Prell, Hemispheric insolation forcing of the Indian Ocean and Asian monsoon: Local versus remote impacts. Journal of Climate, 2006, 19(23), 6195–6208.
[9] Liu X.D., Z. Liu, S. Clemens, W. Prell and J. Kutzbach, A coupled model study of glacial Asian monsoon variability and Indian Ocean Dipole. J. Metero. Soc. Japan, 2007, 85(1), 1-10.
[10]Liu X.D., Z.-Y. Yin, X.M. Shao and N.S. Qin, Temporal trends and variability of daily maximum and minimum, extreme temperature events, and growing season length over the eastern and central Tibetan Plateau during 1961-2003. J. Geophys. Res., 2006, 111, D19109, doi:10.1029/ 2005JD006915.
[11]Liu X.D., Z.G. Cheng, L.B. Yan and Z.Y. Yin, Elevation dependency of recent and future minimum surface temperature trends in the Tibetan Plateau and its surroundings, Global and Planetary Change, 2009, 68, 164-174.
[12]Liu X.D., A.J. Bai, C.H. Liu, Diurnal variations of summertime precipitation over the Tibetan Plateau in relation to orographically-induced regional circulations, Environ. Res. Lett., 2009, 4, 045203, doi:10.1088/1748-9326/4/4/045203.
[13]Liu X.D., L.B. Yan, P. Yang, Z.-Y. Yin, and G.R. North, 2011: Influence of Indian summer monsoon on aerosol loading in East Asia, Journal of Applied Meteorology and Climatology, 50 (3), 523-533.
[14]Liu X.D., X.N. Xie, Z.-Y. Yin, C.H. Liu, A. Gettelman, 2011: A modeling study of the effects of aerosols on clouds and precipitation over East Asia, Theoretical and Applied Climatology, 106, DOI 10.1007/ s00704-011-0436-6.
[15]Liu X.D. and Y. Wang, 2011: Contrasting impacts of spring thermal conditions over Tibetan Plateau on late-spring to early-summer precipitation in Southeast China, Atmospheric Science Letters, 12, DOI: 10.1002/asl.343.
[16]Shi ZG, XD Liu*, ZS An, BQ Yi, P Yang, N Mahowald, 2011: Simulated variations of eolian dust from inner Asian deserts during late Pliocene-Pleistocene periods, Climate Dynamics, 37, 2289-2301.
[17]Liu XD, SG Ding, L Bi, and P Yang, 2012: On the use of scattering kernels in the calculation of the bulk optical properties of ice clouds, Journal of Atmospheric and Oceanic Technology, 29(1). 50-63.
[18]Liu XD and BW Dong, 2013: Influence of the Tibetan Plateau uplift on the Asian monsoon-arid environment evolution, Chinese Science Bulletin, 58(34), 4277-4291.
[19]Li XZ, XD Liu*, LJ Qiu, ZS An and Z-Y Yin, 2013: Transient Simulation of Orbital-scale Precipitation Variation in Monsoonal East Asia and Arid Central Asia during the Last 150ka, J. Geophys. Res., 118, 7481–7488.
[20]Yin ZY, Wang HL, Liu XD, 2014: A Comparative Study on Precipitation Climatology and Interannual Variability in Subtropical East Asia and Central Asia, Journal of Climate, 27, 7830-7848
[21]Liu XD, H Sun, YF Miao, BW Dong and Z-Y Yin, 2015: Impacts of uplift of northern Tibetan Plateau and formation of Asian inland deserts on regional climate and environment, Quaternary Science Reviews, 116, 1−14.
[22]Liu XD, Y Hui, Z-Y Yin, ZS Wang, XN Xie, JG Fang, 2015: Deteriorating haze situation and the severe haze episode during December 18-25 of 2013 in Xi’an, China, the worst event on record, Theor. Appl. Climatol., DOI 10.1007/s00704-015-1509-8.
[23]Liu XD, QC Guo, ZT Guo, Z-Y Yin, B Dong and R Smith, 2015: Where were the monsoon regions and arid zones in Asia prior to the Tibetan Plateau uplift, National Science Review, 2(4), 403-416
[24]Xie XN and Liu XD, 2015: Aerosol-cloud-precipitation interactions in WRF Model: Sensitivity to autoconversion parameterization, Journal of Meteorological Research, 29(1), 72-81
[25]Sun Hui and Xiaodong Liu, 2015: Numerical simulation of the direct radiative effects of dust aerosol on the East Asian winter monsoon, Advances in Meteorology, 142617, doi:http://dx.doi.org/10.1155/2015/142617.
[26]Sun YB, ZS An, J Kutzbach, S Clemens, ZY Liu, WG Liu, XD Liu, ZG Shi, WP Zheng, LJ Liang, Y Yan, Y Li, 2015: Impacts of Insolation, Ice and CO2 on Asian Hydrological Change, Quaternary Science Reviews, 115, 132-142.
[27]Pepin N. R., S. Bradley, H. F. Diaz, M. Baraer, E. B. Caceres, N. Forsythe, H. Fowler, G. Greenwood, M. Z. Hashmi, X. D. Liu, J. R. Miller, L. Ning, A. Ohmura, E. Palazzi, I. Rangwala, W. Schöner, I. Severskiy, M. Shahgedanova, M. B. Wang, S. N. Williamson and D. Q. Yang, 2015: Elevation-dependent warming in mountain regions of the world, Nature Climate change, 5, 424-430.
[28]Wang HL, Xie XN, Liu XD, 2015: On the robustness of the weakening effect of anthropogenic aerosols on the East Asian summer monsoon with multi-models results, Advances in Meteorology, 2015, 397395, doi:http://dx.doi.org/10.1155/2015/397395.
[29]Shi ZG, XD Liu, YM Liu, YY Sha & TT Xu, 2015: Impact of Mongolian Plateau versus Tibetan Plateau on the westerly jet over North Pacific, Clim Dyn, 44: 3067–3076.
[30]Sha YY, ZG Shi, XD Liu, and ZS An, 2015: Distinct impacts of the Mongolian and Tibetan plateaus on the evolution of the East Asian monsoon, J. Geophys. Res., 120, 4764–4782.
[31]Li Xinzhou and Xiaodong Liu, 2015: Numerical simulation of Tibetan Plateau heating anomaly influence on westerly jet in spring, Journal of Earth System Science, 124, 1599-1607.
[32]Sun Hui and Xiaodong Liu, 2016: Numerical simulation of topography-modulated dust aerosol distribution and its influence on the onset of East Asian summer monsoon, Advances in Meteorology, 6951942, doi:http://dx.doi.org/10.1155/2016/6951942.
[33]Pan ZT, YJ Zhang, XD Liu, and ZQ Gao, 2016: Current and Future Precipitation Extremes over Mississippi and Yangtze River Basins as Simulated in CMIP5 Models, Journal of Earth Science, 27(1), 22-36.
[34]Wang ZS, XD Liu and XN Xie, 2016: Effects of strong East Asian cold surges on improving the air quality over mainland China, Atmosphere, 7(3), 38, doi:10.3390/atmos7030038.
[35]Qiu LJ and XD Liu, 2016: Sensitivity analysis of modelled responses of vegetation dynamics on the Tibetan Plateau to doubled CO2 and associated climate change, Theoretical and Applied Climatology, 124:229–239, doi: 10.1007/s00704-015-1414-1.
[36]Yan LB, ZY Liu, GS Chen, JE Kutzbach and XD Liu, 2016: Mechanisms of elevation-dependent warming over the Tibetan plateau in quadrupled CO2 experiments, Climatic Change, 135: 509–519.
[37]Li XZ, Pan ZT, Liu XD, 2016: Numerical simulation of influence of Tibetan Plateau uplift on winter dust cycle in Asian arid regions, Environmental Earth Sciences, 75, 601, doi: 10.1007/s12665-016-5403-1.
[38]Miao XD, H Wang, PR Hanson, JA Mason, XD Liu, 2016: A new method to constrain soil development time using both OSL and radiocarbon dating, Geoderma, 261, 93–100
[39]Ao H, AP Roberts, MJ Dekkers, XD Liu, EJ Rohling, ZG Shi, ZS An, X Zhao, 2016: Late Miocene–Pliocene Asian monsoon intensification linked to Antarctic ice-sheet growth, Earth Planet. Sci. Lett., 444, 75-87.
[40]Liu XD, Y Hui, Z-Y Yin, ZS Wang, XN Xie, JG Fang, 2016: Deteriorating haze situation and the severe haze episode during December 18-25 of 2013 in Xi’an, China, the worst event on record, Theoretical and Applied Climatology, 125: 321–335. doi: 10.1007/s00704-015-1509-8.
[41]Xie, X., H. Wang, X. Liu, J. Li, Z. Wang, and Y. Liu, 2016: Distinct effects of anthropogenic aerosols on the East Asian summer monsoon between multidecadal strong and weak monsoon stages, J. Geophys. Res. Atmos., 121, 7026–7040. doi:10.1002/2015JD024228.
[42]Dong BW, RT Sutton, W Chen, XD Liu, RY Lu, and Y Sun, 2016: Understanding abrupt summer warming and change in temperature extremes over Northeast Asia since the mid-1990s, Adv. Atmos. Sci., 33(9), 1005-1023.
[43]Xie Xiaoning, Xiaodong Liu, Hongli Wang and Zhaosheng Wang, 2016: Effects of aerosols on radiative forcing and climate over East Asia with different SO2 emissions, Atmosphere, 7(8), 99, doi: 10.3390/atmos7080099
[44]Feng, X., Liu, C., Fan, G., Liu, X., and Feng, C., 2016: Climatology and structures of southwest vortices in NCEP climate forecast system reanalysis. Journal of Climate, 29, 7675-7701.
[45]Liu Xiaodong, Buwen Dong, Zhi-Yong Yin, Robin S. Smith and Qingchun Guo, 2017: Continental drift and plateau uplift control origination and evolution of Asian and Australian monsoons, Sci. Rep. 7, 40344, doi: 10.1038/srep40344.
[46]Peng Y, XD Liu, J Dai, Z Wang, ZP Dong, Y Dong, XM Li, N Zhao, C Fan, C Chen, 2017: Aerosol size distribution and new particle formation events in the suburb of Xi’an, northwest China, Atmos. Environ., 153, 194-205.
[47]Qiu LJ, XD Liu, YQ Hao, 2017: Quantitative assessment of the role of doubled CO2 and associated climate change in the vegetation dynamics and hydrological cycle in the Sino-Mongolia arid and semi-arid region, Stochastic Environmental Research and Risk Assessment, 31: 785–797.
[48]Shi ZG, YY Sha and XD Liu, 2017: Effect of Yunnan-Guizhou topography at the southeastern Tibetan Plateau on the Indian monsoon, J. Climate, 30(4), 1259–1272.
[49]Xie X. N., H. Zhang, X. D. Liu, Y. R. Peng, and Y. Liu, 2017: New cloud parameterization with relative dispersion in CAM5.1: model evaluation and impacts on aerosol indirect effects, Atmos. Chem. Phys. Atmos. Chem. Phys., 17, 5877–5892.
[50]Liu Xiaodong, Buwen Dong, Zhi-Yong Yin, Robin S. Smith and Qingchun Guo, 2017: Continental drift and plateau uplift control origination and evolution of Asian and Australian monsoons, Sci. Rep. 7, 40344, doi: 10.1038/srep40344.
[51]Peng Y, XD Liu, J Dai, Z Wang, ZP Dong, Y Dong, XM Li, N Zhao, C Fan, C Chen, 2017: Aerosol size distribution and new particle formation events in the suburb of Xi’an, northwest China, Atmos. Environ., 153, 194-205.
[52]Qiu LJ, XD Liu, YQ Hao, 2017: Quantitative assessment of the role of doubled CO2 and associated climate change in the vegetation dynamics and hydrological cycle in the Sino-Mongolia arid and semi-arid region, Stochastic Environmental Research and Risk Assessment, 31: 785–797.
[53]Liu H, XD Liu, BW Dong, 2017: Intraseasonal variability of winter precipitation over central Asia and the western Tibetan plateau from 1979 to 2013 and its relationship with the North Atlantic Oscillation, Dynamics of Atmospheres and Oceans, 79, 31-42.
[54]Liu Xiaodong and Libin Yan, 2017: Elevation dependent climate change in the Tibetan Plateau, Oxford Research Encyclopedia of Climate Science, doi: 10.1093/acrefore/9780190228620.013.593.
[55]Li Xinzhou, Xiaodong Liu, Hongli Zhao, 2017: Transient simulation of the Tibetan Plateau modulated distinct orbital-scale precipitation variation in East and South Asia, Palaeogeography, Palaeoclimatology, Palaeoecology, 485, 899-905.
[56]Zheng YH, RD Pancost, XD Liu, ZZ Wang, BDA Naafs, XX Xie, Z Liu, XF Yu, H Yang, 2017, Atmospheric connections with the North Atlantic enhanced the deglacial warming in northeast China, Geology, 45, 1031-1034. doi:10.1130/G39401.1
[57]Sun Hui, Xiaodong Liu and Zaitao Pan, 2017: Direct radiative effects of dust aerosols emitted from the Tibetan Plateau on the East Asian summer monsoon – a regional climate model simulation, Atmos. Chem. Phys., 17, 13731–13745.
[58]Yan Peng, Yan Dong, Xingmin Li, Xiaodong Liu, Jin Dai, Chuang Chen, Zipeng Dong, Chuanli Du, Zhaosheng Wang, 2017: Different characteristics of new particle formation events at two suburban sites in northern China, Atmosphere, 8, 258, doi:10.3390/atmos8120258
[59]Xie XN, H Zhang, XD Liu, YR Peng, and YG Liu, 2018: Role of microphysical parameterizations with droplet relative dispersion in IAP AGCM 4.1, Advances in Atmospheric Sciences, 35(2), 248-259.
[60]Xie XN, XD Liu, HZ Che, XX Xie, HL Wang, JD Li, ZG Shi, YG Liu, 2018: Modeling East Asian dust and its radiative feedbacks in CAM4-BAM, Journal of Geophysical Research: Atmospheres, 123, 1079–1096..
[61]Ao H, MJ Dekkers, AP Roberts, EJ Rohling, ZS An, XD Liu, ZX Jiang, H Chang, XK Qiang, Y Xu, 2018: Mineral magnetic record of the Miocene-Pliocene climate transition on the Chinese Loess Plateau, North China, Quaternary Research, 89(3), 619-628
[62]Liu H, XD Liu and BW Dong, 2018: Influence of Central Siberian snow-albedo feedback on the East Asian spring dust cycle and connection with the preceding winter Arctic Oscillation, J. Geophys. Res. Atmos., 123, 13368–13385.
[63Liu XD, BW Dong, ZY Yin, RS Smith and QC Guo, 2019: Continental Drift, Plateau Uplift, and the Evolutions of Monsoon and Arid Regions in Asia, Africa, and Australia during the Cenozoic, Sci. China: Earth Sci., 62, 1053-1075
[64]Wang ZS, M Huang, R Wang, SQ Wang, XD Liu, XN Xie, ZJ Liu, H Gong, M Hao, 2019: Global NDVI patterns in response to atmospheric water vapor anomalies over the Indo-Pacific warm pool during Apr-May-June, Journal of Climate, 32(4), 1167–1180.
[65]Shi ZG, XN Xie, XZ Li, L Yang, XX Xie, J Lei, YY Sha, XD Liu, 2019: Snow-darkening versus direct radiative effects of mineral dust aerosol on the Indian summer monsoon: role of the Tibetan Plateau, Atmos. Chem. Phys., 19, 1605-1622.
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