[1] Wang X., R. Lu, and X. Hong*, 2023: Weakening of the Silk Road Pattern in August after the Mid-1990s. J. Climate, 36, 4275–4286.

[2] Hong X.*, R. Lu, S. Chen, and S. Li, 2022: The relationship between the North Atlantic Oscillation and the Silk Road pattern in summer. J. Climate, 35, 6691–6702.

[3] Hong X.*, R. Lu, and S. Li, 2021: Interannual relationship between the West Asian and East Asian jet meridional displacements in summer. J. Climate, 34(2), 621–633.

[4] Wang X., R. Lu, and X. Hong*, 2021: Reduction of mid-summer rainfall in northern India after the late-1990s induced by the decadal change of the Silk Road pattern. Environ. Res. Lett., 16(10), 104051.

[5] Lu R., S. Hina, and X. Hong*, 2020: Upper- and lower-tropospheric circulation anomalies associated with interannual variation of Pakistan rainfall during summer. Adv. Atmos. Sci., 37(11), 1179–1190.

[6] Hong X.*, R. Lu, and S. Li, 2018: Differences in the Silk Road Pattern and its relationship to the North Atlantic Oscillation between early and late summers. J. Climate, 31(22), 9283–9292.

[7] Hong X.*, R. Lu, and S. Li, 2018: Asymmetric relationship between the meridional displacement of the Asian westerly jet and the Silk Road Pattern. Adv. Atmos. Sci., 35(4), 389–397.

[8] Hong X.*, S. Xue, R. Lu, and Y. Liu, 2018: Comparison between the interannual and decadal components of the Silk Road pattern. Atmos. Oceanic Sci. Lett., 11(3), 270–274.

[9] Hong X.*, R. Lu, and S. Li, 2017: Amplified summer warming in Europe-West Asia and Northeast Asia after the mid-1990s. Environ. Res. Lett., 12(9), 09400.

[10] Hong X., R. Lu*, 2016: The meridional displacement of the summer Asian jet, Silk Road Pattern, and tropical SST anomalies. J. Climate, 29(10), 3753–3766.

[11] Lu R.*, Hong X., and X. Li, 2016: Asymmetric association of rainfall and atmospheric circulation over East Asia with anomalous rainfall in the tropical western North Pacific in summer. Atmos. Oceanic Sci. Lett., 9(3), 185–190.

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