1. Zhang J, Tian W, Chipperfield M P, et al. Persistent shift of the Arctic polar vortex towards the Eurasian continent in recent decades[J]. Nature Climate Change, 2016, 6(12): 1094-1099.
2. Zhang J, Tian W, Pyle J A, et al. Responses of Arctic sea ice to stratospheric ozone depletion[J]. Science Bulletin, 2022, 67(11): 1182-1190.
3. Huang J, Tian W, Zhang J, et al. The connection between extreme stratospheric polar vortex events and tropospheric blockings[J]. Quarterly Journal of the Royal Meteorological Society, 2017, 143(703): 1148-1164.
4. Huang J, Hitchcock P, Maycock A C, et al. Northern hemisphere cold air outbreaks are more likely to be severe during weak polar vortex conditions[J]. Communications Earth & Environment, 2021, 2(1): 147.
5.Tian W, Chipperfield M P. A new coupled chemistry–climate model for the stratosphere: The importance of coupling for future O3‐climate predictions[J]. Quarterly Journal of the Royal Meteorological Society: A journal of the atmospheric sciences, applied meteorology and physical oceanography, 2005, 131(605): 281-303.
6. Tian W, Chipperfield M P, Lü D. Impact of increasing stratospheric water vapor on ozone depletion and temperature change[J]. Advances in Atmospheric Sciences, 2009, 26: 423-437.
7. Zhang J, Tian W, Xie F, et al. Stratospheric ozone loss over the Eurasian continent induced by the polar vortex shift[J]. Nature communications, 2018, 9(1): 206.
8. Tian W, Chipperfield M, Huang Q. Effects of the Tibetan Plateau on total column ozone distribution[J]. Tellus B: Chemical and Physical Meteorology, 2008, 60(4): 622-635.
9. Tian W, Chipperfield M P, Stevenson D S, et al. Effects of stratosphere‐troposphere chemistry coupling on tropospheric ozone[J]. Journal of Geophysical Research: Atmospheres, 2010, 115(D3).
10. Tian W, Chipperfield M P, Gray L J, et al. Quasi‐biennial oscillation and tracer distributions in a coupled chemistry‐climate model[J]. Journal of Geophysical Research: Atmospheres, 2006, 111(D20).