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Wenhao Dong
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- Dong, W., M. Zhao, Y. Ming, V. Ramaswamy (2021). Representation of tropical mesoscale convective systems in a general circulation model: Climatology and response to global warming. J Climate, 34 (14): 5657-5671.
- Dong, W., Y. Ming, V. Ramaswamy (2020). Projected changes in Indian monsoon low-pressure system, J Climate, 33 (17): 7275–7287. [GFDL Research Highlights].
- Dong, W., Y. Lin, M. Zhang, & X. Huang (2020). Footprint of tropical mesoscale convective system variability on stratospheric water vapor, Geophys. Res. Lett., 47, e2019GL086320.
- Dong, W., Y. Lin, J. Wright et al. (2019). Precipitable water and CAPE dependence of rainfall intensities in China,Clim. Dyn., 52, 3357–3368.
- Dong, W., Y. Lin, J. Wright et al. (2018) Connections between a late summer snowstorm over the southwestern Tibetan Plateau and a concurrent Indian monsoon low pressure system, J. Geophys. Res. Atmos., 123 (24), 13,676–13,691.
- Dong, W., Y. Lin, J. Wright, Y. Ming et al. (2018). Regional disparities in summer rainfall changes over the arid eastern-Central Asia. Sci. Rep., 8, 13051, DOI:10.1038/s41598-018-31246-3.
- Lin, Y., Dong, W., M. Zhang et al. (2017): Causes of model dry and warm bias over central U.S. and impact on climate projections, Nat. Commun., 8, 881.
- Dong, W., Y. Lin, J. Wright et al. (2017): Monsoon low pressure systems feed up-and-over moisture transport to the southwestern Tibetan Plateau, J. Geophys. Res. Atmos., 122, 12140–12151.
- Dong, W., Y. Lin, J. Wright, Y. Ming et al. (2016): Summer rainfall over the southwestern Tibetan Plateau controlled by deep convection over the Indian subcontinent, Nat. Commun., 7, 10925.