According to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC, 2013), global mean surface temperature shows warming of 0.85 °C during 1880–2012. However, the TP has warmed much more rapidly. In situ observations, reanalyses and climate models show a clear amplification of the warming rate over the TP in recent decades.
Some important works in this context are highlighted below. For your reference:
Tan, X., Zhenni, W., Xingmin, M., Peng, G., Guangju, Z., Wenyi, S., Chaojun, G., 2019.
Spatiotemporal changes in snow cover over China during 1960–2013. Atmos. Res. 218, 183–194.
Smith, T., Bookhagen, B., 2018. Changes in seasonal snow water equivalent distribution in High Mountain Asia (1987 to 2009). Sci. Adv. 4 (1), e1701550. https://doi.org/10.1126/sciadv.1701550
Zhu, Y., Liu, H., Ding, Y., Zhang, F., Li, W., 2015. Interdecadal variation of spring snow depth over the Tibetan Plateau and its influence on summer rainfall over East China in the recent 30 years. Int. J. Climatol. 35 (12), 3654–3660.
Wang, Z., Wu, R., Zhao, P., Yao, S.-L., Jia, X., 2019. Formation of snow cover anomalies over the Tibetan Plateau in cold seasons. J. Geophys. Res. 124 (9), 4873–4890. https://doi.org/10.1029/2018JD029525.
Wang, X., Wu, C., Wang, H., Gonsamo, A., Liu, Z., 2017b. No evidence of widespread decline of snow cover on the Tibetan Plateau over 2000–2015. Sci. Rep. 7 (1), 14645. https://doi.org/10.1038/s41598-017-15208-9.
Wang, Z., Wu, R., Huang, G., 2017c. Low-frequency snow changes over the Tibetan
Plateau. Int. J. Climatol. 38 (2), 949–963. https://doi.org/10.1002/joc.5221.
Wang, A., Xu, L., Kong, X., 2018a. Assessments of the Northern Hemisphere snow cover response to 1.5 and 2.0 °C warming. Earth Syst. Dynam. 9 (2), 865–877. https://doi. org/10.5194/esd-9-865-2018.
Pu, Z.X., Xu, L., 2009. MODIS/Terra observed snow cover over the Tibet Plateau: distribution, variation and possible connection with the East Asian Summer Monsoon (EASM). Theor. Appl. Climatol. 97 (3–4), 265–278. https://doi.org/10.1007/s00704- 008-0074-9.
Pu, Z.X., Xu, L., Salomonson, V.V., 2007. MODIS/Terra observed seasonal variations of snow cover over the Tibetan Plateau. Geophys. Res. Lett. 34 (6), L06706.
Generally, the rainfall and temperature have a negative feedback effect on snow increasing. But to see the influence of snowfall in TP on extreme events in Africa, you may need to analyse the patterns and link them. This article may be a starting point for you. "Review of snow cover variation over the Tibetan Plateau and its influence on the broad climate system." Earth-Science Reviews 201 (2020): 103043.