Study finds gravity waves caused by complex terrain over the Tibetan Plateau can enhance the intensity of spring rainfall in East Asia
image: The breaking of orographic gravity waves induces a zonal wave drag in the middle troposphere, which destroys the geostrophic balance of the large-scale westerly flow and thus drives an ageostrophic meridional circulation across the Tibetan Plateau. The rising branch of the meridional circulation acts to lower the pressure and increase the meridional pressure gradient to the south of the Tibetan Plateau by dynamically pumping the lower-tropospheric air upwards. The southwesterly monsoonal flow on the southeastern flank of the Tibetan Plateau thus intensifies and transports more water vapor to East Asia, resulting in an enhancement of the springtime persistent rainfall.
Credit: ©Science China Press
The springtime persistent rainfall is the major rainy period before the onset of summer monsoon in East Asia. For example, it accounts for about 35% of the annual precipitation in South China, which brings plentiful water for agricultural and industrial use but can also cause heavy rainfall and flash flooding.
According to Xin Xu, an associate professor of Nanjing University, “Previous studies demonstrated great importance of the mechanical and thermal effects of the Tibetan Plateau large-scale orography on the formation of springtime persistent rainfall. However, the impact of small-scale orography over the Tibetan Plateau remains poorly understood.”
The team finds that the orographic gravity waves triggered by small-scale orography over the Tibetan Plateau contribute importantly to the spring rainfall in East Asia. The impact is even comparable to that of surface sensible heating of the Tibetan Plateau’s large-scale orography. The breaking of orographic gravity waves induces a zonal wave drag in the middle troposphere which destroys the geostrophic balance of the large-scale westerly flow and thus drives an ageostrophic meridional circulation across the Tibetan Plateau. The rising branch of the meridional circulation acts to lower the pressure and increase the meridional pressure gradient to the south of the Tibetan Plateau by dynamically pumping the lower-tropospheric air upwards. Consequently, the southwesterly monsoonal flow on the southeastern flank of the Tibetan Plateau intensifies and transports more water vapor to East Asia, resulting in an enhancement of the springtime persistent rainfall.
- This study proposes a new type of air pump, which is in analogy to the well-known thermal sensible heating air pump (i.e., SHAP) but driven dynamically by the orographic gravity wave drag over the Tibetan Plateau.
- It helps more completely understand the climatic effects of Tibetan Plateau’s multiscale orography, and provides a new perspective on the westerly-monsoon synergy in East Asia.
See the article:
Li R, Xu X, Xu X, Shepherd T G, Wang Y. 2023. Importance of orographic gravity waves over the Tibetan Plateau on the spring rainfall in East Asia.Science China Earth Sciences, 66(11): 2594–2602, https://doi.org/10.1007/s11430-023-1204-6