A copy of this work was available on the public web and has been preserved in the Wayback Machine. The capture dates from 2022; you can also visit the original URL.
The file type is
Quantitative attribution of vertical motion responsible for summer heavy rainfall over North China
Journal of Geophysical Research - Atmospheres
Some studies have investigated the dynamic and thermodynamic contributions to the heavy rainfall over NC in terms of the moisture budget. Zhao, Xu, Zhao, and Yang (2019) considered the moisture paths and topography and demonstrated that during the summer monsoon phase, the Tibetan Plateau and its extended topography can affect the moisture transport channels. Moisture is transported to the NC region at lower levels along the east anddoi:10.1029/2021jd035765 fatcat:gb5p4cjbdzaa3jtd3wj4eit734