Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
8864678 | Atmospheric Research | 2018 | 55 Pages |
Abstract
A severe squall line that occurred in east China on 12 July 2014 was simulated using the Weather Research and Forecasting model. Based on the cloud-resolving simulation results, the structural features and propagation mechanisms of the squall line were analyzed in detail. The main results were as follows: (1) The dynamic and thermodynamic structures of the simulated squall line were mainly characterized by a rain-induced cold pool in the near-ground level, front inflow in the low levels, descending rear inflow in the middle levels, and slightly ascending front-to-rear outflow in the upper levels. (2) The coupling between the low-level updrafts induced by the cold pool and the upper-level updrafts caused by the gravity wave was the main reason for the development and propagation of the squall line. (3) The descending mid-level rear inflow cut off the front inflow in the low levels and eventually resulted in the squall line's decay. Based on these findings, a conceptual model of the initial, mature and dissipating stages of the squall line is presented.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Atmospheric Science
Authors
Lei Yin, Fan Ping, Jiahua Mao,