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1 期                     刘成瀚等:长白山南部暴雨的环流前兆和复杂地形作用研究                                         163
                  指标及其与灾情的关系研究[J]. 气象与环境科学, 44(5): 33-              Rainstorm Process and its Relationship with Disasters in Sichuan
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                     Study on Circulation Precursors and Complex Topographic Effects of

                          the torrential rain events in the South of Changbai Mountains


                        LIU Chenghan 1, 2, 3, 4 , LU Jinglong , YAN Qi , WANG Yue , JIAO Haoran , Jin Yan 6
                                                                              4, 5
                                                                                            2
                                                      2, 3
                                                                2, 3
                            (1. China Meteorological Administration Hydro-Meteorology Key Laboratory, Beijing  100081, China;
                                     2. Liaoning Meteorological Observatory, Shenyang  110166, Liaoning, China;
                         3. Institute of Atmosphere Environment, China Meteorological Administration, Shenyang  110166, Liaoning, China;
                                      4. Panjin National Climate Observatory, Panjin  124000, Liaoning, China;
                                    5. Shenyang District Meteorological Bureau, Shenyang  110166, Liaoning, China;
                                          6. Shanghai Meteorological Center, Shanghai  200030, China)

               Abstract: Based on the observed precipitation data from 2010 to 2019 in the complex terrain region of southeast‐
               ern Liaoning, this study identified 44 torrential rain events (TRECT). By employing composite analysis methods
               and decomposing the lower-level wind field using flow-over and flow-around equations, the circulation precur‐
               sors, common characteristics of circulation fields, and the dynamic impact mechanism·s of topography on re‐
               gional torrential rain were systematically investigated. The results indicate that: Six days prior to the occurrence
               of TRECT events, the mid-troposphere over the Eurasian continent exhibited a blocking high pattern, followed
               by the eastward movement and development of a shallow trough near Lake Baikal. On the day of the event, the
               subtropical high moved northward and intensified, forming a slanting trough over the western part of the key ar‐
               ea, with a closed cyclonic circulation appearing in the lower troposphere. The North China low-pressure system
               developed and moved eastward, positioning the key area at the top of the inverted trough, providing a favorable
               circulation  background  for  widespread  precipitation. During  the  peak  period  of  the  event,  the  flow  over  and
               around the terrain in the key area showed stronger southern and weaker northern characteristics, with high-value
               areas concentrated in the trumpet-shaped terrain region of the Changbai Mountain's foothills. Areas with flow-
               over speeds exceeding 4 m⋅s  were located on the southern slopes of the low-altitude hills in the trumpet-shaped
                                       -1
               area,  while  flow-around  was  observed  around  the  high-altitude  mountains,  with  meridional  branches  of  both
               flows playing a dominant role. The flow-over and flow-around entered the trumpet-shaped area by crossing and
               bypassing the mountains, respectively, primarily from two air stream·s originating from the Yellow Sea and the
               Korean Peninsula. In the trumpet-shaped area, the upward motion contributed by the flow-over accounted for
               more than 80% of the total system's upward motion, serving as the main dynamic source for precipitation en‐
               hancement. The flow-around, under the influence of topography, formed local positive vorticity, further enhanc‐
               ing the dynamic conditions for precipitation. This study systematically investigates the evolutionary characteris‐
               tics of precursor large-scale circulation system·s associated with torrential rain events in the complex topography
               of the Changbai Mountain foothills, exploring atmospheric circulation precursors preceding extreme precipita‐
               tion. Through mesoscale topographic dynamic forcing mechanism·s, it specifically elucidates the orographic lift‐
               ing-convergence effect and flow-around vorticity development within the trumpet-shaped terrain of southeastern
               Liaoning Province. It provides a theoretical basis for improving the accuracy of regional mountain type rainstorm
               forecast.
               Key words: complex topographic; torrential rain; circulation precursors; flow over; flow around
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