Association Between Upstream Conditions and the Intensity of Orographic Precipitation in the Main Mountain Ranges of South Korea

IF 2.9 3区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Chia-Lun Tsai, Kwonil Kim, Heechul Park, Hongmok Park, Wonbae Bang, GyuWon Lee
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Abstract

This study uses high temporospatial surface precipitation rate obtained from radar observations (hybrid surface rainfall, HSR), 3D winds retrieved from the Wind Synthesis System using Doppler Measurements (WISSDOM), and 3D thermodynamic fields to investigate the association between orographic precipitation and upstream conditions for the main mountain ranges of South Korea during the 2018–2020. The main objective was to determine the dominate meteorological factors affecting the rain intensity over this terrain. Three rainfall cases were analyzed covering western, and eastern slopes of the Taebaek mountain range (TMR), Mt. Jiri, and Busan City. Correlation coefficients ( R $R$ ) were used to evaluate the strength of the relationship between rain intensity and meteorological factors in these regions, including the wind directions, wind speed, Froude number, saturated Froude number, water vapor, moist flux, stability, vertical velocity, and convergence. The results revealed that the wind direction determined the location of precipitation in the mountains, with the wind speed and moist flux identified as the most influential factors for rain intensity, with high correlation coefficients of 0.55–0.85. The upstream Froude number appeared to modulate the orographic enhancement on rain intensity over Mt. Jiri and the western slopes of the TMR. Low-level convergence was another critical factor affecting the rain intensity along the northeastern coast of South Korea (i.e., the eastern slopes of the TMR) and Busan ( R $R$ of ∼0.6–0.7). Statistical analysis of all orographic precipitation cases (52 cases over the 3 years) revealed that the upstream wind speed, and moist flux in the mid-layers had a higher correlation with rain intensity over the western slopes of the TMR and Mt. Jiri. The relationship between rain intensity and both water vapor and low-level convergence was also stronger along the northeastern coast of South Korea.

Abstract Image

韩国主要山脉上游条件与地形降水强度的关系
本研究利用雷达观测获得的高时空地表降水率(混合地表降水,HSR)、利用多普勒测量(WISSDOM)的风综合系统(Wind Synthesis System)获取的三维风以及三维热力学场,研究了2018-2020年韩国主要山脉地形降水与上游条件之间的关系。主要目的是确定影响该地形上降雨强度的主要气象因素。分析了太白山脉西坡、东坡、智异山、釜山市等3个地区的降雨情况。利用相关系数R$ R$评价降雨强度与风向、风速、弗劳德数、饱和弗劳德数、水汽、湿通量、稳定性、垂直速度、辐合等气象因子的关系强弱。结果表明:风向决定了降水在山区的位置,风速和湿通量是影响降雨强度的主要因素,相关系数为0.55 ~ 0.85;上游的弗劳德数似乎调节了日异山和TMR西坡的雨强地形增强。低辐合是影响韩国东北海岸(即TMR东坡)和釜山(R$ R$为~ 0.6-0.7)降雨强度的另一个关键因素。3年52次地形降水的统计分析表明,上游风速和中层湿通量与TMR西坡和智异山的降雨强度有较高的相关性。在韩国东北海岸,降雨强度与水汽和低层辐合的关系也更强。
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来源期刊
Earth and Space Science
Earth and Space Science Earth and Planetary Sciences-General Earth and Planetary Sciences
CiteScore
5.50
自引率
3.20%
发文量
285
审稿时长
19 weeks
期刊介绍: Marking AGU’s second new open access journal in the last 12 months, Earth and Space Science is the only journal that reflects the expansive range of science represented by AGU’s 62,000 members, including all of the Earth, planetary, and space sciences, and related fields in environmental science, geoengineering, space engineering, and biogeochemistry.
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