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Enhancement mechanism of the 30 June 2006 precipitation system observed over the northwestern slope of Mt. Halla, Jeju Island, Korea

机译:2006年6月30日的降水系统的增强机制在山的西北斜坡上观察到。韩国济州岛汉拿市

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摘要

Doppler radar analysis and a cloud-resolving storm simulator (CReSS) are used to investigate the enhancement mechanism of a localized intense precipitation system that occurred over Jeju Island, Korea, on 30 June 2006. Rain gauge data revealed intensive rainfall (>80 mm in 100 min) over northwest of Jeju Island, and relatively low rainfall (≤20 mm) over the northeast of the island. The environment of the precipitation system consisted of near-saturated air (relative humidity (RH): ~95%) from the surface to 700 hPa and a low lifting condensation level of 951 hPa. Doppler radar analysis revealed enhancement of the precipitation system on the northwestern lateral side (in this study, the term 'lateral side' refers to the sides of the mountain other than the lee-side and windward side) of Mt Halla, the central mountain on the island (1950 m). In the region of enhancement, low-level convergence (7×10~(-4)s~(-1)) induced by orographic blocking with a relatively low Froude number (0.55) was observed. These observations were well simulated by a control run (CNTL) using CReSS. The simulated precipitation system was enhanced over the northwestern part of the island due to wind passing around Jeju Island, low-level convergence (1.6×10~(-3) s~(-1)) due to orographic blocking, and high RH (~95%). In order to clarify the influence of topography and the low-level moist environment on enhancement of the precipitation system, numerical sensitivity experiments were conducted. The NOTR (no terrain) experiment produced straightforward wind without low-level convergence over the topography. Associated with these features, the CNTL rainfall amount on the northwestern lateral side of the island was 30.6% more than that produced in NOTR. A comparison of RH-controlled experiments and CNTL revealed that increasing moisture in the low-level environment resulted in greater intensity of the precipitation system. A reduction in low-level RH by as little as 2% could result in a 20.8% reduction in rainfall amount Therefore, land areas with small, narrow, but steep topographic features, such as Jeju Island, could determine the intensity and location of the precipitation system under a moist environment during the rainy seasoa
机译:多普勒雷达分析和云解风暴模拟器(CReSS)用于调查2006年6月30日发生在韩国济州岛上的局部强降水系统的增强机制。雨量器数据显示强降雨(> 80 mm距济州岛西北部100分钟),岛东北部相对较低的降雨量(≤20毫米)。降水系统的环境包括从表面到700 hPa的近饱和空气(相对湿度(RH):〜95%)和951 hPa的低扬露水平。多普勒雷达分析表明,哈拉山(Mt Halla)的西北侧(本研究中,“侧”是指除背风侧和迎风侧以外的山的侧面)的降水系统得到了增强。岛(1950 m)。在增强区域中,观测到了由弗洛德数(0.55)相对较低的地形阻塞引起的低水平收敛(7×10〜(-4)s〜(-1))。通过使用CReSS的对照运行(CNTL),可以很好地模拟这些观察结果。由于风在济州岛周围绕行,地形阻塞造成的低水平会聚(1.6×10〜(-3)s〜(-1))和高RH( 〜95%)。为了阐明地形和低水平的潮湿环境对增强降水系统的影响,进行了数值敏感性实验。 NOTR(无地形)实验产生的风力直截了当,而地形没有低水平的收敛。与这些特征相关联,该岛西北侧的CNTL降水量比NOTR产生的降雨量高30.6%。 RH对照实验与CNTL的比较表明,低空环境中水分的增加导致降水系统的强度增加。低水平的RH降低2%可能会导致降雨量减少20.8%。因此,地形较小,狭窄但陡峭的地形地区(例如济州岛)可以确定该区域的强度和位置。雨海中潮湿环境下的降水系统

著录项

  • 来源
    《Atmospheric research》 |2010年第3期|P.343-358|共16页
  • 作者单位

    Dept. of Environmental Atmospheric Sciences, Pukyong National University, Republic of Korea;

    rnDept. of Storm, flood and landslide Research, National Research Institute for Earth Science and Disaster Prevention, Japan;

    rnDept. of Storm, flood and landslide Research, National Research Institute for Earth Science and Disaster Prevention, Japan;

    rnAtmospheric Environmental Research Institute, Pukyong National University, Republic of Korea;

    rnHydrospheric Atmospheric Research Center, Nagoya University, Japan;

    rnDept. of Environmental Atmospheric Sciences, Pukyong National University, Republic of Korea Atmospheric Environmental Research Institute, Pukyong National University, Republic of Korea #4310, Dept. of Environmental Atmospheric Sciences, Pukyong National University, 599-1, Nam-Gu, Busan, Republic of Korea;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    orographically-enhanced precipitation; moist environment; small topography;

    机译:地理上增强的降水;潮湿的环境小地形;
  • 入库时间 2022-08-18 03:36:07

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