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首页> 外文期刊>ournal of the Meteorological Society of Japan >Characteristics of Low-level Jets in Shanghai during the 2008-2009 Warm Seasons as Inferred from Wind Profiler Radar Data
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Characteristics of Low-level Jets in Shanghai during the 2008-2009 Warm Seasons as Inferred from Wind Profiler Radar Data

机译:从Wind Profiler雷达数据推断的2008-2009暖季期间上海低空喷气机的特征

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In order to understand the characteristics of low-level jets (LLJs) over coastal areas of China Continent and its linkages with rainfall during the warm seasons, half-hourly data from a wind profiler radar (WPR) at the Qingpu site during the Meiyu periods of 2008 and 2009 in addition to data from one month prior to and after (non-Meiyu periods) were used to develop a climatology of the LLJs over Shanghai, China. Two peaks in LLJ incidence were revealed at 500-800 m and 2100-2200 m altitudes. Thus, we classified the observed LLJs into two types: (1) boundary-layer jets (BLJs, below 1 km) and (2) synoptic-system-related LLJs (SLLJs, within 1-3 km). BLJs and SLJs showed different behavior in their temporal variation of the occurrence frequency, wind direction, and relation to rainfall. The BLJs displayed a more evident diurnal cycle than the SLLJs, with maximum incidence occurring in nighttime and early morning. The SLLJs occurred more frequently during Meiyu periods than non-Meiyu periods, whereas the occurrence frequency of BLJs increased throughout the warm seasons with no peak during Meiyu periods. BLJs are mostly southerly winds that might be induced by inertial oscillation with a strong background southerly geostrophic wind due to the west-east land-ocean thermal difference. SLLJs most frequently appeared as southwesterly and westerly winds embedded in the East Asian monsoon circulation. The relation between LLJs and precipitation was examined by comparing the frequency of LLJs occurrence on rainy days (cases), with daily (4-hourly) accumulated rainfall within 1 to 10 mm, and non-rainy days (cases) because the missing rate of WPR data is high during heavy rainfall events. Both BLJs and SLLJs occur more often on rainy days than on non-rainy days. In shorter time scales (4 hours), both BLJs and SLLJs tend to occur frequently during, before and after rainy cases, except SLLJs before rainy cases.
机译:为了了解中国大陆沿海地区低空急流(LLJ)的特征及其与暖季降雨的联系,在梅雨期青浦站风廓线雷达(WPR)的半小时数据除了使用2008年和2009年之前和之后一个月(非梅雨期)的数据外,还利用该数据开发了中国上海低空急流的气候。在500-800 m和2100-2200 m的高度处发现了LLJ发生率的两个峰值。因此,我们将观测到的低空急流分为两类:(1)边界层射流(BLJ,低于1 km)和(2)与天气系统有关的低空急流(SLLJ,在1-3 km之内)。 BLJ和SLJ在其出现频率,风向以及与降雨的关系的时间变化中表现出不同的行为。 BLJs比SLLJs表现出更明显的昼夜周期,最大的发生发生在夜间和清晨。在梅雨期SLLJs的发生频率要高于非梅雨期,而BLJs的出现频率在整个暖季都增加,梅雨期没有峰值。 BLJs主要是向南风,可能是由惯性振荡引起的,并且由于东西陆海温差而产生强烈的背景向南地转风。 SLLJs最经常出现在东亚季风环流中的西南风和西风中。通过比较LLJs在雨天(例),每天(4小时)累积降雨在1至10mm内和非雨天(例)中的LLJ发生频率,比较了LLJs的发生频率,从而检查了LLJs与降水的关系。在强降雨事件中,WPR数据较高。 BLJ和SLLJ都在雨天比在非雨天更频繁地发生。在较短的时间范围内(4小时),BLJ和SLLJ倾向于在雨天期间,之前和之后频繁发生,除了在雨天之前的SLLJ。

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