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首页> 外文期刊>Advances in Meteorology >Easterly Wave Disturbances over Northeast Brazil: An Observational Analysis
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Easterly Wave Disturbances over Northeast Brazil: An Observational Analysis

机译:巴西东北部的东风波扰动:观测分析

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This paper aims to identify the circulation associated with Easterly Wave Disturbances (EWDs) that propagate toward the Eastern Northeast Brazil (ENEB) and their impact on the rainfall over ENEB during 2006 and 2007 rainy seasons (April-July). The EWDs identification and trajectory are analyzed using an automatic tracking technique (TracKH). The EWDs circulation patterns and their main features were obtained using the composite technique. To evaluate the TracKH efficiency, a validation was done by comparing the EWDs number tracked against observed cases obtained from an observational analysis. The mean characteristics of EWDs are 5.5-day period, propagation speed of similar to 9.5 m.s(-1), and a 4500 km wavelength. A synoptic analysis shows that between days -2 d and 0 d, the low level winds presented cyclonic relative vorticity and convergence anomalies both in 2006 and 2007. The EWDs signals are strongest at low levels. The EWDs propagation is associated with relative humidity and precipitation positive anomalies and OLR and omega negative anomalies. The EWDs tracks are seen over all ENEB and their lysis occurs between the ENEB and marginally inside the continent. The tracking captured 71% of EWDs in all periods, indicating that an objective analysis is a promising method for EWDs detection.
机译:本文旨在确定与2006年和2007年雨季(4月至7月)向巴西东北部(ENEB)传播的东风波扰动(EWD)相关的环流及其对ENEB上方降雨的影响。使用自动跟踪技术(TracKH)分析EWD的识别和轨迹。利用复合技术获得了EWD的循环模式及其主要特征。为了评估TracKH效率,通过将跟踪的EWD数量与从观察分析中获得的观察病例进行比较来进行验证。 EWD的平均特征为5.5天,传播速度类似于9.5 m.s(-1),波长为4500 km。概要分析表明,在-2 d和0 d之间,低水平风在2006年和2007年均表现为气旋相对涡度和会聚异常。EWD信号在低水平时最强。 EWD的传播与相对湿度和降水正异常,OLR和ω负异常有关。在所有ENEB上都可以看到EWD轨迹,并且它们的裂解发生在ENEB之间以及大陆内部的边缘。跟踪在所有期间都捕获了71%的EWD,这表明客观分析是一种有前途的EWD检测方法。

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