Modified Refractivity-Based Lifted Index Using Exact Formula for Lifted Condensation Level

IF 1 4区 工程技术 Q4 INSTRUMENTS & INSTRUMENTATION
MAPAN Pub Date : 2024-10-15 DOI:10.1007/s12647-024-00779-6
Festus Kehinde Adejumobi, Modupe E. Sanyaolu, Alexander A. Willoughby, Oluropo F. Dairo
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引用次数: 0

Abstract

Temperature is responsible for the rise of air parcels in the atmosphere, which in turn impairs the transmission of electromagnetic waves. Therefore, atmospheric stability is a function of the temperature of the rising and sinking air parcel with respect to the environmental air temperature at the lifted condensation level (LCL). Refractivity-based lifted index (RLI), a stability index model, uses an approximate LCL value. This study modifies the RLI using the exact formula of the LCL to obtain a precise modified refractivity-based lifted index (MRLI) model for the computation of refractivity-based atmospheric stability profiles. Two years (2020–2021) reanalysis data of atmospheric parameters (temperature, relative humidity and atmospheric pressure) were obtained from European Centre for Medium-Range Weather Forecasts (ECMWF) satellite for Lagos (6.6018° N, 3.3515° E), Abuja (9.0765° N, 7.3986° E) and Yola (9.2095° N, 12.4782° E) at 500–1000 hPa. RLI and MRLI were analysed at four synoptic hours (0, 6, 12, and 18 h) Local Time (LT). The trend shows that when RLI is negative, MRLI is negative; when RLI becomes less negative, MRLI is less negative, except in some cases where a significant amount of water vapour is observed at 500 hPa. Furthermore, a higher negative MRLI value indicates more environmental moisture and is supportive of convective activity, which implies an unstable atmosphere. MRLI has higher night-time (18–0 h LT) values compared to the daytime (6–12 h LT) due to low temperature and high humidity. Also, MRLI negative value decreases as the altitude increases with seasonal averages of − 97, − 86, and − 83 N-units over Lagos, Abuja, and Yola, respectively. A strong positive relationship was observed between MRLI and RLI, with correlation coefficients of 0.99999 for Lagos, 0.99823 for Abuja, and 0.99765 for Yola. MRLI attempts to lower the approximation error exhibited by RLI values for dry season months over Abuja and Yola.

基于折射率的修正提升指数,使用提升凝结水平的精确公式
温度会导致大气中的气团上升,进而影响电磁波的传输。因此,大气稳定性是上升和下沉气团的温度与抬升凝结水平(LCL)处环境空气温度的函数。基于折射率的抬升指数(RLI)是一种稳定指数模型,它使用近似的 LCL 值。本研究利用 LCL 的精确公式对 RLI 进行了修改,从而获得了精确的修改折射率升力指数(MRLI)模型,用于计算基于折射率的大气稳定性剖面。从欧洲中期天气预报中心(ECMWF)卫星获取了拉各斯(北纬 6.6018°,东经 3.3515°)、阿布贾(北纬 9.0765°,东经 7.3986°)和约拉(北纬 9.2095°,东经 12.4782°)500-1000 百帕的两年(2020-2021 年)大气参数(温度、相对湿度和大气压力)再分析数据。在当地时间(LT)的四个同步小时(0、6、12 和 18 小时)分析了 RLI 和 MRLI。趋势表明,当 RLI 为负值时,MRLI 也为负值;当 RLI 变为较小的负值时,MRLI 的负值也较小,除非在某些情况下,在 500 hPa 观测到大量水汽。此外,较高的 MRLI 负值表明环境湿度较大,有利于对流活动,这意味着大气层不稳定。由于低温和高湿度,夜间(18-0 h LT)的 MRLI 值比白天(6-12 h LT)高。此外,MRLI 的负值随着海拔的升高而降低,拉各斯、阿布贾和约拉的季节平均值分别为-97、-86 和 -83N-单位。在 MRLI 和 RLI 之间观察到了很强的正相关关系,拉各斯的相关系数为 0.99999,阿布贾为 0.99823,而约拉为 0.99765。MRLI 试图降低阿布贾和约拉旱季月份的 RLI 值所显示的近似误差。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
MAPAN
MAPAN 工程技术-物理:应用
CiteScore
2.30
自引率
20.00%
发文量
91
审稿时长
3 months
期刊介绍: MAPAN-Journal Metrology Society of India is a quarterly publication. It is exclusively devoted to Metrology (Scientific, Industrial or Legal). It has been fulfilling an important need of Metrologists and particularly of quality practitioners by publishing exclusive articles on scientific, industrial and legal metrology. The journal publishes research communication or technical articles of current interest in measurement science; original work, tutorial or survey papers in any metrology related area; reviews and analytical studies in metrology; case studies on reliability, uncertainty in measurements; and reports and results of intercomparison and proficiency testing.
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