分数法大气内波模型的解析研究

IF 13 1区 工程技术 Q1 ENGINEERING, MARINE
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引用次数: 0

摘要

本研究探讨了发生在流体内部而非表面的大气内波(通常称为重力波)的数学模型。根据浅层流体假设,大气内波可以用非线性偏微分方程系统来描述。浅层流模型的主要概念是,波浪在垂直上升之前会在很大的水平范围内扩散。分数微分变换法(FRDTM)可用于为任何给定模型提供近似解。这有助于全球大气建模,在天气和气候预报中也有应用。对于整阶值(α=1),将 FRDTM 解法与精确解法、EADM 和 HAM 进行比较,以评估所建议技术的正确性和有效性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Analytical study of atmospheric internal waves model with fractional approach

This study looks at the mathematical model of internal atmospheric waves, often known as gravity waves, occurring inside a fluid rather than on the surface. Under the shallow-fluid assumption, internal atmospheric waves may be described by a nonlinear partial differential equation system. The shallow flow model’s primary concept is that the waves are spread out across a large horizontal area before rising vertically. The Fractional Reduced Differential Transform Method (FRDTM) is applied to provide approximate solutions for any given model. This aids in the modelling of the global atmosphere, which has applications in weather and climate forecasting. For the integer-order value (α=1), the FRDTM solution is compared to the precise solution, EADM, and HAM to assess the correctness and efficacy of the proposed technique.

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来源期刊
CiteScore
11.50
自引率
19.70%
发文量
224
审稿时长
29 days
期刊介绍: The Journal of Ocean Engineering and Science (JOES) serves as a platform for disseminating original research and advancements in the realm of ocean engineering and science. JOES encourages the submission of papers covering various aspects of ocean engineering and science.
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