温度扰动对水分动力学的影响

IF 1.1 Q3 PHYSICS, MULTIDISCIPLINARY Journal of Physics Communications Pub Date : 2024-03-13 DOI:10.1088/2399-6528/ad335e
Admasu Abawari, Yitagesu Elfaged
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引用次数: 0

摘要

考虑到饱和现象,我们分析了温度对大气中水分含量的扰动效应。饱和大气的气团由干燥的空气、水汽、云和雨水组成,它们在旋转的地球上流动,在北纬 9o1′48",东经 38o44′24",距地球表面 6.324km 处产生温度扰动。该饱和潮湿空气的基本大气参数被视为与温度有关,数值计算中未考虑降水和云水对其施加的压力。在这项拟议的研究中,沿纵向、经向和垂直方向的风速初始值随海拔高度的变化而变化,并且没有忽略大气与地球表面的相互作用。研究结果表明,大气变量的单一对流层扰动是不同长周期波型(350 小时)传播的主要因素,这种大气振荡在大气不同部分之间传递能量、动量和质量方面发挥着至关重要的作用,对全球气候系统产生影响。
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Influence of temperature perturbation on moisture dynamics
We analyzed the perturbation effect of temperature on the moisture content in the atmosphere,considering the saturation phenomenon. The air parcels of a saturated atmosphere are made of dry air, vapor, cloud, and rain water that flow on a rotating Earth, with a temperature perturbations induced at 9o1′48”N, 38o44′24”E and 6.324km above the Earth’s surface. The fundamental atmospheric parameter of this saturated moist air was treated as temperature-dependent, and the pressure force exerted on it by the precipitation and cloud water is not considered in the numerical computation. In this proposed research, the initial value of wind speed along zonal, meridional, and vertical directions varies with elevation, and the interaction of the atmosphere with the Earth’s surface is not neglected. The result of the investigation revealed that a single tropospheric disturbance of an atmospheric variable is a major factor in the spread of different long period waves patterns (350 hours) and this atmospheric oscillations play a crucial role in transferring energy, momentum, and mass across different parts of the atmosphere, impacting global climate systems.
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来源期刊
Journal of Physics Communications
Journal of Physics Communications PHYSICS, MULTIDISCIPLINARY-
CiteScore
2.60
自引率
0.00%
发文量
114
审稿时长
10 weeks
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