Abstract
Rain is an important phenomenon occurring in nature. Nowadays, in some places across the world, less amount of rain is observed, which affects human population in several ways, like shortage of drinking water, less production from agriculture fields, increase in pollution level, etc. Keeping this point in view, in this paper, a mathematical model for making artificial rain is proposed and analyzed. In the modeling process, it is assumed that water vapors are continuously formed in the atmosphere and are not condensed enough to form clouds. Further, it is assumed that aerosols (mixture of two or more) are introduced in the atmosphere to increase the process of nucleation of cloud droplets from water vapors and changing them into raindrops. The qualitative analysis of the proposed model is presented using stability theory of differential equations. It is found that model exhibits only one nonnegative equilibrium. The sufficient conditions for stability of the equilibrium have been obtained. Numerical simulation is carried out to see the effect of key parameters on the process leading to rainfall.
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Acknowledgments
Author is thankful to the handling editor and both the referees for their useful suggestions. Author also thankfully acknowledges Dr. M.K. Bharty, Department of Chemistry, Institute of Science, BHU Varanasi for making discussions on the chemical properties of aerosols.
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Appendix
Appendix
1.1 1: Proof of Theorem 1
We linearize the system (1) about \(E^*\) by using the following transformations
Now consider the following positive definite function
(where \(m_1 , m_2 , m_3 \) are some positive constants to be chosen appropriately). Differentiating above equation with respect to t along the solutions of linearized system of (1), we get
Choosing \(m_2=m_1\frac{\pi _1\theta _1\lambda _2C_v^*}{\pi _2\lambda _1^2C_d^*}\) and \(m_3=m_1\frac{\pi _1\theta _1C_v^*}{\lambda _1C_h^*}\), \(\frac{dV}{dt}\)is simplified as:
Now \(\frac{dV}{dt}\) will be negative definite provided the conditions (11), (12) and (13) are satisfied.
1.2 2: Proof of Theorem 2
To prove this theorem we consider the following positive definite function about \(E^*\),
(where \(k_1 , k_2 , k_3 \) are some positive constants to be chosen appropriately). Differentiating above equation with respect to t along the solutions of system (1) and making simple algebraic manipulations, we get
Choosing \(k_2=k_1\frac{\pi _1\theta _1\lambda _2C_v^*}{\pi _2\lambda _1^2C_d^*}\) and \(k_3=k_1\frac{\pi _1\theta _1C_v^*}{\lambda _1C_h^*}\), \(\frac{dU}{dt}\)is simplified as
Now \(\frac{dU}{dt}\) will be negative definite inside the region of attraction provided the following conditions are satisfied:
From above inequalities (25), (26) and (27), we may choose \(k_1>0\) if the following condition is satisfied:
Here we have used the fact that \((\theta _0+\theta _1C_h^*)=Q_v/C_v^*\). Thus, the system (1) is globally stable inside the region of attraction if the conditions (14), (15) and (16) are satisfied.
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Misra, A.K. Effects of aerosols in making artificial rain: a modeling study. J Math Chem 54, 1596–1611 (2016). https://doi.org/10.1007/s10910-016-0639-2
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DOI: https://doi.org/10.1007/s10910-016-0639-2