Abstract
The water vapor in the atmosphere is mainly formed through the vaporization of water from oceans, open land water sources, and transpiration through forests and agricultural crops. In the present study, our aim was to formulate a mathematical model to see the effect of transpiration from agricultural crops on rainfall. In the model formulation, it is assumed that clouds are formed in the atmosphere through the transpiration of agricultural crops proportional to the crops apart from the oceans and other sources (assumed constant). It is observed that in the presence of agriculture crops, the average rainfall increases. In the presence of clouds, cloud seeding techniques (use of conducive aerosols) are used to stimulate rainfall, which increases the agricultural crops with saturated type functional form. To capture the impact of environmental fluctuations, the stochastic version of the proposed model is also studied. The analysis of the model reveals that cloud seeding not only increases the rainfall, but it also increases the agricultural crops and clouds in the atmospheric environment.
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Acknowledgements
Amita Tripathi is thankful to University Grants Commission, New Delhi, India, for granting financial assistance to this research work (Ref. No 21/12/2014 (ii) EU-V).
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Appendices
Appendix A
Proof
Since the right-hand side of the Eq. (7) are locally Lipschitz continuous, hence system Eq. (7) possesses a unique local solution in \([-\tau , \tau _l]\), Now from the third equation of Eq. (7)
While from the first equation of model Eq. (7), \(\frac{dC_d(t)}{dt}\ge -\lambda _0 C_d(t), \ \ \forall \ t\ge -\tau ,\) which gives \(C_d(t)\ge C_d(-\tau ) e^{-\lambda _0t}>0.\) Similarly, the second equation of model Eq. (7) gives \(C_r\ge C_r(-\tau ) e^{-r_0 t}>0\).
Appendix B
Proof
Suppose that \((C_d(t), C_r(t), A(t))\) be a solution of the system Eq. (7) with initial conditions Eq. (8), then from the third equation of the system Eq. (7), we can write
Let \(M_1>\frac{(s^u+w^u)L}{s^l}\) then if \(A(0)<M_1,\) we have \(A(t)\le M_1\) \(\forall \ t\ge 0\). But if \(A(0)>M_1\), then \(-e_1=M_1(s+w^u-\frac{sM_1}{L^l})<0,\) so we have \(\frac{dA(t)}{dt}\le -e_1\). Therefore, there exists \(T_1>0\) such that \(A(t)\le M_1 \ \forall \ t\ge T_1.\) Let \(M_2>\frac{Q_d^u+\kappa ^u M_1}{\lambda _0}\) then from the first equation of Eq. (7)
So if \(C_d(0)<M_2,\) then \(C_d(t)\le M_2\) \(\forall \ t\ge T_1+\tau .\) In case \(C_d(0)>M_2\), \(\frac{dC_d(t)}{dt}<-e_2,\) where \(e_2=(Q_d^u+\kappa M_1 -\lambda _0 M_2),\) therefore there exists \(T_2>T_1+\tau ,\) such that \(C_d(t)\le M_2\)\(\forall t\ge T_2>T_1+\tau\). Similarly, we can show that there exists \(T_3>T_2>T_1+\tau ,\) such that \(C_r(t)\le M_3\) \(\forall\) \(t\ge T_3\), \(M_3>rM_2/r_0.\)
Now \(\frac{dC_d(t)}{dt}\ge Q_d^l-\lambda _0 C_d(t),\) let \(0<m_2< \frac{Q_d^l}{\lambda _0},\) then \(C_d(t)>\frac{Q_d^l}{\lambda _0}\) \(\forall t\ge T_4.\) Same way if \(m_3< \frac{r^lQ_d^l}{\lambda _0r_0},\) then there exists a \(T_5>0,\) such that \(C_r(t)>m_3\) \(\forall \ t \ge T_5\) and if \(m_1< \frac{\left( s^l+\frac{w^l m_3}{m+M_3}\right) L}{s^u},\) then there exists \(T_6>0,\) such that \(A(t)\ge m_1 \ \forall \ t\ge T_6.\)
Now to prove global stability Let \((C_d, C_r, A)\) and \((\tilde{C_d}, \tilde{C_r}, \tilde{A})\) be any two solutions of the system Eq. (7) with initial conditions Eq. (8). Define \(W_1(t)=\vert C_d(t)-\tilde{C}_d(t)\vert ,\) \(W_2(t)=\vert C_r(t)-\tilde{C}_r(t)\vert ,\) \(W_3(t)=\vert A(t)-\tilde{A}(t)\vert .\) The right upper derivative of \(W_1, \ W_2\) and \(W_3\) can be obtained as
Let \(W_4(t)=\int _{t-\tau }^t\kappa (u+\tau )\vert A(u)-\tilde{A}(u)\vert du,\) then
So if \(W=W_1+W_2+W_3+W_4,\) then
where \(C_1=\lambda _0-r_u,\) \(C_2=r_0-w^um_1\) and \(C_3=\frac{2m_1s^u}{L^l}\)\(-\kappa ^u-s^u-w^um.\) Thus for \(t\ge T,\) we get \(D^+W(t)\le -C_1\)\(\vert C_d(t)-\tilde{C}_d(t)\vert -C_2\vert C_r(t)-\tilde{C}_r(t)\vert -C_3\vert A(t)-\tilde{A}(t)\vert .\)
Integrating the above inequality from T to t, we have
Appendix C
Proof
By comparison theorem, the fourth equation of model Eq. (12) gives \(0\le A\le L\left( 1+\frac{w}{s}\right)\). Now we define a function \(V_4(x(t))=\sum _{i=1}^3x_i(t)\), then Itô’s formula gives
Multiplying by \(e^{\beta t}\) both sides, we get
Some algebraic manipulation gives
Let \(c=\min \{(\lambda _0-r-\phi -\beta ), (r_0-\beta ), (\delta _0-\beta )\}\), then
Therefore, \(\lim _{t\rightarrow \infty } EV_4(x(t))\le \frac{\left( Q_d+L\left( 1+\frac{w}{s}\right) \right) }{\beta }.\) Thus \(x_i\le \)\(\frac{\left( Q_d+L(1+\frac{w}{s})\right) }{\beta },\) for \(i=1,2,3\) and \(x_4\le L\left( 1+\frac{w}{s}\right) .\)
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Misra, A.K., Tripathi, A. Mathematical Models of how the Transpiration Affects Rainfall through Agriculture Crops. Environ Model Assess 26, 837–848 (2021). https://doi.org/10.1007/s10666-021-09769-3
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DOI: https://doi.org/10.1007/s10666-021-09769-3