Study of Brownian functionals for a Brownian process model of snow melt dynamics with purely time dependent drift and diffusion

• Published in: The European physical journal. B, Condensed matter physics Vol. 91; no. 11
• Main Authors: Dubey, Ashutosh, Bandyopadhyay, Malay
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.11.2018; Springer; Springer Nature B.V
• Subjects: Analysis; Aquatic resources; Asymptotic properties; Brownian motion; Complex Systems; Computer simulation; Condensed Matter Physics; Diffusion; Distribution (Probability theory); Distribution functions; Drift; Fluid- and Aerodynamics; Laws, regulations and rules; Mathematical analysis; Mathematical models; Numerical analysis; Physics; Physics and Astronomy; Power law; Predictions; Probability distribution functions; Probability distributions; Regular Article; Snowmelt; Solid State Physics; Stochastic processes; Time dependence; Water; Water resources; Statistical and Nonlinear Physics
• ISSN: 1434-6028; 1434-6036
• DOI: 10.1140/epjb/e2018-90222-6

In this paper, we investigate a Brownian motion (BM) with purely time dependent drift and diffusion by suggesting and examining several Brownian functionals, which characterize the stochastic model of water resources availability in snowmelt dominated regions with power law time dependent drift and diffusion. Snow melt process is modelled by a overdamped Langevin equation for a Brownian process with power law time dependent drift ( μ ( t ) ~ qkt α ) and diffusion ( D ( t ) ~ kt α ) where they are proportional to each other. We introduce several probability distribution functions (PDFs) associated with such time dependent BMs. For instance, with initial starting value of snow amount H 0 , we derive analytical expressions for: (i) the PDF P ( t f | H 0 ) of the first passage time t f which specify the lifetime of such stochastic process, (ii) the PDF P ( A | H 0 ) of the area A till the first passage time and it provides us numerous valuable information about the average available water resources, (iii) the PDF P ( M ) associated with the maximum amount of available water M of the BM process before the complete melting of snow, and (iv) the joint PDF P ( M ; t m ) of the maximum amount of available water M and its occurrence time t m before the first passage time. We further confirm our analytical predictions by computing the same PDFs with direct numerical simulations of the corresponding Langevin equation. We obtain a very good agreement of our theoretical predictions with the numerically simulated results. Finally, several nontrivial scaling behaviour in the asymptotic limits for the above mentioned PDFs are predicted, which can be verified further from experimental observation.