activity
20172022
most citedDerivation of the nonlocal pressure form of the fractional porous medium equation in the hydrological setting

18 citations · 18 across the 4 of their papers we have counts for

collaborators

9 papers

math.CA2022

The Bushell-Okrasiński inequality

Łukasz Płociniczak

We present an expository account of the Bushell-Okrasiński inequality, the motivation behind it, its history, and several generalizations. This inequality originally appeared in st…

math.NA2022

Error of the Galerkin scheme for a semilinear subdiffusion equation with time-dependent coefficients and nonsmooth data

Łukasz Płociniczak

We investigate the error of the (semidiscrete) Galerkin method applied to a semilinear subdiffusion equation in the presence of a nonsmooth initial data. The diffusion coefficient…

math.DS2021

Stability of fixed points in an approximate solution of the spring-mass running model

Zofia Wróblewska, Piotr Kowalczyk, Łukasz Płociniczak

We consider a classical spring-mass model of human running which is built upon an inverted elastic pendulum. Based on our previous results concerning asymptotic solutions for large…

math.CA2019

Asymptotic behaviour of a solution to a nonlinear equation modelling capillary rise

Łukasz Płociniczak, Mateusz Świtała

We are concerned with the asymptotics and perturbation analysis of a singular second-order nonlinear ODE that models capillary rise of a fluid inside a narrow vertical tube. We pro…

cs.CE2019

A weighted finite difference method for subdiffusive Black Scholes Model

Grzegorz Krzyżanowski, Marcin Magdziarz, Łukasz Płociniczak

In this paper we focus on the subdiffusive Black Scholes model. The main part of our work consists of the finite difference method as a numerical approach to the option pricing in…

math.DS2019

Asymptotic analysis of internal relaxation-oscillations in a conceptual climate model

Łukasz Płociniczak

We construct a dynamical system based on the KCG (Källén, Crafoord, Ghil) conceptual climate model which includes the ice-albedo and precipitation-temperature feedbacks. Further, w…