Otto Šling and his propagandistic campaign ,,Youth lead Brno''

The subject of the Bachelor thesis are the life fates of Otto Šling and his family. In the beginning the interpretation of Šling's life is centered on his motives to organise the propagandistic action "The Youth lead Brno". Following in the text there is mediated a reflection of pro communist campaign in selected Czechoslovakian media of that time. While in the observation period between May 1st, 1949 and June 2nd, 1949 the action was publicly supported, after Šling's arrest in October of the following year on the contrary it was condemned by the communist functionaries. Based on concrete medial announcements and accessible professional literature changes of the moods of the society are presented that took place in dependence on the fabrication of the political trials in the fifties of the last century. This fact is closely specified in the third part of the thesis which concerns itself with the role of Otto Šling in the Trial of anti-state conspiracy centered around Rudolf Slánský and his impact on the lives of Šling's closest relatives

Simulated and observed daily average temperatures.

<p>Simulated and observed daily average temperatures.</p

Pseudo-code of the EMPSO algorithm.

<p>Pseudo-code of the EMPSO algorithm.</p

High-order scheme for the source-sink term in a one-dimensional water temperature model

<div><p>The source-sink term in water temperature models represents the net heat absorbed or released by a water system. This term is very important because it accounts for solar radiation that can significantly affect water temperature, especially in lakes. However, existing numerical methods for discretizing the source-sink term are very simplistic, causing significant deviations between simulation results and measured data. To address this problem, we present a numerical method specific to the source-sink term. A vertical one-dimensional heat conduction equation was chosen to describe water temperature changes. A two-step operator-splitting method was adopted as the numerical solution. In the first step, using the undetermined coefficient method, a high-order scheme was adopted for discretizing the source-sink term. In the second step, the diffusion term was discretized using the Crank-Nicolson scheme. The effectiveness and capability of the numerical method was assessed by performing numerical tests. Then, the proposed numerical method was applied to a simulation of Guozheng Lake (located in central China). The modeling results were in an excellent agreement with measured data.</p></div

Simulated and observed water temperatures in the vertical direction, on July 13.

<p>Simulated and observed water temperatures in the vertical direction, on July 13.</p

Comparison of simulation outcomes and analytical solutions for Experiment 1: (a) <i>D</i> = 0.0001; (b) <i>D</i> = 1; (c) <i>D</i> = 5; (d) <i>D</i> = 10.

<p>Comparison of simulation outcomes and analytical solutions for Experiment 1: (a) <i>D</i> = 0.0001; (b) <i>D</i> = 1; (c) <i>D</i> = 5; (d) <i>D</i> = 10.</p

Comparison of simulation outcomes and analytical solutions for Experiment 2, using the refined mesh: (a) <i>D</i> = 0.0001; (b) <i>D</i> = 1; (c) <i>D</i> = 5; (d) <i>D</i> = 10.

<p>Comparison of simulation outcomes and analytical solutions for Experiment 2, using the refined mesh: (a) <i>D</i> = 0.0001; (b) <i>D</i> = 1; (c) <i>D</i> = 5; (d) <i>D</i> = 10.</p

Pseudo-code of the IGSA.

<p>Pseudo-code of the IGSA.</p

RRE values for Experiment 2.

<p>RRE values for Experiment 2.</p

Meteorological data for the period from July 1 to August 31, 1978.

<p>Meteorological data for the period from July 1 to August 31, 1978.</p