Abstract

Statistical monitoring tools are well established in the literature, creating organizational cultures such as Six Sigma or Total Quality Management. Nevertheless, most of this literature is based on the normality assumption, e.g., based on the law of large numbers, and brings limitations towards truncated processes as open questions in this field. This work was motivated by the register of elements related to the water particles monitoring (relative humidity), an important source of moisture for the Copiapó watershed, and the Atacama region of Chile (the Atacama Desert), and presenting high asymmetry for rates and proportions data. This paper proposes a new control chart for interval data about rates and proportions (symbolic interval data) when they are not results of a Bernoulli process. The unit-Lindley distribution has many interesting properties, such as having only one parameter, from which we develop the unit-Lindley chart for both classical and symbolic data. The performance of the proposed control chart is analyzed using the average run length (ARL), median run length (MRL), and standard deviation of the run length (SDRL) metrics calculated through an extensive Monte Carlo simulation study. Results from the real data applications reveal the tool’s potential to be adopted to estimate the control limits in a Statistical Process Control (SPC) framework.

Highlights

  • Departamento de Matemática, Facultad de Ingeniería, Universidad de Atacama, Copiapó 1530000, Chile; Laboratorio de Investigación de la Criósfera y Aguas, IDICTEC, Universidad de Atacama, Institute of Mathematical and Computer Sciences, University of São Paulo, São Carlos 13566590, Brazil; Abstract: Statistical monitoring tools are well established in the literature, creating organizational cultures such as Six Sigma or Total Quality Management

  • standard deviation of the run length (SDRL), which consider the occurrence of false alarms at the LCL and UCL, respectively

  • We developed a new control chart based on the unit-Lindley distribution by [17], named as unit-Lindley chart, and its inferential properties

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Summary

The Data

Precipitation is only a few millimeters per year or sometimes non-existent, making it one of the driest places on Earth [22,23]. An important event occurs in this area, where marine stratocumulus cloud banks that form on the Chilean coast, called Camanchaca, which is daily the passageway of “low clouds”, right after sunrise, sequentially for a couple of hours. This event is the source of water for many types of flora and fauna in the Atacama desert. In addition to relative humidity, the data measured are atmospheric pressure, temperature, global solar radiation, precipitation, and wind direction and speed, the last both are installed at 10 meters above ground level. Our data acquisition came from a weather station located at the University of Atacama in Copiapó, Chile (in the top left-hand picture)

Methodology
The Unit-Lindley Distribution
Proposed Unit-Lindley Chart
Statistical Performance
In-Control Processes
Out-of-Control Processes
Comparison with Some Standard Control Charts
Application
Findings
Concluding Remarks and Future Prospects
Full Text
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