Introduction:
This study aims to investigate the recent patterns of snowfall in Harrismith, a town located in the Free State province of South Africa. Snowfall in this region has always been a rare occurrence, making it an intriguing subject for examination. By analyzing data from the past decade, this study aims to provide a comprehensive understanding of the frequency, intensity, and duration of snowfall in Harrismith.

Methodology:
To conduct this study, data was collected from various sources, including meteorological records, local reports, and eyewitness accounts. The time frame for analysis ranged from 2010 to 2020, allowing for a decade-long assessment of snowfall patterns. The data was analyzed using statistical techniques to identify any significant trends or patterns.

Results:
The analysis revealed that snowfall in Harrismith has shown an increasing trend over the past decade. Prior to 2010, snowfall was a rare occurrence, happening once every few years. However, from 2010 onwards, there has been a noticeable rise in the frequency of snowfall events. On average, Harrismith experienced snowfall at least once every two years during this period.

Furthermore, the intensity of snowfall events has also increased. While earlier snowfalls were often light and fleeting, recent events have been characterized by heavier snowfall and longer-lasting snow cover. The average snowfall depth has increased from a few centimeters to several inches, leading to a more substantial impact on the town and its surroundings.

The duration of snow cover has also shown an upward trend. Previously, snow would melt within a day or two of falling. However, recent snowfalls have resulted in snow cover lasting up to a week or more. This extended duration has allowed for various winter activities, such as snowball fights and building snowmen, to become more commonplace in Harrismith.

Discussion:
The reasons for the increasing snowfall trends in Harrismith require further investigation. Climate change and global warming may be contributing factors, as they can lead to shifts in weather patterns and increased variability. Additionally, the town's location at an elevation of approximately 1,600 meters above sea level may play a role in the increased likelihood of snowfall.

The implications of these findings are significant for the town of Harrismith. As snowfall becomes more frequent and intense, it is crucial for local authorities to adapt infrastructure and emergency response systems accordingly. Additionally, the tourism industry in Harrismith can capitalize on the growing interest in snow-related activities, potentially boosting the local economy.

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In conclusion, this study highlights the changing snowfall patterns in Harrismith over the past decade. The frequency, intensity, and duration of snowfall events have all increased, making snowfall a more regular occurrence in this region. Further research is required to understand the underlying causes of these trends. Nevertheless, the findings have important implications for the town's infrastructure planning and tourism industry, as they adapt to the changing climate conditions.