Suhu Makassar: Past, Present, and Future

Climate Trends and Historical Patterns

Makassar, the capital of South Sulawesi, is known for its tropical climate with consistent temperatures. Historical data shows that the city has experienced a gradual increase in its average temperature over the past few decades.

Records indicate a steady rise in both the minimum and maximum temperatures. The average minimum temperature has risen by approximately 0.5 degrees Celsius since the 1960s, while the average maximum temperature has increased by about 1 degree Celsius during the same period.

These changes align with global warming trends observed worldwide, with human activities contributing to increased greenhouse gas emissions and subsequent temperature increases.

Factors Influencing Temperature Changes

Urbanization and Land Use Changes

Rapid urbanization and the expansion of impervious surfaces, such as buildings and roads, have contributed to the increase in temperatures in Makassar.

Urban areas tend to absorb and retain more heat, leading to a phenomenon known as the urban heat island effect.

Deforestation and Land Conversion

The conversion of natural areas, including forests, to agriculture or urban development, has reduced the amount of vegetation that can absorb and regulate heat.

Deforestation and land conversion can alter local climate patterns, leading to increased temperatures and changes in precipitation.

Greenhouse Gas Emissions

The burning of fossil fuels, deforestation, and other human activities release greenhouse gases into the atmosphere.

Suhu Makassar