October 23, 2025 | 06:54 pm

TEMPO.CO, Jakarta - IPB University's Geophysics and Meteorology Department lecturer, Sonni Setiawan, revealed another theory about the recent heatwaves affecting various regions in Indonesia. The Meteorology, Climatology, and Geophysics Agency (BMKG) and researchers from the National Research and Innovation Agency (BRIN) previously stated that the high temperatures during the day were due to the apparent shift of the sun to the southern part of Indonesia. Another reason is the dry air mass from the Australian monsoon.
According to Sonni, the daily maximum temperature rise is also related to the absorption of electromagnetic field radiation by the atmosphere. This condition affects changes in air temperature, especially in the lower tropospheric layer.
The atmosphere acts as a medium that receives radiation from two main sources: the Sun and the Earth. "Radiation from the sun is called shortwave radiation, while radiation from the Earth is called longwave radiation. Both have different absorption spectra," said Sonni in a written statement on Thursday, October 23, 2025.
Sonni mentioned that solar radiation is mostly absorbed in the stratospheric to thermospheric layers, especially in the ultraviolet (UV) spectrum. Meanwhile, longwave radiation from the Earth's surface is predominantly absorbed by the tropospheric layer in the infrared (IR) spectrum. The amount of radiation energy absorbed by the atmosphere depends on the density of absorbing particles and the intensity of the received radiation.
"The higher the concentration of absorbing particles, the greater the energy absorbed, thus increasing the air temperature," he said.
According to Sonni, two main factors can trigger air heating in the lower atmospheric layer. First is the increase in the concentration of longwave radiation-absorbing gases, such as water vapor and carbon dioxide (CO2), as well as aerosol particles from pollutants and dust. This process is known as the greenhouse effect, where heat from the Earth is trapped in the atmosphere.
The second factor is the change in land cover due to the conversion of green areas into built-up areas. This change is believed to impact the Earth's surface heat capacity.
A surface with low heat capacity, such as concrete or asphalt, absorbs and releases heat more quickly than soil or vegetation. "This increases the surface temperature and strengthens the heating of the air in the lower layer," he said.
The Earth's astronomical position also affects the variation of received radiation. In October, the sun is almost directly above Java and Bali. As a result, these two regions receive a higher intensity of solar radiation.
"This phenomenon is a natural physical process that occurs every year. However, the temperature will feel more extreme when influenced by changes in land use and increasing pollutants in the atmosphere," said Sonni.
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