14. Lightning Strikes Create Radiocarbon
Every time lightning strikes, the atmosphere generates a tiny quantity of radiocarbon, sometimes known as carbon-14. This happens when the powerful energy of the lightning bolt splits nitrogen atoms in the air and recombines with atmospheric carbon to create radiocarbon. Although the total effect of billions of lightning strikes occurring worldwide each year greatly influences the natural background levels of radiocarbon on Earth, even the miniscule quantity generated by one lightning strike. Radiocarbon dating, a method used by archaeologists and geologists to ascertain the age of biological materials, depends critically on this process. Knowing how lightning contributes to radiocarbon generation enables researchers to improve their dating techniques and offers understanding of previous climate conditions and lightning activity. Furthermore, research on this phenomenon could provide fresh approaches to follow atmospheric processes and grasp the global carbon cycle.