The weakening intensity of the Earth‘s magnetic field may actually be coming down to normal rather than approaching a reversal, a new study says. Also Read - National Science Day: Top 5 AR apps available on Apple's App Store to learn scienceAlso Read - Discovery Plus App: Discovery launches new app with Rajnikanth and Bear Grylls
The intensity of the Earth’s magnetic field has been weakening for the last couple of hundred years, leading some scientists to think that its polarity might be about to flip. But now scientists said the field’s intensity may simply be coming down from an abnormal high rather than approaching a reversal. Also Read - New ultrafast camera takes 1 trillion frames per second
The weakening of the Earth’s magnetic field would affect technology. The magnetic field deflects the solar wind and cosmic rays. When the field is weaker, more radiation gets through, which can disrupt power grids and satellite communications.
“The field may be decreasing rapidly, but we are not yet down to the long-term average. In 100 years, the field may even go back the other direction [in intensity],” said study co-author Dennis Kent from Columbia University’s Lamont-Doherty Earth Observatory.
The scientists used a new technique to measure changes in the magnetic field’s strength in the past and found that its long-term average intensity over the past five million years was much weaker than the global database of paleointensity suggests – only about 60 percent of the field’s strength today.
The findings raise questions both about claims that the magnetic field may be nearing a reversal. The study’s results fit expectations that the magnetic field’s intensity at the poles should be twice its intensity at the equator. In contrast, the time-averaged intensity calculated from the PINT paleointensity database doesn’t meet the two-to-one, poles-to-equator dipole hypothesis, and the database calculation suggests that the long-term average intensity over the past five million years is similar to the field’s intensity today.
The study appeared the journal Proceedings of the National Academy of Sciences.