Over the past 3,000 years, the core of the earth has been speeding up a little, and the mantle-crust on which we stand is slowing down, scientists believe.

TOP INSIGHT
In a century from now, the length of a day will increase by 1.7 milliseconds, this may not seem like much, but this is a cumulative effect that adds up over time.
"In order to fully understand the sea-level change that has occurred in the past century, we need to understand the dynamics of the flow in the Earth's core" Dumberry explained. The connection is through the change in the speed of the Earth's rotation.
The water melting from glaciers not only causes sea-level rise, but also shifts mass from the pole to the equator, which slows down the rotation. The gravity pull from the moon also contributes to the slow down, acting a little like a leaver break.
"This can help to better prepare coastal towns, for example, to cope with climate change," Dumberry added. The study was published in the journal Science Advances.
Source-IANS
MEDINDIA




Email




