Map of gravity distribution in the world.
Several years ago, scientists from the Harvard-Smithsonian Center for Astrophysics and the University of Toronto (Canada) measured planetary gravity with a sensor attached to NASA's GRACE satellite.
Data from GRACE allows scientists to create topographic maps depicting the Hudson Bay during the last ice age, when the bay is still covered by Laurentide ice .
Laurentide ice is 3.2 km thick and 2 places in Hudson Ice Bay is 3.7 km thick. It was a very heavy piece of ice on the Earth. Over 10,000 years, the Laurentide ice sheet has melted and disappeared only to leave a dent on the green planet. The ice melts slowly so the crust doesn't push back. According to experts, gravity has lost half.
According to geophysicist Mark Tamisiea of Proudman Oceanographic Laboratory in Liverpool, the clear indication that gravity at Hudson Bay is increasing every year.
The Laurentide iceberg hypothesis only explains 25% to 45% of gravity variation around Hudson Bay.
The 3D graph shows the larger the gravity bulge.
Eliminating the " recovery effect ", scientists have determined that 55% to 75% of gravity changes are due to convection occurring in the earth's crust.
The coating is a layer of molten rock called magma and exists at a depth (100 to 200 km) below the surface of the Earth. Magma is very hot and moves continuously, rising and falling, and creating convection. Convection pulls down the continental plates of the earth, reducing the mass in that area and reducing gravity.
The Hudson Bay of Canada is also considered a low-gravity place for a long time. Scientists estimate that the Earth takes about 5,000 years to recover more than 0.2 km of rock to return to its original position. We can see the recovery effect.
Although the sea level is rising worldwide, the sea level at the coast of Hudson Bay is reduced because the rock continues to recover due to the weight of the Laurentide ice sheet.
GRACE satellites are very sophisticated machines, orbiting around 500 km above the earth. The satellites can measure distances to micron sizes, so they can detect gravity variations even if only very small. When satellites lead the way over Hudson Bay, weak gravity causes the satellite to travel further than the earth and with satellites accompany it. The change in this distance is detected by the satellites and used to calculate the change in gravity. Any changes recorded are used to create attractive field maps.