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That model incorporates data not just from atmospheric pressure and ocean dynamics—changing currents, rising ocean temperatures and salinity all influence sea level—but also, for the first time, ice mass change in Greenland and Antarctica.The researchers say their model supports a growing consensus that sea level rise began accelerating in 1990 and that what they found will improve estimates of future sea level rise at a local level.
You will chat, you will date, meet foreign singles, and hopefully find that one perfect Azerbaijan women who will become your love, your soulmate and life partner!Their model, which incorporated assumptions that acceleration of sea level rise began in the 1990s and not before that, accurately predicted variations in sea level rise along North America’s East Coast that have been observed in tide-gauge data for over a half century. East Coast north of Cape Hatteras, rates of sea level rise were found to be some three to four times higher than the global average over certain periods.Recent research indicates that global mean sea level, or the average height of the world’s oceans, has been increasing by 3 millimeters (.1 inches) per year on average since 1993, when satellites first started measuring it. Essential to the model Davis and Vinogradova built was research published in 2014 that for the first time measured acceleration in glacial melt in Greenland and Antarctica using data from NASA satellite GRACE.Davis and Vinogradova chose to focus on the acceleration of sea level rise specifically to avoid the problem of accurately measuring what is known as post-glacial rebound.Post-glacial rebound is the ongoing shape-shifting of the earth’s surface that occurs after it is released from the burden of mountains of glacial ice, a process that began in North America at the end of its last ice age 16,000 years ago.“A lot of people have been looking for sea level acceleration and have been having trouble finding it,” said James Davis, co-author on the paper and a professor and researcher at the Lamont-Doherty Earth Observatory.
“The fact that we could model this well seems to indicate that what we are measuring is correct.” Davis worked together with oceanographer Nadya Vinogradova, founder of Cambridge Climate Institute in Massachusetts, on the sea level rise modeling project.
Typically the Gulf Stream depresses sea level right along the coast, so as this current weakens, sea levels bounce back.
Meanwhile, higher ocean temperatures kick up sea level by expanding the water column.
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Though the melted ice adds volume to the oceans, it also causes sea levels closest to a melted glacier to fall due to a decline in gravitational pull from mass loss, called gravitational self-attraction.