The map of regional mean sea level trends provides an overview of variations in the rates of relative
local mean sea level observed at long - term tide stations (based on a minimum of 30 years of data in order to account for long - term sea level variations and reduce errors in computing sea level trends based on monthly mean sea level).
Not exact matches
There's great fear in
local governments about what
sea -
level rise
means for all those mortgage holders who pay taxes.
A working group known as PALSEA2 (Paleo constraints on
sea level rise) used past records of
local change in
sea level and converted them to a global
mean sea level by predicting how the surface of the Earth deforms due to changes in ice - ocean loading of the crust, along with changes in gravitational attraction on the ocean surface.
This
means that, relative to whatever the
local sea level is in the future, the risk of huge storm surges could be lower than it is today.
Vertical land movements such as resulting from glacial isostatic adjustment (GIA), tectonics, subsidence and sedimentation influence
local sea level measurements but do not alter ocean water volume; nonetheless, they affect global
mean sea level through their alteration of the shape and hence the volume of the ocean basins containing the water.
Projections of
mean global
sea -
level (GSL) rise provide insufficient information to plan adaptive responses;
local decisions require
local projections that accommodate different risk tolerances and time frames and that can be linked to storm surge projections.
As you are aware there are major
local variations from the global pattern, with coastal land in some regions sinking faster than the average and in other regions being uplifted with respect to
mean sea level.
That
means that rising
sea levels could reduce
local reef water temperatures by a substantial amount, helping protect them from becoming stressed and bleaching as a consequence.
Although
mean sea levels are rising by 1mm / year,
sea level rise is
local rather than global, and is concentrated in the Baltic and Adriatic
seas, South East Asia and the Atlantic coast of the United States.
But one modeling study put the threshold
level for the eventual near - complete loss of Greenland's ice sheet at a
local warming of just 2.7 C — which, due to Arctic amplification,
means a global warming of only 1.2 C. Total melting of Greenland — luckily, something that would likely take centuries — would raise
sea levels by 7 meters, submerging Miami and most of Manhattan, as well as large chunks of London, Shanghai, Bangkok and Mumbai.