Experts weigh in on
the local effects of sea level rise.
Not exact matches
Perrette has modelled all
of these
effects and calculated
local sea level rises in 2100 for the entire planet.
The reasons why the projected
sea -
level rise at Copenhagen is more severe than at Oslo are complicated, but are primarily related to the
effects that we have discussed: Differing rates
of crustal rebound and
local gravitational changes at the two cities.
If we lose them rapidly then there would be a small rapid
sea -
level rise, major rapid
local effects to do with huge quantities
of meltwater, and an albedo feedback
effect.
In a recent
local article on the
effects of «climate change» on the Outer Banks
of North Carolina, the author actually admitted that parts
of the northern barrier island were actually sinking, but all
of the other erosion was due to
sea level rise.
A 2017 disclosure by San Francisco reads: «The city is unable to predict whether
sea level rise or other impacts
of climate change or flooding from a major storm will occur, when they may occur, and if any such events occur, whether they will have a material adverse
effect on the business operations or financial condition
of the city and the
local economy.»
In the future, high - end estimates
of ice discharge and regional
effects, such as
local thermal expansion and coastal subsidence, place the upper limits
of relative
sea -
level rise for the Netherlands at 0.65 to 1.3 m by 2100, excluding gravitational
effects.
But a new study published in the journal Science Advances has concluded that another impact
of global climate change might help coral reefs survive increasing
sea temperatures: «even a modest
sea level rise can substantially reduce temperature extremes within tide - dominated reefs, thereby partially offsetting the
local effects of future ocean warming,» the authors
of the study write.
The Virginian Pilot's editorial board and, specifically news writer Scott Harper have been repeatedly advised by me and others that the answer to modifying the
local effects of rising sea levels involves reestablishment / establishment
of large, healthy fringe marshes (living shorelines).