Not exact matches
Beyond honing communications skills, participants said while the discussions often started off with broad
trends in climate science, invariably the exchanges shifted to specific
local issues such as wildfires, ozone
levels, crop rotations,
sea level rise, droughts and air quality.
This decreasing
trend in
local gravity is sufficient to counteract all other sources of
local sea -
level rise.
Note that the variation in
sea level due to ENSO is only a few mm, really small compared to both the longer - term anthropogenic
trend and to the
local variations in
sea level in the Pacific which can be even decimetres in places.
However the general
sea level rise
trend has a lot of
local variation.
The biggest difficulty in using tidal gauges to study global
sea level trends is separating
local changes from global changes.
This will have introduced an artificial «
sea level rise»
trend into the tidal gauge records for those areas, which is actually due to the
local land subsiding.
However, as we have seen throughout this section, the tidal gauge estimates the IPCC used to estimate global
sea level trends are contaminated by
local trends, such as tectonic activity, post-glacial rebound... and the coastal subsidence that Syvitski et al. identified!
Over the long - term, melting of the West Antarctic Ice Sheet could yield as much as 10 to 14 feet of global average
sea level rise, with
local sea level rise varying considerably depending on land elevation
trends, ocean currents and other factors.
In order to use tidal gauges to reliably estimate global
sea level changes, researchers have to successfully separate the components of shifting land heights and
local sea level variability from any global
trends.
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).
Stations illustrated with negative
trends (blue - to - purple) are experiencing global
sea level rise and a greater vertical rise in the
local land, causing an apparent decrease in relative
sea level.
Stations illustrated with positive
sea level trends (yellow - to - red) are experiencing both global
sea level rise, and lowering or sinking of the
local land, causing an apparently exaggerated rate of relative
sea level rise.
Choice of GIA correction is critical in the
trends for the
local and regional
sea levels, introducing up to 8 mm · yr − 1 uncertainties for individual tide gauge records, up to 2 mm · yr − 1 for regional curves and up to 0.3 — 0.6 mm · yr − 1 in global
sea level reconstruction.
However, this is complicated by non-tidal, short - term,
local sea -
level variability that is orders of magnitude greater than the
trend.»
He continually confuses global, regional, and
local temperature
trends, which may differ considerably; he mischaracterizes the results of a poll that was undertaken to determine scientists» views on global warming; and he mistakenly asserts that the
sea level has not risen significantly, when it has.
Note that these
trends may include a component of subsidence / uplift of the islands themselves and so are the numbers most relevant for
local planning (not eustatic
sea level change).