New Tool May Assist US
Regional Sea Level Planning
From NASA’s Jet Propulsion Laboratory
Projections for future sea level rise show this prospect for Trump's Mar-A-Lago resort (a.k.a. the Winter White House) |
Thanks
in large part to satellite measurements, scientists' skill in measuring how
much sea levels are rising on a global scale - currently 0.13 inch (3.4
millimeters) per year - has improved dramatically over the past quarter
century.
But
at the local level, it's been harder to estimate specific regional sea level
changes 10 or 20 years away - the critical timeframe for regional planners and
decision makers.
That's
because sea level changes for many reasons, on differing timescales, and is not
the same from one place to the next.
Developing
more accurate regional forecasts of sea level rise will therefore have
far-reaching benefits for the more than 30 percent of Americans who currently
reside along the Pacific, Atlantic or Gulf Coasts of the contiguous United
States. This
means you, Charlestown.
New research published this week in the Journal of Climate reveals that one key measurement -- large-scale upper-ocean temperature changes caused by natural cycles of the ocean -- is a good indicator of regional coastal sea level changes on these decadal timescales.
Such
data may give planners and decision makers a new tool to identify key regions
of U.S. coastlines that may be vulnerable to sea level changes on 10- to
20-year timescales.
"Decision
makers need a diverse set of tools with different informational needs,"
said lead author Veronica Nieves of UCLA and NASA's Jet Propulsion Laboratory
in Pasadena, California.
"Having
a better understanding of the chances of local flood damage from rising seas in
coastal areas is a key factor in being able to assess vulnerability, risk and
adaptation options."
Such tools could help planners decide whether a given part of a coastline would be better served by "soft" techniques, such as beach replenishment or preservation of wetlands, or by "hard" techniques, such as construction of sea walls or levees.
Such tools could help planners decide whether a given part of a coastline would be better served by "soft" techniques, such as beach replenishment or preservation of wetlands, or by "hard" techniques, such as construction of sea walls or levees.
Nieves'
team, which included participation from the Mediterranean Institute for
Advanced Studies in Esporles, Spain, set out to detect decadal sea level
changes over large U.S. coastal ocean regions.
They
compared existing National Oceanic and Atmospheric Administration (NOAA)
records of upper-ocean temperatures in coastal waters for each U.S. ocean
coastline with records of actual sea level changes from 1955 to 2012, and data
from U.S./European satellite altimeter missions since 1992.
They
identified those sea level changes that have a large impact at regional scales
in many locations, including largely populated cities. Sea level along the U.S.
East Coast and West Coast can rise and fall by an inch or two (several
centimeters) over the course of a decade or two because of fluctuations in
upper ocean temperatures.
Their
method was able to explain about 70 percent of regional sea level variability
on decadal time scales for the West Coast, about 80 percent for the East Coast,
and about 45 percent for the Gulf Coast.
Along
the Gulf Coast, the authors say other factors, such as tidal effects and the
ongoing subsidence, or sinking, of the land, can play a more important role.
"Our
study shows that large-scale upper-ocean temperature changes provide a good way
to distinguish decade-long natural ocean signals from longer-term global
warming signals," said Nieves.
"This
is important for regional planning, because it allows policymakers to identify
places where climate change dominates the observed sea level rise and places
where the climate change signal is masked by shorter-term regional variability
caused by natural ocean climate cycles."
Nieves
said an example is the U.S. West Coast, where the phase of a multi-decadal
ocean climate pattern called the Pacific Decadal Oscillation has helped keep
sea level rise lower during the past two decades. With the recent shift of this
oscillation to its opposite phase, scientists expect sea level rise along the
West Coast to accelerate in coming years.
"Scientists
have worked hard to understand the really fast changes in sea level, such as
storm surges, because they cause major damage, and the really slow changes
because long-term sea level rise will shape the coastlines of the future,"
said study co-author Josh Willis of JPL. "But in between these fast and
slow changes, there's a gap in our understanding. The results of our study help
fill that gap."