Many Hawai`i beaches are eroding and it should be no
surprise that the primary culprit is sea level rise.
Sunday, September 8, 2013
Coastal erosion in Hawai`i? It's sea level rise, silly.
Hawai`i researchers recently published a paper in the
journal Global and Planetary Change that concluded that the main cause of
coastal erosion in the Islands is rising ocean levels.
(Image: Maui beaches are eroding at an average of half a
foot a year. Shown here is a coastal building on Maui, threatened by chronic
coastal erosion. Credit: Zoe Norcross-Nuu.)
There are certainly other factors, like currents and the
relative rise and subsidence of the islands themselves, but sea level’s the big
one.
It means, in part, that people assuming those disappeared beaches will
return cyclically to their previous size will wait in vain, and that the state’s
decision-makers need to plan for continued coastal erosion.
“Shorelines find an equilibrium position that is a balance
between sediment availability and rising ocean levels. On an individual beach
with adequate sediment availability, beach processes may not reflect the impact
of SLR. With this research, we confirm the importance of SLR as a primary
driver of shoreline change on a regional to island-wide basis,” said Brad
Romine, a coastal geologist with the University of Hawai`i Sea Grant College
Program.
What he’s saying there is that if a beach still has a large
natural dune system behind it—like, for instance, Polihale on Kaua`i—the sand
will replenish the retreating shoreline and you’ll still have a beach. But of
course, most of the state’s dune systems are long gone.
Sea level has been going up at nearly a tenth of an inch a
year for most of the 1900s, but the level has increased recently to slightly
more than a tenth of an inch a year—from 2 millimeters to 3 millimeters. That
works out to sea level rise of three-quarters of an inch per decade
accelerating to more than an inch.
Doesn’t seem like much, but at the current rate, a kid born
today will see sea levels more than half a foot higher by retirement age.
Imagine an additional seven or so inches on top of today’s highest tides, and
the picture looks ominous for coastal roads, beach parks, coastal resorts, and
sandy beach oceanfront homes.
That’s because each inch in sea level rise translates to
several inches of coastal retreat. Maui beaches, of which 78 percent are
eroding, have lost on average half a foot a year. Most O`ahu beaches are also
eroding, but at a far lower rate, about an inch a year.
Some coastlines clearly get hurt more than others, and
calculating the different coastal responses has been a major piece of Charles “Chip”
Fletcher’s work.
“Improved understanding of the influence of SLR on
historical shoreline trends will aid in forecasting beach changes with
increasing SLR,” said Fletcher, Associate Dean and Professor of Geology and Geophysics
at the University of Hawai`i School of Ocean and Earth Science and Technology.
Citation: B M
Romine, C H Fletcher, M M Barbee, T R Anderson, L N Frazer (2013) Are beach
erosion rates and sea-level rise related in Hawaiʻi? Global and Planetary Change, doi: 10.1016/j.gloplacha.2013.06.009
A press release on the project adds: “The research described
in this paper was carried out by the University of Hawaiʻi Coastal Geology
Group with the support of the State of Hawaiʻi; Counties of Kauaʻi, Oʻahu and
Maui; U.S. Geological Survey; U.S. Army Corps of Engineers; NOAA; Hawaiʻi CZM;
Hawaiʻi Sea Grant; and the Harold K.L. Castle Foundation. This paper is funded in part by a
grant/cooperative agreement from the National Oceanic and Atmospheric
Administration, Project A/AS-1, which is sponsored by the University of Hawaiʻi
Sea Grant College Program, SOEST.”
© Jan TenBruggencate 2013
Posted by Jan T at 9:23 AM 0 comments
Labels: Climate Change, Geology, Government, Marine Issues, Oceanography, Reefs, Sustainability
Saturday, September 7, 2013
Deep ocean canyons around Hawai`i are hot spots for species diversity
Often science
simply confirms what you’d suspect. Example: Life is more interesting in a
complicated landscape than a simple one.
Case in point: You get more life and more kinds of life in the wrinkled landscape of Hawaiian undersea canyons than on the broad flats.
University of
Hawai`i marine researchers determined that biodiversity is significantly higher
in the submarine canyons around Hawai`i than on the flats, largely because the
canyons provide so many more types of habitat, but also because they
concentrate nutrients.
The
researchers reported in the journal Deep Sea Research Part II after 34 dives
with the submersibles Pisces IV and V up and down the archipelago, from the
main Hawaiian Islands to the Papahānaumokuākea Marine National Monument in the
Northwestern Hawaiian Islands.
Their dives took them to study points at multiple depths, the deepest of them near a mile
down. The principal researcher was UH oceanography professor Craig Smith.
In the
canyons, they found both complexity of habit an increased biodiversity.
“Submarine canyons encompass myriad habitat
types. This heterogeneity at the landscape-scale helps to enhance local biodiversity
in canyon seafloor sediments,” said lead author Fabio C. De Leo, a doctoral
graduate from UH Mānoa’s department of oceanography. Species diversity is
considerably higher in canyons, he said.
In canyons,
many things are happening. There are diverse physical habitats. Ocean currents
are channeled. Sinking particles are captured. Too, a lot of the organic
material washed off the islands ends up settling in canyons, where they
decompose and add nutrients to a portion of the ocean normally limited in food
availability.
“When there’s
more food, there’s more life,” De Leo said.
Says the
University press release: “This series of dives was conducted on the Pisces IV and Pisces V
manned submersibles operated by the Hawai‘i Undersea Research Laboratory
(HURL). The research was conducted in
partnership with Hawai‘i Pacific University and the New Zealand National
Institute of Water and Atmospheric Research.”
Here is the
citation: Fabio C. De Leo, E.W. Vetter, C. R. Smith, A. R. Ashley, and M.
McGranaghan. Spatial scale-dependent
habitat heterogeneity influences submarine canyon macrofaunal abundance and
diversity off the Main and Northwest Hawaiian Islands. Deep Sea Research Part II: Topical Studies in
Oceanography. 11 July 2013.
© Jan
TenBruggencate 2013
Posted by Jan T at 8:13 AM 0 comments
Labels: Fisheries, Geology, Government, Marine Issues, Oceanography, Reefs, Zoology
Wednesday, September 4, 2013
Hawaii Energy Storage 9: A wrapup message: Follow the money
At the end of this series on energy storage, perhaps the
best message is an old one in investigations.
Follow the money.
There is no end of storage technologies: regular chemical
batteries, flow batteries, pumped storage, flywheels, heat storage and even
phase change materials.
Which one will change the face of the energy landscape? That’s
not yet clear.
And one reason is cost. Most of these technologies are still very expensive.
(Here is a good place to insert a notice of conflict. I am
an elected member of an electric cooperative board of directors. If lots of
people go off-grid, it certainly impacts the finances of the co-op, but as a
community co-op it’s also our imperative to serve the members, so if that’s the
better alternative for them…)
I talked a while back with the son of an old Wisconsin
farmer, who remembers his dad turning down a battery-based electrical system
for the farm. At the time, there was no electricity at the farm. Kerosene lamps
illuminated the place, and humans or animals did the work, not electric motors.
He turned down the battery system, in part because it was
far more expensive than the anticipated power line that an electric cooperative
would soon provide him.
“I’ll wait for the wire,” he said.
It costs a utility in Hawai`i $.30 to $.45 per kilowatt hour to
deliver power to your house, as it does in other areas
dependent on oil-fired power. It's a lot of money. Running your own power system might seem like a
slam dunk.
But follow the money.
You may spend $.20 to $.25 per kilowatt-hour or so
to make photovoltaic power at home (less with the tax credits included, but
they may not be around a lot longer). It can cost another $.25 to $.75 per kilowatt-hour
to store that energy for nighttime use—the numbers are all over the place
depending on technology and system size and financing. (If anyone wants to
nitpick these numbers, I’d be pleased to hear from you.)
If those numbers are good approximations, then without even talking about maintenance, equipment replacement, damage repair and so forth, the cost of your power is
at a minimum equal to utility power, and at a maximum much, much higher.
And and
if you’re your own power supplier, you have the added benefit, when the lights go
out, of personally responding rather than waiting for a trained lineman.
This is not to say going off-grid can’t work. It has always
made sense in some limited applications—like a remote location where up-front
infrastructure costs are prohibitive or a utility line isn’t available at all. It
is not an accident that most home power magazines describe remote homes, far
from existing grids.
And it’s not to say that going off-grid might not make economic
sense soon. When the price to make the power drops to a dime and it costs another
dime to store it, that’s when the big crossover comes.
We’re not there yet. But we may be there within a very few
years.
For utilities, which benefit from economies of scale,
certain storage applications already make sense, but even for them, those
applications generally require special situations.
© Jan TenBruggencate 2013
Posted by Jan T at 12:12 PM 0 comments
Labels: Energy, Government, Photovoltaic, Physics, Solar, technology
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