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Mountain Views News Saturday, October 2, 2010
Only One Earth
Climate Change and the
World’s Oceans
by Albert Metzger
The disaster in the Gulf has focused
attention on mankind’s potential
to negatively impact the marine
environment on a large scale.. A
less dramatic but even broader and
more far reaching situation involves
the world’s oceans. An article in
the July 4th issue of the Sacramento
Bee by Les Blumenthal has drawn
our attention to a report entitled
“The Impact of Climate Change on
the World’s Marine Ecosystems”
in the June 18th issue of Science.
This heavily referenced summary
article draws on a multitude of
studies, most of them published
within the last four years, to review
and summarize the condition
of the oceans. Oceans make up
71% of the world’s surface. The
“overwhelming evidence” is that
their condition is deteriorating,
that the cause is predominantly
the result of human activities, and
that serious consequences are likely
in the next 20 to 100 years. Their
extent will depend on actions taken
or ignored.
The data discussed includes
ocean temperatures, acidity,
and carbonate concentrations.
Increased greenhouse gas (carbon
dioxide being the principle one)
concentrations have increased the
energy content of the atmosphere.
Most of the additional energy
is being absorbed in the ocean,
which has lead to an increase in the
upper 2000 feet of over one degree
Fahrenheit in the past century.
This may sound small but a great
deal of energy is involved. The
global upper ocean temperature
average for January 2010 was the
second warmest January on record.
Oceans are also absorbing about
a third of the man-made carbon
dioxide. The resultant acidification
has lead to a substantial decline
in carbonate ion concentration
and represents a major departure
from the ocean chemistry which
has existed unchanged for at
least hundreds of thousands, and
perhaps millions, of years until
now.
With an increase in water
temperature comes thermal
expansion. This thermally-caused
expansion of ocean volume, along
with the melting of glaciers and ice
sheets, forms the basis for current
observations and future predictions
of sea level rise. Current estimates
of the rise in sea level by the year
2100 range from 20 to 47 inches.
This is hardly consequential in
Sierra Madre, but check it out with
someone living, for example, in
Venice, Italy.
The surface temperature of
large bodies of water affects the
weather. As tropical storms are
tracked out of the Caribbean,
it’s become common to hear in
weather reports how warmer
water temperatures intensify wind
and wave movements. Increasing
surface water temperatures will
tend to increase the severity of
tropical storms.
The effect of global warming
on the oceans is not uniform,
depending in part on local factors
such as current, water depth, and
wind. This is particularly true with
regard to latitude. Temperature
and the acidity of the polar oceans
are changing at more than twice
the global average, with the rate
in the northernmost 15 degrees of
latitude running about twice that
in the southernmost 15 degrees.
Arctic sea ice is disappearing at an
increasing rate and the stability of
the continental ice sheets in high
latitudes, both north and south, is
in question.
Yet another consequence of upper
layer warming is to increase the
thermal contrast of the (vertical)
water column. Circulation
models predict such an increase
will result in less mixing and in
decreased oxygen concentration,
with an adverse effect on nutrient
production and availability. To
this is ascribed the startling
finding that nutrient-poor ocean
“deserts” have grown by over
2.5 million square miles in only
nine years, from 1998 to 2006.
This is almost 2% of the entire
surface area of the Earth’s oceans.
Paleontological evidence points to
declining oxygen concentrations
as playing an important role in
some mass extinction events.
Another unsettling measurement
reported is that the production of
phytoplankton, which represents
the base of the ocean food chain,
has decreased by 6% in the past
thirty years.
The article points out that the
effects on marine species stemming
from the extent and rapidity of
changes to the global ocean need to
be considered in terms of metabolic
rates, population growth, and the
degree to which organisms can
adapt to changing conditions.
All of these are temperature
dependent. Emphasis is placed on
the interrelated nature of marine
ecosystems, and on global warming
as facilitating the spread of diseases
and intrusive species to the
detriment of native populations,
and on other factors such as
sediment deposit, coastal pollution,
overfishing and increased
ultraviolet exposure, all of which
act to intensify the effects of global
warming. Among the most
vulnerable and already impacted
ecosystems are coral reefs, kelp
forests, mangrove, and sea grass
communities, all four of which
share the property of providing
habitat for thousands of species,
many of whom will disappear when
their habitat expires or is seriously
degraded. Polar warming puts at
risk, not only the polar bear, but
also penguins, seals, walruses, and
many species of birds.
The article’s authors, Ove Hoegh-
Guldberg who directs the Global
Change Institute at the University
of Queensland in Australia, and
John F. Bruno at the University
of North Caroling, state that,
with continuing increases in the
concentrations of atmospheric
carbon dioxide, we face a growing
risk that several thresholds for
long term and perhaps irreversible
damage will soon be reached
and therefore, in their words, “...
avoiding any further increases and
aiming to reduce the atmospheric
concentration of carbon dioxide
below 350 ppm in the long term [ed
note: the Mauna Loa Observatory
in Hawaii puts it now at 390
ppm] must be an international
imperative.” This is so, “...not
only because it will reduce the
huge costs of adaptation but also
because it will reduce the growing
risk of pushing our planet into an
unknown and highly dangerous
state.” The situation can hardly be
put more strongly than that.
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