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Wednesday,
April 23, 2008, Rabi us Sani 16, 1429 A.H
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Under
pressure:
Earth science
A
bunch of agencies and scientific departments have encouraged leading
Earth science boffins to bang their heads together to identify the
10 most pressing Earth science questions of the 21st century. This
week we continue with the second part of the top ten list released
in a new report by the NRC
By
Rusty Rockets
(Part II)
ToThis week we
continue with the second part of the top ten list of urgent Earth
science questions devised by a group of leading Earth science
experts at the behest of the National Research Council (NRC). The 10
"big picture" questions raised are ones that have been
difficult to answer in the past, but are nonetheless questions that
Earth scientists must face this century if we are to protect the
planet and its inhabitants.
Why does the Earth
have plate tectonics and continents?
When did Earth's
continents first form, and what will their movements be in the
future? These are questions that don't have exact answers as yet,
but answering them may
provide further clues to such fundamental questions as why Earth has
plate tectonics at all.
Serious attempts
at explaining the existence of continents and how they shift have
been kicking around since the late 16th century, when cartographer
Abraham Ortelius - and a string of other luminaries including
Francis Bacon and Ben Franklin - first pondered the possibility of
continental drift. But it wasn't until 1912 that a theory of
continental drift - as well as the theory that all of Earth's
continents once formed a giant land mass called Pangaea - was
properly fleshed out by German interdisciplinary scientist and
meteorologist Alfred Wegener.
But Wegener's
theories were to remain supposition right up until 1947. During this
year, a team of scientists studying the Atlantic Ocean found
differences in seabed foundations, and variations in oceanic crust
thickness that indicated Wegener's theory was likely correct.
Unfortunately, however, Wegener died in 1930, and missed the
opportunity to bask in the kudos he was due.
Contemporary plate
tectonic theory is now very robust in regard to the mechanisms
behind plate movements. So much so that research has now turned to
discovering links between plate tectonics and Earth's water
supplies, continent creation, oceans, and life itself. According to
the authors of the NRC report, answering such questions would be
extremely useful, as the continental crust is known to play a key
role in regulating Earth's climate.
What causes the
climate to change - and how much can it change?
The authors of the
NRC report acknowledge that out of all the Earth systems they
discuss, climate is the most widely (and heatedly) discussed topic
within the public arena. A situation that has no doubt been fuelled
by its politicisation, and the subsequent media interest - often
provoking controversy where none previously existed - that has
arisen as a consequence. At the heart of climate change research
lays the question: what causes the climate to change?
Referring to the
2007 IPCC report on climate change, the authors of the NRC report
say that it is now "widely recognized" that Earth's
surface temperatures have increased since the beginning of the
industrial age, and that CO2 is "at least partly, if not
wholly, responsible" for this rise. Even if you're an
anthropogenic climate change sceptic, it doesn't change the fact
that our climate is changing.
For now,
scientists search for clues in ice cores, sediments, fossils, and
rocks, which show how Earth's climate has changed over the past four
billion years. Such samples provide a glimpse at the Earth's
geological record that may allow researchers to make predictions
about the Earth's climate in the future. According to the report,
researchers have already identified some of Earth's more extreme and
abrupt climate changes, and their possible causes. Periods of abrupt
climate change in Earth's history include the Permian-Triassic
boundary, the Paleocene-Eocene Thermal Maximum, and
Dansgaard-Oeschger events in the more recent Pleistocene Epoch. The
latter of these are abrupt climate fluctuations that occurred every
1,500 years during the last ice age. "Each oscillation is
characterised by gradual cooling followed by abrupt warming,
typically over just a few decades," write the NRC report
authors. "Even though these changes are rapid, their magnitude
is large - annual temperature swings of up to 16∞C are
recorded in Greenland ice cores."
How are Earth
processes controlled by material properties?
From little
things, big things grow; seems to be the key to this question. While
the ten big Earth science questions have so far tackled the
macroscale behaviours of plate tectonics and mantle convection,
these large behaviours are themselves the result of microscale
properties of Earth materials - down to the atomic level. This may
seem obvious, but sometimes it takes a while before the simplest of
concepts becomes clear. According to the report, research exploring
the atomic structure of Earth materials will be crucial to
understanding Earth's macroscale history, and how Earth processes
may unfold into the future.
How do fluid flow
and transport affect the human environment?
The Earth is not a
bottomless waste dump, and what we discard will in some form or
another come back to haunt us - usually via waterways on which we
are heavily dependent. As a result, scientists have made it a
priority to model fluid movements at the surface level; observing
rivers and streams, how stream erosion and sediment transport can
change landscapes, and how human activity affects the evolution of
these waterways. Modelling subsurface fluid movements is equally as
important, though here has been some difficulty in this department.
Efficient
management of natural resources (like water) requires a sound
knowledge of the behaviour of both surface and subsurface fluids,
which allows scientists to predict fluid movements and their
interactions with the environment. But creating a mathematical model
representing these fluid movements has been problematic.
How has life
shaped Earth - and how has Earth shaped life?
Put another way,
this question seeks to illuminate how biology and geology interact.
But no matter how you want to put it, scientists are still in the
dark as to the exact nature of this relationship. Nonetheless, there
are many points of interest currently under investigation, including
how biological processes oxygenate Earth's atmosphere, and how
geological processes affect climate. And on a much grander scale,
scientists are also keen to understand how geological events caused
mass extinctions, which in turn shaped the course of evolution.
Geological and
biological interactions are of great interest to scientists because
their interactions produce a cyclical chain of events that, as the
question suggests, shape one another.
Other
sub-questions pertinent to the research of Earth's geo-biological
processes - which is a multidisciplinary investigation, involving
fields such as inorganic chemistry, physics, and hydrology - include
how long life has fostered a habitable surface environment, how
organisms influenced the oxygenation of the atmosphere and oceans,
and what factors govern the history of Earth's biological diversity.
These questions, together with the rest of the "big ten",
highlight the complexity inherent in the interactions between macro
and micro processes, and emphasize how difficult it is to find
causes to events that are geo-biological in nature, such as mass
extinctions.
But now armed with
a clearly defined set of probing questions, perhaps a clear history
of Earth's evolution will become apparent to Earth scientists over
the coming decades.
"To keep the
field moving forward," writes geochemist professor Donald J
DePaolo, the NRC report's committee chairman, "we have to look
to the past and ask deeper fundamental questions, about the origins
of the Earth and life, the structure and dynamics of planets, and
the connections between life and climate."
Our future
survival may
depend on it. |
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Baby
galaxy cluster discovered
A cluster of
galaxies in a very early stage of formation that is 11.4 billion
light years from Earth has been detected. These galaxies are so
distant that the universe was in its infancy when their light was
emitted...
Irvine scientists
have discovered a cluster of galaxies in a very early stage of
formation that is 11.4 billion light years from Earth - the farthest
of its kind ever to be detected. These galaxies are so distant that
the universe was in its infancy when their light was emitted.
The galaxy
proto-cluster, named LBG-2377, is giving scientists an unprecedented
look at galaxy formation and how the universe has evolved. Before
this discovery, the farthest
known event like this was approximately nine billion light years
away.
"When you
observe objects this far away, you are actually seeing the universe
as it was a very long time ago," said Jeff Cooke, a McCue
Postdoctoral Fellow in physics and astronomy at UCI and lead author
of this study. "It is as if a timeline is just sitting out
there in front of you. These galaxies represent what the universe
looked like well before the Earth existed."
Using the Keck
Telescope in Hawaii, Cooke detected LBG-2377 while looking for
single galaxies. At first, it appeared to be a bright, single
object. But after analysing the wavelengths of its light (galaxies
emit light with telltale colours) he discovered it was three
galaxies merging together, and likely two additional smaller
galaxies.
Scientists use
light to look back in time. Because light takes a measurable amount
of time to travel, detecting it on Earth today allows scientists to
view the source, as it was billions of years ago. In the case of
LBG-2377, scientists believe the light has been travelling for 11.4
billion years, beginning just a few billion years after the Big Bang
when the universe was only 15 percent of its current age. By
comparison, the Earth was formed about 4.5 billion years ago.
The process of
galaxy formation largely is a mystery. Current theory is that large
galaxies formed over time from the interaction and merging of
smaller galaxies. This process began more than 12 billion years ago,
shortly after the Big Bang. Scientists have observed galaxies
merging over a large range of distances and time, providing hard
evidence to reinforce the theory. However, using current technology,
it is difficult to detect this process at the most extreme
distances, when galaxy formation was in its infancy.
Scientists believe
galaxy clusters form in a similar manner. As galaxies congregate and
interact in large, dense regions of space, the cluster grows with
time. Witnessing this
process first-hand helps scientists confirm their theory and deepen
their understanding of the universe. Galaxy clusters can be detected
at extreme distances with current technology because they are
bright, but they are difficult to find.
Clusters closer to
Earth contain upwards of 1,000 galaxies. Our Milky Way galaxy
belongs to a lesser grouping of galaxies called the Local Group,
which contains more than 35 galaxies, but only a few bright ones.
"We believe
LBG-2377 is a seed that eventually will grow into a massive galaxy
cluster," said James Bullock, director of the Centre for
Cosmology at UCI and a study co-author.
"Our finding
suggests that this is a monster structure being born in a very
bright, catastrophic event with a lot of gas and matter collapsing
at once," Bullock said. "We are not just seeing one
solitary galaxy. We are seeing a bunch of bright galaxies coming
together at the dawn of structure formation in the universe."
Scientists
Elizabeth Barton and Kyle Stewart of UCI, along with Arthur Wolfe of
the University of California, San Diego, worked on this study.
--www.msnbc.com |
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Emission
reduction assumptions
for carbon dioxide overly optimistic
Reducing global
emissions of carbon dioxide over the coming century will be more
challenging than society has been led to believe
Reducing global
emissions of carbon dioxide (CO2) over the coming century will be
more challenging than society has been led to believe, according to
a research. The authors, from the University of Colorado at Boulder,
the National Centre for Atmospheric Research
(NCAR) in Boulder, and McGill University in Montreal, said the
technological challenges of reducing CO2 emissions have been
significantly underestimated by the Intergovernmental Panel on
Climate Change (IPCC).
The study
concludes the IPCC is overly optimistic in assuming that, even
without action by policymakers, new technologies that will result in
dramatic reductions in the growth of future emissions will be
developed and implemented.
Titled
"Dangerous Assumptions", the Nature commentary is
co-authored by scientists Roger Pielke, Jr., of CU-Boulder, Tom
Wigley of NCAR and economist Christopher Green of McGill University.
"This welcome
commentary is an indication that the science policy discussions have
shifted from 'is there global warming?' to 'how does society
respond?'" said Cliff Jacobs of the National Science Foundation
(NSF)'s Division of Atmospheric Sciences, which funds NCAR.
"In the end,
there is no question whether technological innovation is
necessary--it is," write the authors. "The question is to
what degree should policy focus explicitly on motivating such
innovation?"
"The IPCC
plays a risky game in assuming that business-as-usual advances in
technological innovation will carry most of the burden of achieving
future emissions reductions, rather than focusing on those
conditions that are necessary and sufficient for those innovations
to occur."
Recent changes in
"carbon intensity"--CO2 emissions per unit of energy
consumed--already are higher than those predicted by the IPCC
because of rapid economic development, says lead author Pielke. In
Asia, for instance, the demands of more energy-intensive economies
are being met with conventional fossil-fuel technologies, a process
expected to continue there for decades and eventually move into
Africa.
Atmospheric CO2
levels are currently about 390 parts per million. A commonly cited
goal is to stabilize concentrations at roughly 500 parts per million
or less.
Because technical
innovation is ongoing, the IPCC authors assume that most of the
needed reductions will occur automatically. According to
calculations by the authors, the IPCC assumes that 57 to 96 percent
of the total carbon removed from the energy supply will occur
automatically through such routine technological progress.
--www.scienceagogo.com |
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Eco-Logic
Laser used to get thunder clouds
sparking
Using a powerful
ground-based laser, European scientists were able to induce
electrical activity in thunderclouds, a precursor to stimulating
lightning strikes on demand. It is reported that the experiment was
conducted at the top of South Baldy Peak, in New Mexico, where the
laser pulses created electricity conducting plasma filaments in the
clouds. The filaments were too short-lived to create air-to-ground
lightning but the researchers believe that triggering actual
lightning strikes is not far away. "This was an important first
step toward triggering lightning strikes with laser beams," says
Jerome Kasparian of the University of Lyon in France. "It was
the first time we generated lighting precursors in a
thundercloud." The next step of generating full-blown lightning
strikes may come, he adds, after the team reprogramme their lasers to
use more sophisticated pulse sequences that will make longer-lived
filaments.
Shorebird
numbers crash in Australia
One of the world's
great wildlife spectacles is under way across Australia: as many as
two million migratory shorebirds of 36 species are gathering around
Broome before an
amazing 10,000-kilometre annual flight to their northern hemisphere
breeding grounds. But an alarming new study has revealed that both
these migrants and Australia's one million resident shorebirds have
suffered a massive collapse in numbers over the past 25 years. A
large scale aerial survey study covering the eastern third of the
continent by researchers at the University of New South Wales has
identified that migratory shorebirds populations there plunged by 73
percent between 1983 and 2006, while Australia's 15 species of
resident shorebirds - such as avocets and stilts - have declined by
81 percent. It is the first long-term analysis of shorebird
populations and health at an almost a continental scale and reveals a
disturbing trend of serious long-term decline.
Lizards
rapidly evolve after introduction to island
Italian
wall lizards introduced to a tiny island off the coast of Croatia are
evolving in ways that would normally take millions of years to play
out, new research shows. In just a few decades the five-inch-long
lizards have developed a completely new gut structure, larger heads,
and a harder bite, researchers say. In 1971, scientists transplanted
five adult pairs of the reptiles from their original island home in
Pod Kopiste to the tiny neighbouring island of Pod Mrcaru, both in
the south Adriatic Sea. Genetic testing on the Pod Mrcaru lizards
confirmed that the modern population of more than 5,000 Italian wall
lizards are all descendants of the original ten lizards left behind
in the 1970s.
Komodo
dragon's bite is "weaker than a house cat's"
The world's largest
living lizard, the fearsome Komodo dragon, has a bite weaker than a
house cat's, researchers say. Though known for killing prey much
larger than itself, t he
Komodo relies on its razor-sharp teeth, strong neck muscles, and
"space frame" skull to subdue its prey, according to a new
study. Using computer models, researchers from Australia's University
of New South Wales analysed a Komodo specimen from the Australian
Museum in Sydney. Measuring the forces and composition of the
lizard's skull, the researchers found that its jaw is not designed
for crushing. "The bite is really quite incredibly weak for such
a big lizard-less than you'd expect from the average house cat,"
said Stephen Wroe, author of the study. If a Komodo actually tried to
crush prey with its jaws, like crocodiles do, "it would break
its own skull," he said.
Captive
tigers harbour rare "purebred" genes
Nearly half of
tested captive tigers are "purebred" members of an
endangered subspecies, raising the possibility they could bolster
conservation efforts, a new genetic analysis
suggests. Similar screening of some of the thousands of tigers with
unknown heritage held on farms and by private owners would
considerably increase the number of animals useful for captive
breeding programmes, the scientists say. The news comes at a dire
time for wild tigers. As few as 3,000 individuals remain where more
than 100,000 roamed just a century ago. Three of the eight subspecies
have become extinct, and a fourth, the South China tiger, persists
only in zoos. The number of captive tigers, on the other hand, has
boomed. Zoos, farms, circuses, and private owners hold an estimated
15,000 to 20,000 tigers. Only a small fraction of these are part of
breeding programs oriented toward conservation.
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