Spring in Antarctica heralds new U.S. science efforts on several
fronts: a series of cruises in the Southern Ocean to trace carbon
cycling associated with plankton blooms; drilling to assess the
stability of the massive ice sheets; and an expedition to search for
more meteorites on the continent that yielded ALH84001, the now-famous
meteorite from Mars that may contain fossil life.
The National Science Foundation (NSF) is supporting approximately
145 Antarctic investigations, based mainly out of three research
stations during Antarctica's summer, from now through February.
The bulk of the research -- astronomy and astrophysics, earth
science, glaciology, oceanography, atmospheric science, and biology --
is supported out of NSF's McMurdo Station, located on Ross Island, and
at Amundsen-Scott South Pole Station, inland on the heights of the ice
cap. Other projects are based at Palmer Station on the Antarctic
Peninsula and on two research vessels.
- Carbon and Climate in the Southern Ocean
Scientists led by Robert Anderson of Columbia University and
Walker Smith of the University of Tennessee are mounting a major
effort to understand the role of the Southern Ocean in the global
cycle of carbon, and ultimately to predict the ocean's response to
climate change. As the southern component of the decade-long Joint
Global Ocean Flux Study (JGOFS), a study of carbon in the world's
oceans, thirteen cruises aboard two ships -- the National Science
Foundation's icebreaking research vessel, the Nathaniel B. Palmer, and
the University National Oceanographic Laboratory System ship Thomas G.
Thompson -- will take place from September, 1996 through March, 1998.
This field season's cruises will center mainly on the Ross Sea,
starting with a cruise embarking in early October to study
Antarctica's largest and most predictable spring bloom of
phytoplankton in these waters, and its role in the carbon cycle. Two
subsequent cruises will track carbon over the season, and investigate
how trace metals, especially iron, affect plant production.
- Deicing Dynamics of Sea Life
The growth and retreat of sea ice around Antarctica is one of the
world's great seasonal events, yet little is known about how ice
dynamics affect zooplankton and other animals in the ocean's topmost
waters (the upper 100 meters). Three cruises in the Weddell Sea and
associated studies, under a project led by Kenneth Smith of the
Scripps Institution of Oceanography, will track the ecology of tiny
animals -- zooplankton (floating) and micronekton (swimming) -- over
one year, to capture how dramatic changes in sea-ice cover affect the
animal populations. The project will develop an instrument to monitor
populations at different depths, and will launch a remotely-operated
vehicle to sample and observe animals beneath the sea ice.
- The Rougher It Is, The Better They Like It
Biologists now agree that archea, or archeobacteria, are one of
the three major branches of life, in addition to bacteria and
eukaryotes (the latter embracing plants, animals, and humans). Archea
seem to like environments that are very hot, or very salty, or
strictly lacking in oxygen -- places where no other life can endure.
Recent studies, however, reveal a surprise: archea comprise more
than 30 percent of biomass in waters off Palmer Station, Antarctica --
the highest rates measured in the ocean. A team led by Edward DeLong
of the University of California-Santa Barbara will sample archea in
the region this season, illuminating the ecology and biology of these
mysterious organisms.
- Hot and Ultraviolet
The greater amount of ultraviolet light (called UV-B) let in by
the ozone hole reduces the productivity of marine phytoplankton, but
how does UV-B affect Antarctica's terrestrial plants? How are such
plants reacting to the 50-year warming trend around the Antarctic
Peninsula? Thomas Day of the University of Arizona and his team will
study the impact of UV-B and warming on the health of two vascular
plant species near Palmer Station on the Antarctic Peninsula. The
study may shed light on the possible consequences of global warming
for land plants.
- Drilling an Ice Dome in West Antarctica
Fast-flowing ice streams, analogous to rivers, drain part of West
Antarctica's ice sheet out to the floating Ross Ice Shelf, and hence
to the sea. How permanent is this ice sheet, which is actually
anchored below sea level? As part of a major, multi-year initiative,
the West Antarctic Ice Sheet program, scientists led by Kendrick
Taylor of the Desert Research Institute will begin drilling a
1000-meter core from Siple Dome, a rise of ice located between two ice
streams on the coast of the Ross Sea, and a critical location for
taking the ice sheet's pulse.
The core's ice record is expected to span 80,000 years, including
part of the last glaciation, and to have distinct annual ice layers
back at least 6,000 years. The core will shed light on coastal
climate and ice stream dynamics in the past. It will also be compared
with the famous deep cores from the Greenland ice sheet, to assess
whether the rapid climate changes recorded in Greenland had a global
reach.
- Flying Above the Rift
If West Antarctica's ice melted, sea level would rise worldwide
by six meters. West Antarctica's swift ice streams lie above a
geologic rift -- an area where the earth's crust is pulling apart,
possibly with profound effects on the ice streams' behavior, and hence
on the ice sheet's overall stability. An aerogeophysical survey headed
by Donald Blankenship of the University of Texas at Austin and Robin
Bell of Lamont-Doherty Earth Observatory is tracing how the sub-ice
rift architecture affects the ice streams. The team uses an aircraft
fitted with geophysical instruments to image the surface and bed of the
ice sheet, while measuring the gravity and magnetic signature, a clue
to volcanism of the rock beneath (this year's survey focuses on Ice
Stream "D").
- Vostok: The World's Deepest and Oldest Ice Core
Drilling to complete the world's deepest and oldest ice core will
continue at Russia's Vostok Station in East Antarctica this season.
Some 30 researchers from the United States, France, and Russia study
the ice record, expected to stretch back perhaps half a million years.
Studies of Vostok's ice have already shown a close link between
climate over the past 200,000 years and changing concentrations of
greenhouse gasses in the atmosphere. The drillers plan to halt at
approximately 3650 meters depth, stopping above Lake Vostok, the
subglacial lake beneath Vostok Station that is comparable in size to
Lake Ontario. The lake and any life it may harbor have apparently
been sealed off from the atmosphere for hundreds of thousands of
years. NSF provides flight support for the project and grants to
glaciologists studying the ice core.
- More Favorite Martians?
The news last summer that ALH84001, a meteorite from Mars found
in Antarctica's Allan Hills, may contain fossils of early life
startled scientists and the public. It also drew the spotlight to the
Antarctic Search for Meteorites, akin to a bargain-priced space
mission on snowmobiles led by Ralph Harvey of Case Western Reserve
University. Antarctica is actually unrivaled in its abundance of
meteorites. Since 1976, the program has found more than 7800
specimens, including samples of the Moon and Mars, expanding knowledge
of the primeval nebula that have birth to the solar system. This
season, the team returns to the Allan Hills and will search other
locations as well.
- AMANDA Expands Its Neutrino Search
Antarctica's ice sheet serves as the detector for an unusual
neutrino telescope, the Antarctic Muon and Neutrino Detector Array
(AMANDA), a project based at the South Pole. AMANDA seeks to map the
sources of the ghostly subatomic particles called neutrinos -- whether
they come from active galactic nuclei, supernovae remnants, pulsars,
neutron stars, or from elsewhere in or outside the galaxy. Such
studies are at the forefront of the new field of neutrino astronomy.
The array already offers some provocative results. From a sample
during the first nine months of observations, AMANDA has spotted about
12 particles that seem to be evidence of incoming neutrinos. This
season, hot-water drillers will bore out holes to install seven new
strings of detectors 2,000 meters deep, to join the four strings
already embedded in the ice sheet.
- Probing the Aurora
When the sixth Automatic Geophysical Observatory is put into
place in a remote location on the Antarctic ice cap this season, it
will complete a network of instruments that take continuous
measurements of the aurora and the polar ionosphere (the highest layer
of the earth's atmosphere). The AGOs will furnish data that could
otherwise be collected only by an entire flotilla of spacecraft.
- Retrieving the Flare Genesis Telescope
One of the world's largest solar telescopes circled Antarctica
last year suspended from a giant balloon, and taking advantage of the
24-hour-long light, imaged sunspots and mapped associated magnetic
fields which are believed to cause solar flares. The balloon was cut
down above the Adelie Coast, 1400 kilometers from McMurdo Station, but
foul weather permitted only the data recorder to be retrieved. This
year, the French Antarctic program will assist the U.S. by mounting a
traverse to recover the balloon payload, including the $10-million
telescope.
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