Number 658, October 21, 2003
by Phillip F. Schewe, Ben Stein, and James Riordon
Direct Imaging of Extrasolar Planets
Direct imaging of extrasolar planets might be easier than astronomers
thought, a new study shows. Evidence for the existence of planets around
nearby stars comes mostly in the form of tiny Doppler shifts in the
star's spectra as one or more orbiting planets tug on the star. In a
few cases the transit of a planet across the face of a star can be detected
from a minute dimming of the star's emission. These approaches are indirect.
The problem of imaging extrasolar planets directly is that the planet
is far outshone by the nearby star. One proposed way of getting around
this glare problem is to use nulling interferometry. In ordinary interferometry
the light waves from two or more telescopes are added together in such
a way that the resulting observation is equivalent to one made with
a single telescope with a much wider diameter than any of the component
scopes. But instead of maximizing the composite signal from the distant
object, it can be minimized (see past
Update item). By doing this, a weaker nearby object, like a planet,
might suddenly emerge from what had been irrepressible glare.
In a new paper, William Danchi (Goddard Space Flight Center) and his
colleagues have performed extensive studies of the interferometry nulling
technique, especially the way in which increasing the precision of component
detectors increases the degree to which the star's image is truly nulled,
the better to see either smaller planets or planets that are closer
in toward their parent star. Both the smaller and closer criteria are
pertinent when searching for earth-like extrasolar planets. Danchi
(301-286-4586) says that the new study shows that with the right configuration
of detectors, the spatial resolution of the overall interferometer (which
is related to its size) can be less than have been thought, an important
consideration for what would be an orbiting space-based observatory.
Danchi envisions that a first-round nulling interferometer using two
half-meter-sized telescopes separated by a 12-meter boom could observe
already discovered extrasolar planets (including spectroscopic studies
of atmospheres). With a later, larger version of the nulling interferometer
one could hope to search for earthlike planets harboring characteristic
molecules such as ozone, and/or oxygen, plus carbon dioxide, water,
and methane. Detecting these molecules could help determine the age
of the planet and what life processes might be occurring there. (Danchi,
Deming, Kuchner, and Seager, Astrophysical Journal Letters,
1 November 2003; preprint astro-ph/0309361)
Evidence for an Unusually Active Sune
Evidence for an unusally active sun since the 1940s comes from a new
estimation of sunspots back to the ninth century. Many natural phenomena
such as solar radiance and sunspots vary according to natural cycles.
The variation is subject also to additional fluctuations (arising from
as yet unexplained effects) which complicate any study which examines
only a short time interval. The longer the baseline, the more confident
one can be in drawing out historical conclusions. In the case of sunspots,
the direct counting goes back to Galileo's time, around 1610. But earlier
sunspot activity can be deduced from beryllium-10 traces in Greenland
and Antarctic ice cores. The reasoning is as follows: more sunspots
imply a more magnetically active sun which then more effectively repels
the galactic cosmic rays, thus reducing their production of Be-10 atoms
in the Earth's atmosphere. Be-10 atoms precipitate on Earth and can
be traced in polar ice even after centuries. Using this approach, scientists
at the University of Oulu in Finland (Ilya
Usoskin, 358-8-553-1377) and the Max Planck Institute in Katlenburg-Lindau
in Germany have reconstructed the sunspot count back to the year 850,
nearly tripling the baseline for sunspot studies. They conclude that
over the whole 1150 year record available, the sun has been most magnetically
active (greatest number of sunspots) over the recent 60 years. (Usoskin
et al., Physical Review Letters,
upcoming article)
Can a Single Gas Bubble Sink a Ship?
Yes, according to an experimental and theoretical analysis performed
by researchers at Monash University in Australia (David May and Joseph
Monaghan). The ocean floor contains vast quantities of methane gas
hydrates, ice-like crystals of methane surrounded by cages of water
molecules. If disturbed, these methane gas hydrates can erupt from the
floor and rise to the surface as gas bubbles, some of which can be very
large. Copious amounts of methane hydrates exist in the North Sea, which
lies in between the United Kingdom and continental Europe. At a large
eruption site in the North Sea known as the Witches Hole off the coast
of Aberdeen, a sonar survey recently uncovered the presence of a sunken
vessel, but the cause of the wreck remains undetermined. Simple experiments
have previously shown that many small bubbles rising to the surface
could sink a cylinder of water (and conceivably a ship), by causing
a loss of buoyancy (Denardo
et al., American Journal of Physics, October 2001). But could
a single large gas bubble do the trick? The Monash researchers investigated
this possibility in a simple, roughly two-dimensional system. Trapping
water between a pair of vertical glass plates, and launching single
gas bubbles from the bottom, they used a video camera to observe a single
large bubble's effect on a small piece of acrylic shaped like the hull
of a boat. Along with numerical simulations of this scenario, the experiments
showed that the bubble could sink the ship, if the bubble's radius was
comparable to or greater than the ship's hull. Sinking would occur because
a mound of water formed above the bubble as it approached the surface.
As the bubble reached the surface, it would temporarily lift the ship.
However, water in the mound would then flow off the sides of the bubble,
forming deep troughs at either side, and the water flow would carry
the boat to one of the troughs. In addition, the eventual rupture of
the bubble would create high-velocity jets of fluid that moved into
the troughs, creating vortices that further pulled down the boat. The
researchers say that their numerical simulations could test other scenarios,
including those involving multiple large bubbles, more realistic boats,
and ultimately a full three-dimensional simulation. (American
Journal of Physics, September 2003).