http://www.terradaily.com/reports/The_role_of_bacteria_in_weather_events_999.html

The role of bacteria in weather events

A diverse range of particles are capable of serving as IN, but the most active 
naturally occurring IN are biological in origin, capable of catalyzing ice 
formations at temperatures near -2 degrees Celsius. The most well-studied 
biological IN is the plant pathogen Psuedomonas syringae.
by Staff Writers
New Orleans LA (SPX) May 27, 2011
Researchers have discovered a high concentration of bacteria in the center of 
hailstones, suggesting that airborne microorganisms may be responsible for that 
and other weather events. They report their findings at the 111th General 
Meeting of the American Society for Microbiology in New Orleans.
"Bacteria have been found within the embryo, the first part of a hailstone to 
develop. The embryo is a snapshot of what was involved with the event that 
initiated growth of the hailstone," says Alexander Michaud of Montana State 
University in Bozeman, who presented the research.

Michaud and his colleagues analyzed hailstones over 5 centimeters in diameter 
that were collected on the University campus after a storm in June 2010. The 
large hailstones were seperated into 4 layers and the meltwater from each layer 
was analyzed. The number of culturable bacteria was found to be highest in the 
inner cores of the hailstone.

"In order for precipitation to occur, a nucleating particle must be present to 
allow for aggregation of water molecules," says Michaud. "There is growing 
evidence that these nuclei can be bacteria or other biological particles."

Michaud's research is part of a growing field of study focusing on 
bioprecipitation, a concept where bacteria may initiate rainfall and other 
forms of precipitation including snow and hail. The formation of ice in clouds, 
which is necessary for snow and most rainfall events, requires ice nuclei (IN), 
particles that the ice crystals can grow around.

"Aerosols in clouds play key roles in the processes leading to precipitation 
due to their ability to serve as sites for ice nucleation. At temperatures 
warmer than -40 degrees Celsius ice formation is not spontaneous and requires 
an IN," says Brent Christner of Louisiana State University, also presenting at 
the meeting.

A diverse range of particles are capable of serving as IN, but the most active 
naturally occurring IN are biological in origin, capable of catalyzing ice 
formations at temperatures near -2 degrees Celsius. The most well-studied 
biological IN is the plant pathogen Psuedomonas syringae.

"Ice nucleating strains of P. syringae possess a gene that encodes a protein in 
their outer membrane that binds water molecules in an ordered arrangement, 
providing a very efficient nucleating template that enhances ice crystal 
formation," says Christner.

Aerosol-cloud simulation models imply that high concentrations of biological IN 
may influence the average concentration and size of ice crystals in clouds, 
horizontal cloud coverage in the free troposphere, precipitation levels at the 
ground and even insulation of the earth from solar radiation.

"Evidence for the distribution of biological IN in the atmosphere coupled with 
the warm temperatures at which they function as IN has implied that biological 
IN may play a role in the Earth's hydrological cycle and radiative balance," 
says Christner.


On 5/26/11 9:53 PM, "BHASKAR M V" <bhaskarmv...@gmail.com> wrote:

Hi John

Thanks, but the paper is about DMS.

DMS is produced by algae growing in oceans.

Bioprecipitation (biological rain) is due to bacteria (and algae and fungi) in 
the atmosphere.

regards

Bhaskar

On Thu, May 26, 2011 at 6:14 PM, JohnDuke <johnd...@johnduke.com> wrote:
See Charlson, Lovelock, Andreae, Warren 1987, paper attached (over 2000 
citations).

----- Original Message ----- From: "M V Bhaskar" <bhaskarmv...@gmail.com>
To: "geoengineering" <geoengineering@googlegroups.com>
Sent: Thursday, May 26, 2011 7:09 AM
Subject: [geo] Mineral Rain vs Biological Rain


Hi All

I thought that clouds only formed due to mineral actions and
artificial rain by cloud seeding was
done by using chemicals like silver iodide.

A report on Bioprecipitation says that bacteria, diatoms and fungi too
can cause clouds and rain.

Can this lead to a biological SRM solution?

Fertilize atmosphere over oceans with Diatoms and Nutrients and cause
clouds to form and the residual diatoms and Nutrients fall into oceans
with the rain and continue to bloom.

--------
http://www.livescience.com/14299-bacteria-create-rain-snow-hail.html

Surprising Find: Live Bacteria Help Create Rain, Snow & Hail

Living bacteria that get whipped up into the sky may be just the spark
needed for rain, snow and even hailstorms, research now finds.

Alexander Michaud of Montana State University in Bozeman, Mont., found
large amounts of bacteria at the centers of giant hailstones.

Traditionally, researchers have thought that minerals or other
particulates in clouds caused water droplets to glom together until
they were large enough to fall as raindrops, snowflakes and hail. The
new research shows that a large variety of bacteria, and even fungi,
diatoms and algae, persist in the clouds and can be used as
precipitation starters, a growing field of study called
bioprecipitation. (In order for snow, say, to fall from clouds,
particles around which ice crystals can form — called ice nuclei — are
needed.)

"Minerals were thought to be the dominant ice nucleators in the
atmosphere, but they aren't nearly as active as biological particles,"
said Brent Christner, a microbiologist studying bioprecipitation at
Louisiana State University who is presenting the work today (May 24)
at the General Meeting of the American Society for Microbiology in New
Orleans.

Bacterial beginnings

For minerals to form ice nuclei, water needs to be much colder than is
usually found in clouds, Christner told LiveScience. Bacteria and
other living particles that get swept up into the sky may serve as
alternative nucleators.

Michaud, also presenting at the conference, collected hailstones about
the size of golf balls (greater than 2 inches, or 5 centimeters, in
diameter) after a huge hailstorm hit Montana in June 2010. He
separated the hail into four layers, which are formed as the ice is
created and moves up and down through the clouds, accumulating layer
upon layer of ice. He found that bacteria levels were highest at the
core of the hail.

"Bacteria have been found within the embryo, the first part of a
hailstone to develop. The embryo is a snapshot of what was involved
with the event that initiated growth of the hailstone," Michaud said
in a statement. "There is growing evidence that these nuclei can be
bacteria or other biological particles."

By determining the temperature at which the hailstones formed, the
team found that these bacteria allowed the ice to form at warmer
temperatures than otherwise expected.

Importance of ice

Previously Christner's group found that the widely studied plant
pathogen Psuedomonas syringae plays an important role in snow
formation all over the world, including Antarctica, where there are
few plants. The pathogen is known to be very good at creating ice at
temperatures above the normal freezing point of water.

These bacteria are equipped with a special substance that binds water
molecules in an orderly arrangement, and in these proximities they can
more easily form ice particles. When on the ground, the bacteria use
this ice to damage plants, causing the plant cells to break apart and
allowing the bacteria to enter.

"An organism that lives on a plant, where you want to be is back on
the ground on another plant. If you have the ability to produce
precipitation, fall down and land on a plant, it could be a cycle,"
Christner told LiveScience. "They could be using this protein as a way
to hitchhike on the water cycle."

Their presence on the ground, and in the clouds, could influence
weather conditions and cycles.
------------------------

regards

Bhaskar

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