Greetings, 
 
eco-loving viewers, 
 
and welcome to 
 
Planet Earth: 
 
Our Loving Home. 
 
On today's program 
 
we examine the effects 
 
of the short-lived climate 
 
forcer, Black Carbon, on ice masses 
 
and planetary warming, 
 
and the role 
 
that animal agriculture 
 
and deforestation 
 
for livestock raising 
 
play in intensifying 
 
Black Carbon's impact.
 
Black Carbon, 
 
also known as soot, is a 
 
powerful warming agent 
 
that originates from 
 
the incomplete combustion 
 
of fossil fuels, 
 
diesel exhaust, inefficient 
 
cook stoves mainly used 
 
in developing countries 
 
burning biomass such as 
 
dried dung, wood, brush, 
 
or crop residue as fuel, 
 
and the clearing forests 
 
and savannas with fire. 
 
 
When the Black Carbon 
 
particles are airborne, 
 
they have an intense 
 
warming effect, but have 
 
an even greater impact 
 
when they are deposited 
 
on ice masses. 
 
This is a major concern 
 
and why Black Carbon 
 
emissions need to be 
 
addressed immediately. 
 
Its atmospheric lifespan 
 
ranges from 
 
one to four weeks 
 
and its Global Warming 
 
Potential (GWP) 
 
over a 20-year timeframe, 
 
has been calculated to be 
 
between a staggering 
 
1,600 to 4,700 times 
 
the warming-power 
 
of carbon dioxide. 
 
Black Carbon's 
 
warming effect occurs 
 
in two ways: 
 
(1) In the atmosphere 
 
as black particles 
 
absorb sunlight 
 
and generate heat; and, 
 
(2) Particles are deposited 
 
on the Earth's surface, 
 
in particular on ice masses 
 
where they reduce 
 
the ability of the ice 
 
to reflect sunlight 
 
back into space 
 
and cause rapid melting 
 
by generating heat 
 
from absorbing sunlight. 
 
 
Professor Jefferson Simões 
 
is the director of the 
 
Brazilian National Institute 
 
for Cryospheric Sciences 
 
and a National Delegate 
 
to the Scientific Committee 
 
on Antarctic Research 
 
(SCAR). 
 
He created the first
 
national laboratory 
 
in Brazil dedicated to 
 
glaciology and 
 
geographical polar research, 
 
and recently gave an 
 
informative presentation 
 
on the presence 
 
of Black Carbon 
 
in Antarctica and 
 
its effect on ice masses 
 
at the November 3, 2010 
 
Leaders Preserving 
 
Our Future: 
 
Pace and Priorities 
 
on Climate Change 
 
conference in London, UK.
 
 
For more details 
 
about the organizations 
 
today's guests represent, 
 
please visit  
 
the following websites
 
Professor Jefferson Simões  
 
of the Brazilian 
 
National Institute 
 
for Cryospheric Sciences 
 
(Part of the Brazilian 
 
Ministry of Science 
 
and Technology)
 
www.CNPQ.br
 
John C. Topping 
 
of the Climate Institute 
 
www.Climate.org
 
Gerard Wedderburn-Bisshop 
 
of the World Preservation 
 
Foundation 
 
www.WorldPreservationFoundation.org