Dear All,

 

Please find attached the news release in full from the UK Meteorological 
Office. 

 

The mean Arctic annual temperature increase could be as high as +15.2C

while the North Pole may see the mean temperature to rise as much as +20C.

 

This suggests styrofoam and polystyrene ice substitution might be necessary.

Please draw your attention to the attached diagram where rises are > +16C.

 

In my view, sulphur oxide and carbon tetrasilicate do not dent the loss of sea 
ice.

Please give feedback on the Meteorological Office modeling what shall we do?

 

We better not to despair, but get our hands on and be prepared to put up fight.

I am not gonna give up for the sinking ship if the Met Office figures are 
correct.

 

I have reproduced the text exhaustively and with the original web link to Met 
Office.

 

With kind regards,

 

Veli Albert Kallio, FRGS

 

Frozen Isthmuses' Protection Campaign

of the Arctic and North Atlantic Oceans

 

 

http://www.metoffice.gov.uk/climatechange/news/latest/four-degrees.html

Four degrees and beyond
28 September 2009

 

If greenhouse gas emissions continue to rise unchecked, it is likely that 
global warming will exceed four degrees by the end of the century, research by 
Met Office scientists has revealed.

 

Our scientists, working on behalf of Department of Energy and Climate Change 
(DECC), have found that if current high emissions continue there could be major 
implications for the world — with higher temperature rises than previously 
thought.

 

Dr Richard Betts, Head of Climate Impacts at the Met Office Hadley Centre, 
presented the new findings at a special conference this month. 4 degrees and 
beyond at Oxford University, attended by 130 international scientists and 
policy specialists, is the first to consider the global consequences of climate 
change beyond 2 °C.

 

Dr Betts said: “Four degrees of warming, averaged over the globe, translates 
into even greater warming in many regions, along with major changes in 
rainfall. If greenhouse gas emissions are not cut soon, we could see major 
climate changes within our own lifetimes.”


High-end temperature change

Fig 1. Comparison of surface temperature projections from the high-end 
emissions scenario, without carbon cycle feedbacks. Temperature increases 
between 1961-1990 and 2090-2099, averaged over all high-end members.

 

In some areas warming could be significantly higher (10 degrees or more).

 


The Arctic could warm by up to 15.2 °C for a high-emissions scenario, enhanced 
by melting of snow and ice causing more of the Sun’s radiation to be absorbed.
For Africa, the western and southern regions are expected to experience both 
large warming (up to 10 °C) and drying.
Some land areas could warm by seven degrees or more.
Rainfall could decrease by 20% or more in some areas, although there is a 
spread in the magnitude of drying. All computer models indicate reductions in 
rainfall over western and southern Africa, Central America, the Mediterranean 
and parts of coastal Australia.
In other areas, such as India, rainfall could increase by 20% or more. Higher 
rainfall increases the risk of river flooding.
 

Dr Betts added: “Together these impacts will have very large consequences for 
food security, water availability and health. However, it is possible to avoid 
these dangerous levels of temperature rise by cutting greenhouse gas emissions. 
If global emissions peak within the next decade and then decrease rapidly it 
may be possible to avoid at least half of the four degrees of warming.”

 

A DECC spokesman said: “This report illustrates why it is imperative for the 
world to reach an ambitious climate deal at Copenhagen which keeps the global 
temperature increase to below two degrees.”









 




 

 
                                          
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