hydrates locked at the seabed

may be released to the atmosphere.

The photosynthetic algae and other micro plants

of the oceans will be destroyed due to the warming and CO

capture

capacity reduces considerably.

to the atmosphere due to the solubility issues.

, CFCs

and HFCs will rise to the stratosphere destroying the ozone layer rapidly,

causing UV rays reach the earth.

Large collection of debris/rock between Earth

and Mars.

Large collection of rock/debris between Mars and

Jupiter

Large cloud of rocks out of solar system but very

close to it.

ElNino is the periodic cooling of sea-surface

temperatures across the east-central equatorial Pacific.

ElNino is an occasional incursion of cold water

along the coast of France.

ElNino is an occasional incursion of warm water

along the coast of Peru.

ElNino is a perennial incursion of cold water

along the coast of Peru.

in the atmosphere and burial of the organic carbon in the marine sediments.

in the atmosphere and final burial of organic carbon in the marine sediments.

the simultaneous accumulation of Oxygen in the

atmosphere, draw down of CO

from the atmosphere and final burial of

organic carbon in the marine sediments.

the simultaneous accumulation of Nitrogen and Oxygen

in the atmosphere and draw down of CO

from the atmosphere to the

oceans.

Troposphere

– stratosphere – Mesosphere - Ionosphere

roposphere

– stratosphere – Ionosphere - Mesosphere

Mesosphere

– stratosphere – Troposphere - Ionosphere

Mesosphere

– stratosphere – Ionosphere - Troposphere

CLC can be easily carried

out using any metal oxide.

and unused Oxygen come out of the air reactor.

During CLC, although

CO

, it is mixed

up with water vapour that is very difficult to separate.

CLC is an advanced

Carbon Sequestration method.