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Monday, December 9, 2019

The long-term history of the Earth’s temperature and of CO2 in the atmosphere

CO2 levels in 
the atmosphere 
were higher 
than today 
for the first 
4 billion years 
of Earth’s 
4.5 billion year 
history.

Modern life formed 
in the past 540 million 
years.

During the Eocene 
Thermal Maximum, 
temperature was likely 
higher than at any time 
in the past 
550 million years, 
while CO2 had been 
on a downward track 
for 100 million years. 

We have been in a major 
cooling period since the 
Eocene Thermal Maximum, 
50 million years ago. 

The Earth was an average 
of +16 degrees C. warmer then, 
mainly at higher latitudes. 

The entire planet 
was ice-free.

The Arctic and Antarctica 
were covered in forests. 

The ancestors of every 
species on Earth today 
survived through what 
may have been the 
warmest time in the 
history of life. 

Glaciers began to form 
in Antarctica 30 million 
years ago, and in the 
northern hemisphere 
3 million years ago. 

Today, even in our 
interglacial "Holocene" 
period, of the Pleistocene 
Ice age, we have one 
of the coldest climates 
in Earth’s long history.

Antarctic ice cores show 
in the past 800,000 years 
there have been regular 
100,000 year cycles, 
including only 
10,000 to 15,000 
warm years out of
every 100,000 years,
called interglacials.

These 100,000 year
"Milankovitch cycles"
are linked to 
the eccentricity of 
the Earth’s orbit and 
its axial tilt, which affect 
the amount of incoming 
solar energy.

The Milankovitch cycles 
are far more likely to cause 
a change in temperature, 
than a change in CO2. 

And a change in 
the temperature 
would cause a change 
in atmospheric CO2, 
due to outgassing of CO2 
from the oceans, during 
warmer times, and
absorption of CO2 
by the oceans,
during colder periods. 

CO2 peaks lagged 
temperature peaks 
by an average 
of 800 years, 
during the 
most recent 
400,000-year period.

That would mean 
temperature 
changes 
CAUSED 
CO2 level 
changes.

A cause always 
comes before
an effect.



20,000 years ago 
was the peak of the 
last major glaciation. 

At that time, there was 
3.3 kilometres (2 miles) 
of ice on top of what is
now the city of Montreal.

95% to 100% 
of Canada 
was covered by
a sheet of ice. 

If the Milankovitch cycle 
continues to prevail, 
this will happen again, 
gradually, during the 
next 80,000 years. 


Could warming 
from CO2 emissions 
prevent another 
glaciation ?

I assume
any warming 
will have a 
positive effect.


At the height 
of the last glaciation, 
20,000 years ago, 
sea level was about 
120 meters (400 feet) 
lower than it is today. 

By 7,000 years ago, 
all low-altitude and
mid-latitude glaciers 
had melted. 

During the Holocene 
Thermal Optimum, 
from 9,000 to 5,000 
years ago, the Sahara 
was green. 

Temperature has risen 
at a slow rate in Central 
England since 1700.

Not from human 
CO2 emissions 
-- they were not 
relevant until 1900,
and not important
until 1950.

CO2 emissions  
began a much faster 
rise after 1950, 
yet there was 
no global warming 
before 1975.



Earth is 'greening' 
as higher levels of CO2, 
due to human emissions 
from the use of fossil fuels, 
promote increased plant 
growth around the world.


If humans had not begun 
to unlock some of the 
carbon stored underground, 
as coal oil and natural gas,
life on Earth would have 
been starved of CO2 
and plants would have
begunn to die off in 
one or two million years. 

if the Earth were 
considered to be
24 hours old, 
we were at 
38 seconds 
to midnight 
when we 
reversed 
the declining 
CO2 trend.

That trend would have 
eventually caused 
the death of all plants, 

and all life, on our planet.