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Thursday, April 16, 2020

Looking at clouds from both sides now

Climate is a complex system, 
composed of many different 
processes, showing non-linear 
relations between variables.

Earth's atmosphere 
can be considered 
as a closed non-linear 
thermodynamic system.

The thermodynamic 
state is maintained by 
a balance between 
incoming solar radiation,
heating the planet,
and outgoing shortwave 
and longwave radiation,
cooling the planet.

The energy 
balance is 
affected  by 
the incoming 
and outgoing
radiation.

Changes in the
energy balance 
of the atmosphere 
are the drivers 
of climate change.

It is believed 
that Earth absorbs 
slightly more energy 
from the Sun, than is 
emitted back to space, 
thanks to increasing 
amounts of CO2 
in the atmosphere, 
creating an energy 
imbalance.

Energy 
imbalance 
has been 
investigated 
using satellites
and models, 
and it seems 
to be increasing 
in the last decades.

Those changes 
have been argued 
to be due to human 
activities.

When reaching 
the Earth, part of 
the incoming 
solar radiation 
is reflected 
off the clouds, 
and the surface, 
as shortwave 
radiation (SW). 

Changes in the
cloud distribution, 
or surface albedo 
      ( reflectivity), 
will change the 
energy balance. 

In the last 
four decades,
changes in 
cloud distribution
of low-level clouds, 
such as subtropical
stratocumulus, 
have been important.

They have the ability 
to reflect large 
amounts of radiation 
back to space,
but do not 
significantly 
reduce outgoing 
radiation cooling 
our planet.

The rest 
of the radiation 
is absorbed 
by the atmosphere, 
or passes through 
to the Earth’s surface.


Shortwave and 
longwave radiation 
are strongly related, 
and changes in one, 
influence the behavior 
of the other. 

When analyzing 
both together, 
measures 
of correlation
do not give 
us information 
about causality
( which variable is 
driving the system? ).


Changes in 
the incoming 
or outgoing 
radiation can
generate an 
energy imbalance 
which drives 
climate change.

Clouds and 
surface albedo 
HAVE changed 
in the last four 
decades.

SW radiation has 
more influence 
on the system.

So clouds 
and albedo, 
which ultimately 
determine the 
SW radiation, are 
important variables 
for climate change

The Decadal Survey 
for Earth Science and 
Applications from Space 
(2018) lists as one of the
key science questions
“How changing 
cloud cover 
and precipitation 
will affect climate, 
weather and Earth’s
energy balance 
n the future”. 


It is not possible 
to guarantee 
that clouds 
are the only 
climate change 
factor, because
climate is a 
complex, highly 
interconnected 
system. 

As usual, with 
real science,
there are many
unanswered
questions
-- the science 
is far from 
being "settled".