The clouds reflecting sunlight back into space reduces warming. But you have not even touched on the cooling caused by rain and evaporation.
Timeline data from 1990 -1995. From the International Satellite Cloud Climatology Project (ISCCP)
Clouds cool Earth’s surface by reflecting incoming sunlight.
Clouds warm Earth’s surface by absorbing heat emitted from the surface and re-radiating it back down toward the surface.
Clouds warm or cool Earth’s atmosphere by absorbing heat emitted from the surface and radiating it to space.
Clouds warm and dry Earth’s atmosphere and supply water to the surface by forming precipitation.
Clouds are themselves created by the motions of the atmosphere that are caused by the warming or cooling of radiation and precipitation.
If the climate should change, then clouds would also change, altering all of the effects listed above. What is important is the sum of all these separate effects, the net radiative cooling or warming effect of all clouds on Earth. For example, if Earth’s climate should warm due to the greenhouse effect, the weather patterns and the associated clouds would change; but it is not known whether the resulting cloud changes would diminish the warming (a negative feedback) or enhance the warming (a positive feedback). Moreover, it is not known whether these cloud changes would involve increased or decreased precipitation and water supplies in particular regions. Improving our understanding of the role of clouds in climate is crucial to understanding the effects of global warming.
A doubling in atmospheric carbon dioxide (CO2), predicted to take place in the next 50 to 100 years, is expected to change the radiation balance at the surface by only about 2 percent. Yet according to current climate models, such a small change could raise global mean surface temperatures by between 2-5°C (4-9°F), with potentially dramatic consequences.
Timeline data from 2022 . Now let’s fast forward 30 years.
Evaluations of the Climatologies of Three Latest Cloud Satellite Products Based on Passive Sensors (ISCCP-H, Two CERES) against the CALIPSO-GOCCP
Clouds cover a large portion of the Earth’s atmosphere at any given time and play a significant role in the weather and climate systems of the Earth by regulating its radiative balance and hydrological cycle. Based on numerous International Plan on Climate Change (IPCC) reports and modeling studies the current general circulation models (GCMs) suffer from significant uncertainties in predicting the future climate. One of the main sources of these uncertainties is believed to be related to the representation of clouds.
What is hot on the radar screen today? Radiative Energy Flux Variation from 2001–2020
What are they talking about? Heat comes from the sun. We have different wavelengths of energy that can change with the sun’s many cycles. For example, this connection can be matched to how Co2 is warmed. Example, sunlight can warm colors differently due to wavelengths of the light and wavelength of the color. Carbon dioxide (CO2) molecules have four different vibration modes. The ability to absorb infrared waves is what makes carbon dioxide a greenhouse gas.
What are the questions trying to be answered today?
Two independent measures and reanalysis agree that the sensitivity to CO2 is less than modeled because some to most of the warming of the last two decades is from solar, not CO2.
Which simply means that there is natural variability in the global energy dynamic that is combined with slow but inexorable anthropogenic climate forcing.
The big picture stated by J. J. Braccili - Fluctuations do not impact planetary temperatures. To cause a continuous increase in planetary temperature requires a continually increasing energy source. Fluctuations are nothing more than noise. Climate has always changed – Earth system science 101. Climate doesn’t vary for no reason. It takes energy to make the climate change.
Robert I. Ellison say it this way. ‘The top-of-atmosphere (TOA) Earth radiation budget (ERB) is determined from the difference between how much energy is absorbed and emitted by the planet. Climate forcing results in an imbalance in the TOA radiation budget that has direct implications for global climate, but the large natural variability in the Earth’s radiation budget due to fluctuations in atmospheric and ocean dynamics complicates this picture.’
