CLIMATE CHANGES

COP29 – UN Climate Conference BAKU (Azerbaijan)

What Is the Greenhouse Effect?

Our planet receives energy from the Sun mostly as ultraviolet (UV), visible (V) and infrared (IR) radiation. About 70% of that energy is absorbed by the Earth’s surface, while the rest is reflected into the Cosmos. The absorbed part warms up the surface temporarily. During the night that energy is emitted from the surface into the outer space in the form of infrared (thermal) radiation. One part of it is absorbed by IR active gases (greenhouse gases) close to the Earth’s surface and remains trapped in the atmosphere. In this way the atmosphere acts as a warming blanket that allows the average temperature of the Earth’s surface to be significantly higher than it would be without this mantle. It is the greenhouse effect.

The greenhouse effect is a natural process of crucial importance for the existence of life on Earth. Without it, the average annual temperature of the Earth’s surface would be about -18 ºC, instead of 14.2 ºC, as it was in the mid-twentieth century (see diagram), before the steep increase, which occurred due to the increase of concentrations of gases with the greenhouse effect. That increase is more than the Earth could absorb. It makes the Earth’s „blanket“ thicker, which leads to so-called global warming. Unfortunately, it still happens.

More greenhouse gases means a warmer Earth.

Greenhouse Gases (GHG)

Earth’s atmosphere contains two types of gases:

  • Homonuclear gases, those whose molecules are composed of the same atoms (nitrogen-N2, 78%, and oxygen-O2, 21%), which are the main components of the Earth’s atmosphere and which are not active in terms of absorbing IR radiation (heat);
  • Heteronuclear gases – their molecules are composed of different elements and are therefore IR active: carbon dioxide, water vapor, methane, nitrous oxide, fluorinated gases. Regardless of the fact that their concentrations in the atmosphere are very low, they have a huge effect on the climate. All of them are of natural origin with the exception of fluorinated gases.
  1. Carbon dioxide-CO2 is created in various processes on Earth and is continuously exchanged among land, water, atmosphere and living organisms, but it is also created as a product of human activities, especially from the combustion of fossil fuels.
  2. Water vapor-H2O enters the atmosphere in different ways, mainly from oceans and other water reservoirs. It is in constant equilibrium with liquid water on Earth. It is also created in the processes of burning some fossil fuels (oil and natural gas). However, its concentration in the atmosphere is not a function of those processes, as is the case with other greenhouse gases. It is mainly determined by temperature: warmer air – more water vapor. Since the increase in the temperature of the atmosphere is still small, regardless of global warming, it can be considered that its concentration is relatively constant.
  3. Methane-CH4 is a gas with powerful greenhouse potential. It enters the atmosphere from various processes in nature, such as rotting, processes in wetlands, animal digestion, etc. as well as from the exploitation of natural gas, which we use as a source of energy, and which is mainly composed of methane.
  4. Nitrous oxides-N2O are released from agriculture, burning of fossil fuels, etc.
  5. Fluorinated gases (hydrofluorocarbons-HFCs, perfluorocarbons-PFCs, nitrogen trifluoride-NF3, and sulfur hexafluoride-SF6) are artificial chemicals. Therefore, their production, usage and release into the atmosphere can be more easily controlled. Their concentrations are very low, but they have huge worming potential.

Global GHG emission is currently over 51 billion tons of carbon dioxide-equivalents per year!!!

SAVE THE PLANET

PARAMETERS RELATED to GLOBAL WORMING for greenhouse gases – Lifetime and GWP100

GLOBAL GHG EMISSIONS PER YEAR from the beginning of the industrial era

EARTH’s SURFACE TEMPERATURE CHANGES since the beginning of the industrial era.

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