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An anthropogenic or artificial cloud, is a cloud induced by human activity. Although generally clouds covering the sky have only a natural origin, from the beginning of the Industrial Revolution, the use of fossil fuels and water vapor and other gases emitted by nuclear, thermal and geothermal power plants yield significant alterations of the local weather conditions. These new atmospheric conditions can thus enhance cloud formation. Anthropogenitus is the term used to designate the origin of clouds produced by human activities.
Contents
- Anthopogenesis
- Cloud classification
- Generating process
- High anthropogenitus
- Middle anthropogenitus
- Low anthropogenitus
- Experiments
- Influence on climate
- References
Various methods have been proposed for creating and utilizing this weather phenomenon. Experiments have also been carried out for various studies. For example, Russian scientists have been studying artificial clouds for more than 50 years. But by far the greatest number of anthropogenic clouds are airplane contrails (condensation trails) and rocket trails.
Anthopogenesis
Three conditions are needed to form a cloud:
- the air must be near saturation of its water vapor,
- the air must be cooled to the dew point temperature with respect to water (or ice) to condensate (or sublimate) part of the water vapor,
- the air must contain condensation nuclei, small solid particles, where condensation/sublimation starts.
The current use of fossil fuels enhances any of these three conditions. First, fossil fuel combustion generates water vapor. Additionally, this combustion also generates the formation of small solid particles that can act as condensation nuclei. Finally, all the combustion processes emit energy that enhance vertical upward movements.
Despite all the processes involving the combustion of fossil fuels, only some human activities, such as, thermal power plants, commercial aircraft or chemical industries modify enough the atmospheric conditions to produce clouds that can use the qualifier anthrogenitus due to its anthropic origin.
Cloud classification
The International Cloud Atlas published by the World Meteorological Organization compiles the proposal made by Luke Howard at the beginning of the 19th century, and all the subsequent modifications. Each cloud has a name in Latin and clouds are classified according to its genus, 'species, variety :
Further terms can be added to describe the origin of the cloud and using Genitus. Anthropogenitus as a suffix is thus a sign of the origin of the cloud that would be new to the World Atlas but that conforms to its spirit. Anthropogenitus should be added at the end of the name of the cloud. For instance Cumulus originated by human activity has to be named as Cumulus anthropogenitus and abbreviated by CUa.
It was uncorrectly proposed to use the prefix anthropo – before the name of the corresponding cloud (Mazon et al., 2012) has it would be a new genus.
Generating process
The international cloud classification divide the different genera in three main groups of clouds according to their altitude:
Anthropogenitus clouds will be generated by different sources at those different levels.
High anthropogenitus
Despite the three genera of high clouds, Cirrus, Cirrocumulus and Cirrostratus, form at the top of the troposphere, far from the earth surface, they may have an anthropogenic origin. In this case, the process that causes their formation is almost always the same: commercial and military aircraft flight. Exhaust products from the combustion of the kerosene expelled by engines provide water vapor to this region of the troposphere.
In addition, the strong contrast between the cold air of the high troposphere layers and the warm and moist air ejected by aircraft engines causes rapid sublimation of water vapor forming small ice crystals. This process is also enhanced by the presence of abundant nuclei of condensation produced as a result of combustion. These clouds are commonly known as condensation trails (contrails) and are initially lineal cirrus clouds that could be called Cirrus anthropogenitus (Cia). Due to the large temperature difference between the air exhausted and the ambiance air generates small-scale convection processes. These processes favor the evolution of the condensation trails to Cirrocumulus anthropogenitus (Cca).
Depending on the atmospheric conditions at the upper part of the troposphere, where the plane is flying, these high clouds rapidly disappear or persist. When the air is dry and stable, the water rapidly evaporates inside the contrails and can only observed up to several hundreds of meters from the plane. On the other hand, if humidity is high enough it exists an ice oversaturation and the anthropogenitus get wide and it can exist for hours. In the later case, depending on the wind conditions Cca may evolve to Cirrus anthropogenitus (aCi), or Cirrostratus anthropogenitus (Csa). The existence and persistence of these three types of high anthropogenic clouds may indicate the approximation of air stability. In some cases, when there is a large density of air traffic, these high anthropogenitus may inhibit the formation of natural high clouds, because the contrails capture most of the water vapor.
Middle anthropogenitus
The intermediate layers of the troposphere are the regions with less influence of human activity. This region is far enough from the surface for not being affected by the surface emissions. Additionally, commercial and military flights only cross this region during ascending or descending maneuvers. Moreover, in this region there exist two types of clouds with a large horizontal extension: Nimbostratus and Altostratus, which cannot originate from human activity. Consequently, it is assumed that there are no anthropic clouds of these two genera. However, what can occur is enhancing existing Nimbostratus or Altostratus due to the additional water vapor or condensation nuclei emitted by a thermal power plant, for instance.
The only anthropic clouds existing in the middle region of the troposphere are Altocumulus anthropogenitus (Aca) from contrails at this region.
Low anthropogenitus
The lowest part of the atmosphere is the region with the largest influence of human activity emission of water vapor, warm air, and condensation nuclei. When the atmosphere is stable, the additional contribution of warm and moist air from emissions enhances fog formation or layers of Stratus anthropogenitus (Sta). If the air is not stable, this warm and moist air emitted by human activities creates a convective movement that can reach the lifted condensation level producing an anthropic cumulus cloud, or Cumulus anthropogenitus (Cua). This type of clouds may be also observed over the polluted air covering some cities or industrial areas in high-pressure conditions.
Stratocumulus anthropogenitus (Sca) are anthropic clouds that may be formed due to the evolution of Sta if the atmosphere is slightly unstable or from Cua if the atmosphere is stable.
Finally, Cumulonimbus (Cb) presents such a great vertical development that only in some particular cases they can be created by anthropic causes. For instance, large wild fires may yield to the formation of pyrocumulus that can evolve to Pyrocumulonimbus cloud and nuclear explosions produce mushroom clouds.
Experiments
Anthropogenic cloud can be generated in laboratory or in situ to study its properties or use it for other purpose. A cloud chambers is a sealed environment containing a supersaturated vapor of water or alcohol. When a charged particle (for example, an alpha or beta particle) interacts with the mixture, the fluid is ionized. The resulting ions act as condensation nuclei, around which a mist will form (because the mixture is on the point of condensation). Cloud seeding, a form of weather modification, is the attempt to change the amount or type of precipitation that falls from clouds, by dispersing substances into the air that serve as cloud condensation or ice nuclei, which alter the microphysical processes within the cloud. The usual intent is to increase precipitation (rain or snow), but hail and fog suppression are also widely practiced in airports.
Numerous experiments have been done with those two methods in the troposphere. At higher altitudes, NASA studied inducing noctilucent clouds in 1960 and 2009. In 1984 satellites from three nations took part in an artificial cloud experiment as part of a study of solar winds and comets. A European satellite released and ignited barium and copper oxide 43,000 miles in space to create a 2,000 mile mauve and green plume visible for 22 minutes. It was part of a study of magnetic and electric fields.
Plans to create artificial clouds over soccer tournaments in the Middle East were suggested in 2011 as a way to help shade and cool down Qatar's 2022 FIFA World Cup.
Influence on climate
There are many studies dealing with the importance and effects of high anthropic clouds (Penner, 1999; Minna et al., 1999, 2003 y 2004; Marquart et al., 2002 y 2003; Stuber and Foster, 2006, 2007), but not about anthropic clouds in general. For the particular case of Cia due to contrails, IPCC estimates positive radiative forcing around 0.01 Wm−2.
When annotating the weather data, using the suffix that indicates the cloud origin allows differentiating these clouds form the ones with natural origin. Once this notation is established, after several years of observations, the influence of anthropogenitus on earth climate will be clearly analyzed.