Global atmospheric electrical circuit explained

A global atmospheric electrical circuit is the continuous movement of atmospheric charge carriers, such as ions, between an upper conductive layer (often an ionosphere) and surface. The global circuit concept is closely related to atmospheric electricity, but not all atmospheres necessarily have a global electric circuit.[1] The basic concept of a global circuit is that through the balance of thunderstorms and fair weather, the atmosphere is subject to a continual and substantial electrical current.

Principally, thunderstorms throughout the world carry negative charges to the earth, which is then discharged gradually through the air away from the storms, in conditions that are referred to as "fair weather".

This atmospheric circuit is central to the study of atmospheric physics and meteorology.[2] The global electrical circuit is also relevant to the study of human health and air pollution, due to the interaction of ions and aerosols. The effects of climate change and temperature-sensitivity of the Earth's electrical circuit are currently unknown.[3]

History

The history of the global atmospheric electrical circuit is intertwined with the history of atmospheric electricity. For example, in the 18th century, scientists began understanding the link between lightning and electricity. In addition to the iconic kite experiments of Benjamin Franklin and Thomas-François Dalibard, some early studies of charge in a "cloudless atmosphere" (i.e. fair weather) were carried out by Giambatista Beccaria, John Canton, Louis-Guillaume Le Monnier and John Read.[4]

Fair weather measurements from the late 18th century onwards often found consistent diurnal variations. During the 19th century, several long series of observations were made. Measurements near cities were (and still are) heavily influenced by smoke pollution. In the early 20th century, balloon ascents provided information about the electric field well above the surface. Important work was done by the research vessel Carnegie, which produced standardised measurements around the world's oceans (where the air is relatively clean).

C. T. R. Wilson was the first to present the concept of a global circuit in 1920.[5]

Mechanism

Lightning

See main article: Lightning. There are about 40,000 thunderstorms per day, generating roughly 100 lightning strikes per second,[6] which can be thought to charge the earth like a battery. Thunderstorms generate an electrical potential difference between the earth's surface and the ionosphere, mainly by means of lightning returning current to ground. Because of this, the ionosphere is positively charged relative to the earth.Consequently, there is always a small current of approximately 2pA per square metre transporting charged particles in the form of atmospheric ions between the ionosphere and the surface.

Fair weather

This current is carried by ions present in the atmosphere (generated mainly by cosmic rays in the free troposphere and above, and by radioactivity in the lowest 1km or so).The ions make the air weakly conductive; different locations, and meteorological conditions have different electrical conductivity. Fair weather describes the atmosphere away from thunderstorms where this weak electrical current between the ionosphere and the earth flows.[7]

Measurement

The voltages involved in the Earth's circuit are significant. At sea level, the typical potential gradient in fair weather is 120 V/m. Nonetheless, since the conductivity of air is limited, the associated currents are also limited. A typical value is 1800 A over the entire planet.When it is not rainy or stormy, the amount of electricity within the atmosphere is typically between 1000 and 1800 amps. In fair weather, there are about 3.5 microamps per square kilometer (9 microamps per square mile).[8]

Carnegie curve

The Earth's electrical current varies according to a daily pattern called the Carnegie curve, caused by the regular daily variations in atmospheric electrification associated with the earth's stormy regions.[9] The pattern also shows seasonal variation, linked to the earth's solstices and equinoxes. It was named after the Carnegie Institution for Science.

See also

External sources

Publications

Notes and References

  1. Aplin . K L . 2022 . The charge of the spheres . Astronomy and Geophysics . 63 . 4 . 4.12-4.17.
  2. Harrison . R. G. . 2004-11-01 . The Global Atmospheric Electrical Circuit and Climate . Surveys in Geophysics . en . 25 . 5 . 441–484 . 10.1007/s10712-004-5439-8 . 1573-0956. physics/0506077 .
  3. Web site: Soaking in atmospheric electricity Science Mission Directorate . 2017-11-05 . science.nasa.gov . en.
  4. Bennett. A. J.. Harrison. R. G.. 2007-10-01. Atmospheric electricity in different weather conditions. Weather. en. 62. 10. 277–283. 10.1002/wea.97. 1477-8696. 2007Wthr...62..277B. free.
  5. Aplin . K. L. . Harrison . R. G. . Rycroft . M. J. . 2008-06-01 . Investigating Earth's Atmospheric Electricity: a Role Model for Planetary Studies . Space Science Reviews . en . 137 . 1 . 11–27 . 10.1007/s11214-008-9372-x . 1572-9672.
  6. https://feynmanlectures.caltech.edu/II_09.html Electricity in the Atmosphere – Feynman Lectures
  7. Harrison . R. G. . Nicoll . K. A. . 2018-11-01 . Fair weather criteria for atmospheric electricity measurements . Journal of Atmospheric and Solar-Terrestrial Physics . en . 179 . 239–250 . 10.1016/j.jastp.2018.07.008 . 1364-6826. free .
  8. Web site: Electric current through the atmosphere. Terry. Mathew. 2006. The Physics Factbook. Elert. Glenn. 2022-01-25.
  9. Harrison. R. Giles. 2013-03-01. The Carnegie Curve. Surveys in Geophysics. en. 34. 2. 209–232. 10.1007/s10712-012-9210-2. 0169-3298. 2013SGeo...34..209H. free.

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