Science, Art, Litt, Science based Art & Science Communication
The North and South magnetic poles wander widely, but sufficiently slowly for ordinary compasses to remain useful for navigation. However, at irregular intervals averaging several hundred thousand years, the Earth's field reverses and the North and South Magnetic Poles relatively abruptly switch places. These reversals of the geomagnetic poles leave a record in rocks that are of value to paleomagnetists in calculating geomagnetic fields in the past. Such information in turn is helpful in studying the motions of continents and ocean floors in the process of plate tectonics.
And how did Earth get its magnetic field? Magnetic fields surround electric currents, so we surmise that circulating electic currents in the Earth's molten metalic core are the origin of the magnetic field.
The Earth's magnetic field is attributed to a dynamo effect of circulating electric current, but it is not constant in direction. Rock specimens of different age in similar locations have different directions of permanent magnetization. Evidence for 171 magnetic field reversals during the past 71 million years has been reported. Although the details of the dynamo effect are not known in detail, the rotation of the Earth plays a part in generating the currents which are presumed to be the source of the magnetic field. It was found that Venus does not have such a magnetic field although its core iron content must be similar to that of the Earth. Venus's rotation period of 243 Earth days is just too slow to produce the dynamo effect. The magnetic field of Eartht depends upon the rotation of the fluid metallic iron which makes up a large portion of the interior, and the rotating conductor model leads to the term "dynamo effect" or "geodynamo", evoking the image of an electric generator.
Why does magnetic north sits off the coast of Canada, rather than at the North Pole? It is because of lopsided nature of Earth's inner core. The inner core is a ball of solid iron about 760 miles (1,220 kilometers) wide. It is surrounded by a liquid outer core (mostly iron and nickel), a rocky, viscous mantle layer and a thin, solid crust. As the inner core cools, crystallizing iron releases impurities, sending lighter molten material into the liquid outer core. This upwelling, combined with the Earth's rotation, drives convection, forcing the molten metal into whirling vortices. These vortices stretch and twist magnetic field lines, creating EarthÕs magnetic field. Currently, the center of the field, called an axis, emerges in the Arctic Ocean west of Ellesmere Island, about 300 miles (500 kilometers) from the geographic North Pole.
Convection (form of heat transfer - convective heat transfer involves the combined processes of conduction -heat diffusion- and advection - heat transfer by bulk fluid flow) drives the outer-core fluid and it circulates relative to the earth. This means the electrically conducting material moves relative to the Earth's magnetic field. If it can obtain a charge by some interaction like friction between layers, an effective current loop could be produced. The magnetic field of a current loop could sustain the magnetic dipole type magnetic field of the Earth. Large-scale computer models are approaching a realistic simulation of such a geodynamo.
Interaction of the terrestrial magnetic field with particles from the solar wind sets up the conditions for the aurora phenomena near the poles.
Although generally Earth's field is approximately dipolar and its magnetic moment is nearly aligned with the rotational axis, occasionally the North and South geomagnetic poles trade places. Evidence for these geomagnetic reversals can be found worldwide in basalts, sediment cores taken from the ocean floors, and seafloor magnetic anomalies. Reversals occur at apparently random intervals ranging from less than 0.1 million years to as much as 50 million years.
The Earth's magnetosphere has weakened by 15 per cent over the last 200 years.
Scientists found that changes in the Earth's magnetic field are more relevant for climatic changes in the upper atmosphere (about 100-500 km above the surface). Understanding the cause of long-term change in this area helps scientists to predict what will happen in the future (1). The increase in atmospheric CO2 concentration has been thought to be the main cause of climatic changes at these high altitudes. But magnetic field changes that have taken place over the past century are as important.
Both increasing levels of CO2 and changes in the Earth's magnetic field affect the upper atmosphere, including its charged portion, also known as the ionosphere. While CO2 causes heat to be trapped in the lower atmosphere, it actually cools the upper atmosphere. The simulations show that the increase in CO2 concentration over the past 100 years has caused the upper atmosphere, at around 300 km altitude, to cool by around 8 degrees. At the same altitude, changes in the Earth's magnetic field caused a similar amount of cooling over parts of North America, but caused a warming over other parts of the world, with the strongest warming, of up to 12 degrees, located over Antarctica.
Earth’s magnetic field is vital for keeping our atmosphere in place. Mars lost its atmosphere because it lost its magnetic field. It was found that while the pressure of the solar wind increased at each planet by similar amounts, the increase in the rate of loss of martian oxygen was ten times that of Earth’s increase. Such a difference would have a dramatic impact over billions of years, leading to large losses of the martian atmosphere, perhaps explaining or at least contributing to its current tenuous state. This proves the efficacy of Earth’s magnetic field in deflecting the solar wind and protecting our atmosphere. Without our magnetic field all the water on our planet would have evaporated and life wouldn't have survived and thrived in the way it is doing now! So no magnetic field means no atmosphere, no oxygen, no water and no life!
This has another significance too : Earth's magnetic field serves to deflect most of the solar wind, whose charged particles would otherwise strip away the ozone layer that protects the Earth from harmful ultraviolet radiation. It protects us from solar winds and excess radiation as it could be potentially dangerous to humans and animals alike.
Animals including birds and turtles can detect the Earth's magnetic field, and use the field to navigate during migration. Disablement of the magnetosphere would interrupt whale navigation and bird flight. Possibly the most closely studied of the variable Sun's biological effects has been the degradation of homing pegions' navigational abilities during geomagnetic storms. Pigeons and other migratory animals, such as dolphins and whales, demonstrate magneto-sensitive behavioral responses that were once thought to be mediated by neurons that contained the mineral magnetite located in the beak. The basis of sensory perception of magnetic fields had been unknown for a long time. However, in 2015 Chinese scientists reported they found a protein complex that may form the basis of magneto-reception in animals.
Many communication systems use the ionosphere to reflect radio signals over long distances. Ionospheric storms can affect radio communication at all latitudes. Some frequencies are absorbed and others are reflected, leading to rapidly fluctuating signals and unexpected propagation paths. TV and commercial radio stations are little affected by solar activity, but ground-to-air, ship-to-shore, shortwave broadcast and amateur radio (mostly the bands below 30 MHz) are frequently disrupted. Radio operators using HF bands rely upon solar and geomagnetic alerts to keep their communication circuits up and running.
Some military detection or early warning systems are too affected by unusual solar activity.
Damage to communications satellites can disrupt non-terrestrial telephone, television, radio and Internet links.
Earth's magnetic field is used by geologists to determine subterranean rock structures. For the most part, these geodetic surveyors are searching for oil, gas or mineral deposits. They can accomplish this only when Earth's field is quiet, so that true magnetic signatures can be detected. Other geophysicists prefer to work during geomagnetic storms, when strong variations in the Earth's normal subsurface electric currents allow them to sense subsurface oil or mineral structures. This technique is called magnetotellurics. For these reasons, many surveyors use geomagnetic alerts and predictions to schedule their mapping activities.
The Earth's magnetic field has so much importance. For any planet in any star system, a magnetic field must be present for life to originate and its sustenance. Therefore, it is taken as an important parameter to search for life on other planets.
Glad our Earth has one. Wish to see more planets like ours.
Earth has two magnetic poles- North and South, and the magnetic field between these two poles protects us from harmful cosmic rays and high speed solar winds.
A recent study reveals that the arrangement of magnetic fields was not always the same. Ancient earth had multiple poles that suddenly appeared across the globe causing planet's magnetic field behave erratically.
Researchers from Carnegie Institution of Science pointed out that between 500 million to 1 billion years ago something strange happened to the Earth's magnetosphere. They believed that inner core of the Earth was not always solid and at some point of the planet's history it began transforming from a molten state into a solid one. The gradual solidification process wrecked havoc on the magnetic field. This period of turmoil lasted until the inner core was completely solidified.
Researchers claim that these findings, published in Geographical research letters, could offer an explanation for the bizarre fluctuations in magnetic field direction seen in the geologic record around 600 to 700 million years ago.
Our solar system is exceptional because of one thing, Saturn. In the vast majority of solar systems the inner rocky planets are pushed into the parent star by the Jupiter equivalents. The “Hot Jupiters” as they are called then eventually merge with the parent star as well leaving the ice giants similar to Neptune and Uranus as what we first started calling “Super Earths” behind. Saturn stopped this process from happening by creating a tug on Jupiter preventing it from its suicidal march into the sun.
We are exceptional because we have long lived rocky planets. That is a very rare thing in the Universe.
How did the chemical makeup of our planet's core shape its geologic history and habitability?
Life as we know it could not exist without Earth's magnetic field and its ability to deflect dangerous ionizing particles from the solar wind and more far-flung cosmic rays. It is continuously generated by the motion of liquid iron in Earth's outer core, a phenomenon called the geodynamo.
Despite its fundamental importance, many questions remain unanswered about the geodynamo's origin and the energy sources that have sustained it over the millennia.
New work from an international team of researchers examines how the presence of lighter elements in the predominately iron core could affect the geodynamo's genesis and sustainability. Their findings are published by Nature Communications.
Our planet accreted from the disk of dust and gas that surrounded our Sun in its youth. Eventually, the densest material sank inward in the forming planet, creating the layers that exist today—core, mantle, and crust. Although, the core is predominately iron, seismic data indicates that some lighter elements like oxygen, silicon, sulfur, carbon, and hydrogen, were dissolved into it during the differentiation process.
Over time, the inner core crystallized and has been continuously cooling since then.
The less thermally conductive the core material is, the lower the threshold needed to generate the geodynamo," Goncharov explained. "With a low enough threshold, the heat flux out of the core could be driven entirely by the thermal convection, with no need for the additional movement of material to make it work."
The team found that a concentration of about 8 weight percent silicon in their simulated inner core, the geodynamo could have functioned on heat transmission alone for the planet's entire history.
Wen-Pin Hsieh et al, Low thermal conductivity of iron-silicon alloys at Earth's core conditions with implications for the geodynamo, Nature Communications (2020). DOI: 10.1038/s41467-020-17106-7