Drifting

Friction helps a car drift by providing the necessary grip between the tires and the road surface. The right balance of friction allows the driver to control the car's slide and maintain control during the drift. Insufficient friction can result in a loss of control, while excessive friction can hinder the car's ability to slide smoothly.

Ballistic spin drift is the tendency of a spinning projectile (such as a bullet) to drift slightly to the side due to the gyroscopic effect created by its spin. This effect influences the trajectory of the projectile and can cause it to deviate from its intended path at longer ranges. Shooters need to account for ballistic spin drift when calculating their shots for increased accuracy.

Genetic drift is caused by random sampling errors in a population's gene pool. These errors can occur during processes like genetic recombination, migration, or founder events, leading to changes in allele frequencies over generations. The smaller the population, the greater the impact of genetic drift.

Set and drift can be found using a navigation instrument such as a compass and comparing the actual direction of travel to the intended direction of travel. Set is the direction of drift due to currents or wind, while drift is the unintended sideways movement from the intended course. By comparing the heading of the vessel or aircraft with the actual track over the ground, you can calculate the set and drift.

The North Atlantic Drift, a warm ocean current, brings mild and humid air from the Gulf Stream to Western Europe, which moderates the climate in the region. This current helps keep temperatures along the Western European coast warmer than they would be at similar latitudes, influencing weather patterns and supporting diverse ecosystems. However, changes in the North Atlantic Drift can have significant impacts on regional climate variability.

Drift motion refers to the horizontal movement of ocean water caused by wind, the Earth's rotation, and the shape of the coastline. This motion can result in the transport of surface water and any materials it carries, such as pollutants or debris.

A primary force refers to a dominant or significant factor that drives a particular process or outcome. It represents the main force responsible for initiating or influencing a particular situation.

There are lots of meaning of the word 'drift'

In the motoring world, drift means sliding a car sideways with the handbrake.

In general, conversation use, you use it in this sort of way:

"He drifted off to sleep"

It's define general use meaning is: Drift: An adjective used to describe a change of action.

(There is a pretty small selection of sentences you can use this word, you don't really need to know much, it's hardly ever used in conversation generally, anyway.) AHH!!theres a drift

Alfred Wegener used several lines of evidence to support the theory of Continental Drift, including the fit of the continents like a jigsaw puzzle, similarities in rock formations and mountain ranges across different continents, matching fossil records on different continents, and evidence of past climates that could only be explained if continents had once been connected.

Pangaea or Pangea was the super-continent in the continental drift hypothesis.

The primary force behind seafloor spreading and continental drift is convection currents in the Earth's mantle. These currents move the tectonic plates above them, causing them to either spread apart or collide. The spreading of seafloor and the shifting of continents are part of the larger process of plate tectonics.

Alfred Wegener, a German meteorologist and geophysicist, first proposed the theory of continental drift in 1912. He suggested that the continents were once part of a single supercontinent called Pangaea, which later broke apart and drifted to their current positions due to the movement of the Earth's mantle caused by thermal convection.

Alfred Wegener proposed the theory of continental drift in 1912. He collected evidence from various fields, such as the fit of continental coastlines, matching rock types and structures across continents, and similar fossil distributions. However, his theory was not widely accepted until decades later when the concept of plate tectonics provided a mechanism for how continents could move.

Magnetic drift refers to the slow and gradual change in the orientation of the Earth's magnetic field over time. It is caused by various factors, including the movement of molten iron in the outer core of the Earth. Magnetic drift is an important phenomenon that is closely monitored by scientists to better understand the behavior of the Earth's magnetic field.

The man who pioneered the continental drift hypothesis was Alfred Wegener. He proposed the theory in 1912, suggesting that Earth's continents were once joined together in a single landmass called Pangea and have since drifted apart.

Quite simply, the answer is no. While there is no doubt better equipment will make the task easier, you basically need RWD vehicle with LSD or locked diff in it. Drifting an open diff car is very hard and almost impossible.

Deep-sea mountain ranges had caught his attention.

Alfred Wegener's fully developed theory of continental drift attempted to point out evidences that the continents were once joined into a single continent he called Pangaea. Wegener's theory hypothesized that the continents were able to push through the rock of the seafloor to their present positions.

As evidence, he noted (as had others before him), of the geographic correlation in coastline perimeters of South America and Africa. This was the feature that led Wegener to investigate other clues. His investigations revealed that mountain ranges in South America and Africa, and strata and composition of coal fields in Europe and North America matched or lined up. Additionally, matching reptilian fossils were found on either side of the ocean, indicating that the continents were once joined together. Although he was unable to find a mechanism for his proposed continental drift theory, he also observed that the more shallow an ocean, the younger its geologic age. It wasn't until the 1950's and 1960's, with the discovery of the Mid-Atlantic Ridge (and other sea floor mapping discoveries) that Wegener's hypothesis started to become more accepted. The newer science of plate tectonics owes much to Wegener's scientific groundwork.

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The idea of continental drift was first proposed by Alfred Wegener in 1912. He suggested that the continents were once joined together in a single supercontinent called Pangaea and have since drifted apart.

The difference between drift current and diffusion current is that drift current depends on the electric field applied: if there's no electric field, there's no drift current. Diffusion current occurs even though there isn't an electric field applied to the semiconductor. It does not have E as one of its parameters. The constants it does depend on are Dp and Dn, and +q and -q, for holes and electrons respectively. The first constants are called the diffusion coefficients, a proportionality factor. We don't worry too much about these because they are constants. We do worry about the gradient of the concentration of p and/or n, though. But, since we are talking about a one dimensional situation when we are solving for current densities, we only worry about the gradient (or derivative) with respect to the x-plane. The other difference between drift current and diffusion current, is that the direction of the diffusion current depends on the change in the carrier concentrations, not the concentrations themselves. In the equation, the signs are reversed as we are used to seeing them. We usually assign a +q to holes and -q to electrons. In the case of diffusion current, they are reversed to be opposite of the derivative of the concentrations. This occurs because the carriers are diffusing from areas of high concentrations to areas of low concentrations. For example, if the derivative of pwith respect to x is positive, then the concentration of holes is growing as you move towards the +x direction. Diffusion current will be the opposite of that, the holes will be diffusing in the -x direction to where there's a lower concentration of holes. If the derivative is negative, the opposite will occur. The concentration of holes is decreasing as you go from the -x to +x direction. Therefore, holes will diffuse to the +x direction where there's a lower concentration of holes. This is why the negative sign is needed in the equation for the hole diffusion current. The same goes for electrons, but in this case, the signs cancel for a positive derivative because the electrons, carrying -q, diffuse to the -x direction where there's less electrons. The sign remains if the derivative is negative, because electrons will be diffusing to the +xdirection carrying a -q charge. For these reasons it's not included in the equation for the electron diffusion current. source: http://www.ece.utep.edu/courses/ee3329/ee3329/Studyguide/ToC/Fundamentals/CAction/diffusion.html The difference between drift current and diffusion current is that drift current depends on the electric field applied: if there's no electric field, there's no drift current. Diffusion current occurs even though there isn't an electric field applied to the semiconductor. It does not have E as one of its parameters. The constants it does depend on are Dp and Dn, and +q and -q, for holes and electrons respectively. The first constants are called the diffusion coefficients, a proportionality factor. We don't worry too much about these because they are constants. We do worry about the gradient of the concentration of p and/or n, though. But, since we are talking about a one dimensional situation when we are solving for current densities, we only worry about the gradient (or derivative) with respect to the x-plane. The other difference between drift current and diffusion current, is that the direction of the diffusion current depends on the change in the carrier concentrations, not the concentrations themselves. In the equation, the signs are reversed as we are used to seeing them. We usually assign a +q to holes and -q to electrons. In the case of diffusion current, they are reversed to be opposite of the derivative of the concentrations. This occurs because the carriers are diffusing from areas of high concentrations to areas of low concentrations. For example, if the derivative of pwith respect to x is positive, then the concentration of holes is growing as you move towards the +x direction. Diffusion current will be the opposite of that, the holes will be diffusing in the -x direction to where there's a lower concentration of holes. If the derivative is negative, the opposite will occur. The concentration of holes is decreasing as you go from the -x to +x direction. Therefore, holes will diffuse to the +x direction where there's a lower concentration of holes. This is why the negative sign is needed in the equation for the hole diffusion current. The same goes for electrons, but in this case, the signs cancel for a positive derivative because the electrons, carrying -q, diffuse to the -x direction where there's less electrons. The sign remains if the derivative is negative, because electrons will be diffusing to the +xdirection carrying a -q charge. For these reasons it's not included in the equation for the electron diffusion current. source: http://www.ece.utep.edu/courses/ee3329/ee3329/Studyguide/ToC/Fundamentals/CAction/diffusion.html The difference between drift current and diffusion current is that drift current depends on the electric field applied: if there's no electric field, there's no drift current. Diffusion current occurs even though there isn't an electric field applied to the semiconductor. It does not have E as one of its parameters. The constants it does depend on are Dp and Dn, and +q and -q, for holes and electrons respectively. The first constants are called the diffusion coefficients, a proportionality factor. We don't worry too much about these because they are constants. We do worry about the gradient of the concentration of p and/or n, though. But, since we are talking about a one dimensional situation when we are solving for current densities, we only worry about the gradient (or derivative) with respect to the x-plane. The other difference between drift current and diffusion current, is that the direction of the diffusion current depends on the change in the carrier concentrations, not the concentrations themselves. In the equation, the signs are reversed as we are used to seeing them. We usually assign a +q to holes and -q to electrons. In the case of diffusion current, they are reversed to be opposite of the derivative of the concentrations. This occurs because the carriers are diffusing from areas of high concentrations to areas of low concentrations. For example, if the derivative of pwith respect to x is positive, then the concentration of holes is growing as you move towards the +x direction. Diffusion current will be the opposite of that, the holes will be diffusing in the -x direction to where there's a lower concentration of holes. If the derivative is negative, the opposite will occur. The concentration of holes is decreasing as you go from the -x to +x direction. Therefore, holes will diffuse to the +x direction where there's a lower concentration of holes. This is why the negative sign is needed in the equation for the hole diffusion current. The same goes for electrons, but in this case, the signs cancel for a positive derivative because the electrons, carrying -q, diffuse to the -x direction where there's less electrons. The sign remains if the derivative is negative, because electrons will be diffusing to the +xdirection carrying a -q charge. For these reasons it's not included in the equation for the electron diffusion current. source: http://www.ece.utep.edu/courses/ee3329/ee3329/Studyguide/ToC/Fundamentals/CAction/diffusion.html

Drift velocity is the average velocity with which charged particles, such as electrons, move in a conductor in the presence of an electric field. It is a very slow velocity due to frequent collisions with atoms in the material. Drift velocity is responsible for the flow of electric current in a circuit.

The magnetic quality of feldspar is caused by the presence of trace elements such as iron, titanium, or manganese in its structure. These trace elements create magnetic moments that align with an external magnetic field, giving feldspar its magnetic properties.

Alfred Wegener is credited with developing the theory of continental drift in the early 20th century. He proposed that the Earth's continents were once all joined together in a single supercontinent called Pangaea, which later broke apart and drifted to their current positions.

Specifically, drift relates the movement of a carrier (e.g., an electron or hole) to an applied electric field (i.e., the velocity of the carrier is proportional to the electric field, where the proportionality constant, mobility, is a quantity derived in solid-state physics). Diffusion relates the movement of carriers due to random (i.e., thermal) behavior and non-uniform distribution (i.e., the velocity of the carrier is proportional to the logarithmic derivative of the density of carriers, where the proportionality constant, the diffusion constant, is a quantity derived in solid-state physics).

There are many factors that can cause a vehicle to drift when moving at highway speed.

First off is the alignment of the vehicles tires. At slow speeds this may not be noticable to the driver, but as the vehicles speed increases, the small inperfection in the tires alignment becomes magnified, causing the vehicle to pull (drift) to one side or the other. This can also be caused by the slight variations in each individual tire's pressure as well.

Second, the drift can be caused by force of and direction of the prevailing wind passing over the highway. In addition, as the vehicle increases in speed, minor inperfections in the vehicles aerodynamic shape (tailpipes, muffler, dings, dents ect) can alter the force of the wind passing both above and below the vehicle causing drift.

Weight distribution in the vehicle also plays a part in this. More weight on one side will cause the vehicle to pull in that direction.

This is just a few of the basic reasons.

A drift current is electric charges being moved in the presence of an electric field, and a diffusion current is electric charges being moved by a chemical diffusion gradient (where no electric field exists, but where there is a concentration gradient of chemical species driving the current).