The temperature gradient is the gradient of the temperature field. It points in the direction of fastest temperature increase.
Spatial variation of the ion temperature. The inverse logarithmic scale in the title is positive for an outward-decreasing profile. A nonzero value is a possible free energy source; it does not by itself establish ion-temperature-gradient instability without the appropriate dynamics and threshold.
Articles by others on the same topic
The temperature gradient is a measure of how temperature changes with distance in a specific direction. It is essentially the rate at which temperature increases or decreases over a certain distance. The concept is important in various fields, including meteorology, geology, and engineering, as it can affect processes such as heat transfer, weather patterns, and geological phenomena.