Difficulty: Easy
Correct Answer: temperature gradient
Explanation:
Introduction / Context:
Understanding how temperature varies in space is fundamental to thermodynamics, meteorology, oceanography, and even engineering heat transfer. The technical term that captures the “rate of change of temperature with distance” is widely used to explain phenomena such as lapse rates in the atmosphere, fronts, and heat flow in solids.
Given Data / Assumptions:
Concept / Approach:
In mathematics and physics, a “gradient” expresses how a quantity changes per unit distance. Therefore, the rate at which temperature changes in space is termed the temperature gradient. This can be vertical (common in meteorology) or horizontal (important for analyzing fronts). The concept generalizes to 3D vector form, indicating both magnitude and direction of greatest increase of temperature.
Step-by-Step Solution:
Verification / Alternative check:
In heat conduction, Fourier’s law uses the temperature gradient to compute heat flux: q = -k * grad(T). In meteorology, vertical temperature gradient underpins stability analysis and lapse rates, confirming the terminology’s correctness.
Why Other Options Are Wrong:
Common Pitfalls:
Confusing “difference” (a scalar change) with “gradient” (change per unit distance, often a vector). Also, isotherms depict patterns but do not express the rate of change directly.
Final Answer:
temperature gradient
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