A rapid change in temperature with depth is known as a A. thermocline
B. halocline
C. temperocline
D. pycnocline

A thermocline (also known as the thermal layer or the metalimnion in lakes) is a thin but distinct layer in a large body of fluid (e.g. water, as in an ocean or lake; or air, e.g. an atmosphere) in which temperature changes more rapidly with depth than it does in the layers above or below.

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