The Cortisol Diurnal Slope quantifies the expected rate of decline in circulating cortisol levels from the morning peak (often around 8 AM) to the evening trough, typically measured over a 24-hour period or a defined subset. A healthy slope reflects robust HPA axis function, signaling appropriate timing for metabolic and stress responses. Flattening or inversion of this slope is a critical clinical indicator of adrenal dysregulation or chronic stress impact.
Origin
This term originates from chronobiology and endocrinology, specifically relating to the rhythmic, time-dependent secretion patterns inherent to many hormones, including glucocorticoids. Diurnal refers to the daily cycle, while slope describes the calculated rate of change over that time course. It is a vital metric in assessing adrenal health beyond a single snapshot measurement.
Mechanism
The mechanism relies on the pulsatile release of ACTH from the pituitary, which drives the adrenal cortex to secrete cortisol according to a circadian rhythm dictated by the suprachiasmatic nucleus. A steep, negative slope indicates successful negative feedback loops and timely clearance of the hormone post-stimulation. Deviation suggests impairment in the hypothalamic-pituitary-adrenal axis feedback sensitivity or rhythmicity.
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