Abstract
Abstract High-resolution observations of the Q branch of the 2 ν 2 band of phosphine at 1972 cm −1 on Jupiter show an enhancement of the PH 3 concentration in the deep troposphere ( p ⩾1 bar) by about 60% at high Northern (∼50°N) latitudes compared to both the North Equatorial Belt and the Great Red Spot. Difference in photochemistry or in deep vertical diffusion of PH 3 could be involved to interpret such variations.
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