The correspondence in the diurnal cycle between the key observational platforms described in this study is demonstrated in a supplemental figure file JAS-Ds1 in the supplementary material. While this boundary layer moistening is not yet understood, it has been observed in previous field campaigns Sui et al. All fields have been smoothed using a min running mean. Johnson, : Sampling errors in rawinsonde-array budgets. Composite date ranges are a 7—13 Oct and b 13—16 Nov end dates are inclusive. Journal of the Atmospheric Sciences October , Vol.
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