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Peter Black, Lee Harrison, Mark Beaubien, Robert Bluth, Roy Woods, Andrew Penny, Robert W. Smith, and James D. Doyle

low level below consisting of high variability centered near 80%. The humidities near the surface observed by the BRO radiosonde over land are almost 100%, about 15% higher than observed by the XDD over the ocean. This again appears real, as fog was reported at BRO at the time of the radiosonde launch; there was no fog over the ocean. The moisture maxima observed by the radiosonde at 1, 3, and 5–6 km are well resolved by the XDD. Fig . 18. Temperature and RH profile observed by sonde C21 (red and

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