Jb. Snider, Long-term observations of cloud liquid, water vapor, and cloud-base temperature in the North Atlantic Ocean, J ATMOSP OC, 17(7), 2000, pp. 928-939
Measurements of precipitable water vapor, cloud liquid, and cloud-base temp
erature made at Porto Santo Island, Madeira Archipelago, are presented. The
observations were made continuously over a 1-yr period from July 1992 to J
une 1993. Instrumentation consisted of a 20- and 31-GHz ground-based microw
ave radiometer for measurement of water vapor and cloud liquid, and a 10.7-
mu m infrared radiometer for measurement of cloud-base temperature, A stati
stical summary of the data is presented for clear and cloudy conditions, co
nsidered both separately and combined. The mean and variance of precipitabl
e water vapor are smaller during clear than during cloudy periods. Values o
f water vapor during the winter are 26% smaller than during summer months.
The mean decorrelation time of precipitable water vapor is generally found
to be less than 12 h.