Xm. Shao et al., Observations of precipitable water vapor fluctuations in convective boundary layer via microwave interferometry, J GEO RES-A, 104(D14), 1999, pp. 16729-16740
At microwave frequencies, each centimeter of precipitable water vapor (PWV)
causes about 6.45 cm of extra electrical path length relative to the "dry"
air. The fluctuations of the water vapor dominate the changes of the effec
tive path length through the atmosphere in a relatively short time period o
f a few hours. In this paper we describe a microwave interferometer develop
ed for water vapor investigations and present the observation results. The
interferometer consists of 10 antennas along two orthogonal 400-m arms that
form many baselines (antenna pairs) ranging from 100 to 400 m. All the ant
ennas receive a common CW signal (11.7 GHz) from a geostationary television
satellite, and phase differences between pairs of antennas are measured. T
he phase differences reflect the column-integrated water vapor differences
from the top of the atmosphere to the spatially separated antennas at the g
round. The interferometric, baseline-differential measurements allow us to
study the statistical properties of the PWV fluctuations, as well as the tu
rbulent activity of the convective boundary layer (CBL). Structure function
analysis of the interferometer measurements shows good agreement with resu
lts obtained from the Very Large Array (VLA) and with a theoretical model d
eveloped for radio astronomical very long baseline interferometry (VLBI), r
eported previously by other investigators. The diurnally varying structure
constant correlates remarkably well with the combination of the latent and
sensible heat fluxes measured simultaneously from a 10-m meteorological tow
er. The average drift velocity of the PWV over the interferometer was also
derived from the measurements. The derived velocity agrees well during the
morning hours with the wind measured by an anemometer at the center of the
interferometer.