During the period June 9 through June 18, 1992, an intensive radiosounding program was conducted to measure atmospheric profiles of the wind velocity, the temperature and the specific humidity. The launch site was located near site MS000 in the northeastern part of the catchment of the Little Washita River; this location was selected in order to ensure that the measured profiles would reflect the catchment's surface features for the prevailing southwesterly winds during this time of the year. The launch times of the rawinsondes are shown

Brutsaert, W.

English

NASA Technical Reports Server

NASA-CR-194383
The National Aeronautics and Space Administration
Final Technical Report
Project Title: Atmospheric Soundings During the Washita-92 Campaign
Project Number: NAG5 - 1989
Period: From June 1, 1992 through September 30, 1992
Institution: Cornell University, Ithaca, New York
Principal Investigator: W. Brutsaert
Civil and Environmental Engineering
Cornell University
Ithaca, NY 14853-3501
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/25 °°
(NASA-CR-194383) ATMOSPHERIC
SOUNDINGS DURING THE WASHITA 1992
CAMPAIGN Final Technical Report,
Jun. - 30 Sep. 1992 (Cornell
Univ.) 10 p
G3/46
N94-13212
Unclas
0185600
A,,571F
https://ntrs.nasa.gov/search.jsp?R=19940008739 2020-06-16T21:56:33+00:00Z
Summary of Work
f -
__/During the period June 9 through June 18, 1992, an intensive radiosounding program was
conducted to measure atmospheric profiles of the wind velocity, the temperature and the
specific humidity. The launch site was located near site MS000 in the northeastern part of the
catchment of the Little Washita River; this location was selected in order to ensure that the
measured profiles would reflect the catchment's surface features for the prevailing
southwesterly winds during this time of the year. The launch times of the rawinsondes are
shown in Table L_
The measurements were carried out by a team from Cornell University consisting of
Wilfried Brutsaert and Nelson Dias.
The radiosounding equipment used was manufactured by Atmospheric Instrumentation
Research (AIR), Boulder, Colorado. The ground station was compact enough that it could be
placed inside a 9 x 12 ft tent. The radiosonde system (AIR-3A, spin type) consisted of
disposable sondes with dry- and wet-bulb temperature and pressure sensors, of a receiving unit
on the ground, and of an optical theodolite to Irack the sonde. During flight the sonde, attached
to a balloon, measures the data in cycles of approximately 4.8s in the following sequence: dry-
bulb temperature is measured at time zero; 0.6 and 1.8s later, wet-bulb temperature and
pressure are measured, respectively; then after approximately 3.0s the dry-bulb temperature
measurement is made again to begin the next cycle. According to the manufacturer, the
response of the pressure sensor is practically instantaneous, but the dry- and wet-bulb sensors
have time constants of 3 and 12s, respectively. Because of these time constants, it is necessary
to further process the data if they are to be used for analysis in the boundary layer. One
possible procedure for this purpose was outlined by Sugita and Brutsaert (Journal of
Geophysical Research, 95(D6), 7617-7624, 1990). The height, y, of the sonde can be
obtained from the pressure, temperature and humidity. The horizontal distance between the
sonde and the release point can be calculated from the elevation angle measured by the
theodolite and from y. This, in turn, with the measured azimuth angle yields the horizontal
position of the sonde. Finally, successive horizontal positions allow the calculation of average
wind velocity and direction over the interval; these average values are then to be assigned to the
midpoint of the interval. For 5s cycles, and with typical balloon ascent rates of around 3 to 4
m/s, the vertical resolution of the measurements was around 15 to 20 m. The sounding was
generally aborted above 600 hPa (i.e., 600 mb). In Table 2, an example is shown of the data
that were obtained from the rawinsonde ascents. These are level-zero, i.e., uncorrected
measurements and processed in a preliminary fashion with the manufacturer's software.
Following timeof day(CDST)anddate,the raw or primary data shown are pressure (mb), dry
bulb temperature (°C), wet bulb temperature, azimuth angle (degrees), elevation angle; the
other data (nameIy height, mixing ratio, potential temperature, wind speed, wind direction,
height of wind speed, and relative humidity) were calculated from the primary data. The
profile data measured during this campaign are now available and ready for distribution.
Table1
ActualLaunchTimesof theSoundings(CDST)
Day Date
161 92/06/09 1150 1540 1800
162 92/06/10 0931 1102 1307 1530 1800
163 92/06/11 0929 1059 1302 1531 1800
164 92/06/12 0932 1059 1308 1529 1800
165 92/06/13 0934 1102 1302 1530 1800
166 92/06/14 0927 1059 1302 1531 1757
167 92/06/15 0931 1056 1301 1530 1800
168 92/06/16 0932 1100 1303 1530 1805
169 92/06/17 0931 1102 1300 1530 1801
170 92/06/18 0931 1100 1302 1532 1800
Table 2
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or Poor QUaL rv


Atmospheric soundings during the Washita 1992 campaign

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