The Scoop on Sensor Selection
Tips on how to pick sensors that accurately measure wind speed, vertical temperature differences, and solar radiation
- By David I. Katz
- Oct 01, 2006
Meteorological monitoring for air quality studies has evolved over the past
four decades. During the summer of 1956 an experimental program to study micrometeorology
and dispersion from near-surface releases was conducted near the town of O'Neil
in north-central Nebraska. This comprehensive turbulence and diffusion program
of 70 tracer experiments was given the name Project Prairie Grass and was instrumental
in providing a basis for development of practical methods for the characterization
of atmospheric dispersion. One of the first papers to discuss these data was
by Cramer, in which a Gaussian plume model was described that related the horizontal
and vertical dispersion to the observed standard deviations of lateral and elevation
angles of the wind fluctuations. Barad and Haugen used the Project Prairie Grass
results to specifically investigate the veracity of Sutton's model for plume
dispersion. Not long after, Dr. F. Pasquill offered a pragmatic technique for
the estimation of Gaussian plume vertical and lateral dispersion that could
be implemented with easily acquired meteorological observations, namely insolation
and wind speed, as shown in Table 1.
Table 1
Key to Pasquill Stablility Categories |
Daytime Insolation |
Nighttime Insolation |
Surface Wind Speed (m/s) |
Strong |
Moderate |
Slight |
Thinly Overcast or ¡Ã ¨ö low cloud |
¡Â 3/8 |
<2 |
A |
A-B |
B |
- |
- |
2-3 |
A-B |
B |
C |
E |
F |
3-5 |
B |
B-C |
C |
D |
E |
5-6 |
C |
C-D |
D |
D |
D |
>6 |
C |
D |
D |
D |
D |
Strong insolation corresponds to sunny, midday, midsummer
conditions in England; slight insolation corresponds to similar conditions
in midwinter. Night refers to the period from one hour before sunset to
one hour after sunrise. The neutral category, D, should be used regardless
of wind speed, for overcast conditions during day or night. |
Dr. Pasquill was corresponding with F.A. Gifford, Jr. (who was then with the
Oak Ridge Field Research Division), R. McCormick, and D.Bruce Turner (who were
then with the Cincinnati Field Research Division) prior to 1961. So it was that
Gifford offered a conversion of Pasquill's angular spread values to standard
deviations of plume spread, and Turner offered a conversion of Pasquill's stability
classification criteria that employed hourly airport observations. These extensions
to Pasquill's scheme simplified its use and made it practical for it to be converted
to a numerical algorithm. The plume-spread coefficients of ¥òz in the vertical
dimension and ¥òy in the horizontal, which he displayed as curves for each stability
category on log-log plots of dispersion parameters as a function of downwind
distance from the source. These dispersion parameters came to be known as Pasquill-Gifford
(P-G) parameters.
As the Clean Air Act regulations have evolved over the years, it became more
important to make meteorological and air-quality observations at locations away
from the traditional airport observation sites. These monitoring sites became
more and more automated with the advent of computer technology. Without human
observers to report on the cloud cover, proxies for the data used by Pasquill
and Gifford were necessary. This has resulted in the use, at various times,
of vertical temperature difference (delta-T), standard deviation of wind direction¥ò¥è,
and various adjustments to these, especially based on the wind speed and the
time of processing the data.
The Development of SRDT
In an effort to avoid the need for onsite cloud cover observations as called
for by Turner's method, the U.S. Environmental Protection Agency (EPA) developed
a technique that uses onsite measurements of solar radiation or vertical temperature
difference between 10 and two meters on a 10-meter tower as a function of wind
speed to determine the local P-G stability class. This technique, identified
by the abbreviation SRDT, was first used in the EPA guideline, "Meteorological
Monitoring Guidance for Regulatory Modeling Applications," United States
Environmental Protection Agency, Office of Air Quality Planning and Standards,
Research Triangle Park, NC 27711, February 2000, EPA-454/R-99-005.
Table 2 is the reproduction of the table from the guideline
showing how these measurements are used to determine the P-G stability class.
Table 2
Key to Solar Radiation Delta-T (SRDT) Method for Estimating Pasquill-Gifford
(P-G) Stability Categories
Daytime: Solar Radiation (W/m2)
|
Wind Speed (m/s) |
¡Ã925 |
925-675 |
675-175 |
<175 |
<2 |
A |
A |
B |
D |
2-3 |
A |
B |
C |
D |
3-5 |
B |
B |
C |
D |
5-6 |
C |
C |
D |
D |
¡Ã6 |
C |
D |
D |
D |
Nighttime Vertical Temperature
Gradient |
Wind Speed (m/s) |
<0 |
¡Ã0 |
<2 |
E |
F |
2.0-2.5 |
D |
E |
¡Ã2.5 |
D |
D |
The upper half of Table 2 is the equivalent to left half the
daytime insolation portion of Table 1, and the bottom half
of Table 2 is the equivalent of the right side (nighttime cloud
cover) of Table 1. Using SRDT measurements avoids having to
have a local observation of the cloud cover or a laser ceilometer, which is
available at airports to measure the cloud height, but is not customarily used
at air quality monitoring systems.
Overview of Sensor Types
Selecting the sensors needed to accurately make the SRDT measurements is described
in the EPA guideline. Wind-speed sensor selection has been well defined for
many years since wind speed has determined the pollutant diffusion and has been
a primary measurement since these stations and guidelines were first developed.
Traditional cup anemometers can easily meet the performance requirements of
the guideline for accuracy and response. In the past 10 years, sonic anemometers
have been developed that are designed for ambient wind sensing and as a direct
replacement for conventional mechanical anemometers, both in terms of performance
and cost. An added benefit is that they require no periodic maintenance or calibration.
The solid-state sonic anemometers will tend to report more very-low wind speeds
since they have no moving parts and the associated inertia to overcome at low
wind speeds. Otherwise, they will tend to report very similar wind speeds over
the range of the sensors.
A critical measurement in the SRDT scheme is the temperatures at the two levels
on the 10-meter tower. Officially stated as the vertical temperature difference
between two and 10 meters, the vertical temperature difference is more practically
between two and nine meters, since the wind sensors are at 10 meters and need
to be unobstructed by other equipment on the tower.
It is quite apparent that the motor-aspirated shield for the temperature sensor
is at least one meter below the height of the anemometer cup set and wind-direction
vane, or about nine meters above ground level. So, in selecting temperature
sensors, it is critical that they be both accurate and precise. This is achieved
by testing the temperature sensors either at the factory or before placing them
in the field to be certain that if they vary from a known value, the variation
is of the same sign. Then if the sensors vary within the tolerance allowed by
the guideline, the user will know that they will report an accurate temperature
difference. This is key since the guideline requires an accuracy of +/- 0.10
degrees Celsius for the delta-T measurement. This is achievable through normal
monitoring methods only if the two sensors are matched to assure a precise measurement.
The last measurement needed to use the SRDT method is solar radiation, which
is measured with a pyranometer. The guideline requires that the pyranometer
respond to radiation in the wavelength range of 285 to 2,800 nanometers. This
wavelength range extends into the near-infrared, which contains approximately
25 percent of the total incoming solar radiation. This is the sensitivity range
of most thermopile pyranometers. The thermopile consists of a series of thermojunction
pairs, an optically black primary junction, and an optically white reference
junction (in some pyranometers, the reference thermojunction is embedded in
the body of the instrument). The temperature difference between the primary
and reference junctions that results when the pyranometer is operating generates
an electrical potential proportional to the solar radiation.
Other pyranometers, which use photovoltaic-sensing elements, should not be
used when SRDT will be used to calculate the local P-G stability class, since
the spectral response of the photovoltaic pyranometer is limited to the visible
spectrum. This can result in the stability class being off by one or two classes
and would drastically affect the results of a dispersion modeling analysis.
When care is taken in the selection of sensors used to make the measurements
needed to use the SRDT method of determining the P-G stability class, the gathered
data will be of great value to the user. It will also be relatively easy to
meet the 90 percent valid data requirement as set forth in the guideline when
starting with top quality equipment.
Acknowledgment: Thanks to John Irwin for his input.
This article originally appeared in the 10/01/2006 issue of Environmental Protection.
About the Author
David I. Katz is the vice president of government sales and corporate meteorologist with Climatronics Corp. His background as a meteorologist with experience in conducting and managing monitoring programs for regulatory compliance offers him a unique perspective for the customers' requirements. Prior to joining Climatronics, Katz worked as an air quality meteorologist for Burns & McDonnell Engineering Co., Kansas City, Mo. He holds a BS in Earth/Planetary Sciences and an MS in Atmospheric Science. He can be contacted at (631) 567-6300.