Forest Service Class I Wilderness Representative Visibility
The goal of this project was to determine the range of visibility
conditions at each U.S. Forest Service Class I Wilderness where
visibility monitoring has been done. Visibility is expressed as
Standard Visual Range (SVR) – the greatest distance at which
an observer can just see a black object viewed against the horizon
sky. These figures are a synthesis of Forest Service quantitative
camera monitoring and IMPROVE and IMPROVE protocol aerosol and
optical monitoring. IMPROVE (Interagency Monitoring of PROtected
Visual Environments) is a national network designed to determine
existing air quality in federal Class I areas, identify sources
of existing manmade impairment, and document long-term trends to
track progress towards goal of no manmade impairment of protected
areas.
Types of monitoring:
Quantitative Camera Monitoring: These
systems function by taking color film pictures along a sight path
from the visibility
monitoring site to a known target on the horizon. Targets are typically
dark in color, are 30 to 70 kilometers from the monitoring site,
and are at approximately the same elevation as the monitoring site.
Once the film is developed, the relative contrast between the target
and the background sky is measured using a "slide scanning
densitometer". This contrast measurement is then used to estimate
the standard visual range. Typically, 3 photographs are automatically
taken per day,
IMPROVE Aerosol Monitoring: Up to
four modules measure the composition and concentration of the fine
particles that produce
extinction and the tracers that identify emission sources. Light
extinction is calculated from the mass of these particles, then
converted to standard visual range. These monitors typically run
for two 24-hour periods per week.
Transmissometers: Comprised of a light transmitter and
a receiver, transmissometers measure total light extinction directly
along a sight path which is usually 5 to 10 kilometers long. Since
the intensity of the light source is known, any loss on the receiving
end is attributable to absorption and scattering of light by particles.
This data can then be used to calculate standard visual range.
Transmissometers typically run 10 minutes every hour, 24 hours/day.
The data is plotted on a rank-order cumulative probability graph.
From this graph, the 10th, 50th, and 90th percentile cumulative
frequency values are derived. Visibility conditons worse (lower
SVR) than the 10th percentile SVR occur on only 10% of days, or
90 % of days have better (higher SVR) visibility.Visibility conditions
worse than the 50th percentile SVR occur half the days and, likewise,
visibility conditions are better than the 50th percentile half the
days. Visibility conditions are better than the 90th percentile
on 10% of days and are worse on 90% of days.
Number Generation Criteria
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Values Used |
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Minimum Samples Required for Valid Analysis
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| Quantitative Camera Only |
2 Summers, >200 Daily SVRs |
=(1/r)ln[RnCo/Cr] |
10% SVR |
Median SVR |
80% SVR |
| IMPROVE Module A |
1 Year, >104 24 hr Samples |
=7.1*MF,west =9*MF,east |
10% SVR |
Median SVR |
90% SVR |
| IMPROVE A-D |
1 Year, >104 24 hr Samples |
=Rbext |
10% SVR |
Median SVR |
90% SVR |
| IMPROVE A-D and Transmissometer |
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ave(10% SVR) |
ave(Median SVR) |
ave(90% SVR) |
| Transmissometer |
1 Year, >365 24 hr Samples |
=(Bext-Bray+10) |
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| Nephelometer |
Data was not used |
Awaiting quality assurance checks |
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*Variable Definitions
Bext = light extinction coefficient – the loss of image-forming
light per unit distance due to scattering and absorption by particles
and gases in the atmosphere. (Mm-1)
r = path length or distance to target (Mm)
Rn = sky radiance ration (unitless)
Co = inherent contrast of the target against the background sky
(unitless)
Cr = apparent contrast o the target against the background sky
(unitless)
MF = fine mass (particles <2.5 mm) concentrations in mg/m3
Rbext = reconstructed extinction based on aerosol species measurements
(Mm-1)
Bray = Rayleigh scattering, scattering by natural gases of the
atmosphere. For calculations of SVR, Rayleigh scattering is assumed
to be 10 Mm-1
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