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What Is This Indicator, and Why Is It Important?
This indicator would report the percentage of lake and reservoir
area with low-, medium-, and high-clarity water (ponds are
not included because of their shallow depth). A map would
show regional patterns of change.
The simplest method for measuring clarity is to lower a standard
painted disk (a Secchi disk) until it cannot be
seen; the clearer the lake or reservoir, the greater the Secchi
depth (SD). Using this method, ranges for SD would be:
low clarity (SD less than 3 feet), medium clarity (SD 310
feet), and high clarity (SD greater than 10 feet).
Water clarity is important both to people and to ecological
functioningpeople like clearer water to swim in, to
drink, and for esthetic reasons, and aquatic plants need light
to grow and fish and other animals need light to feed and
reproduce. Lakes and reservoirs can become cloudy when streams
and runoff carry silt, clay, and organic materials into them.
Runoff may also add phosphorus and other nutrients to lake
or reservoir water; these nutrients fuel algae growth (see
Phosphorus in Lakes, Reservoirs, and
Large Rivers), which also reduces water clarity.
Why Can't This Indicator Be Reported at This Time?
Although considerable amounts of water clarity data are available
from various sources, some areas are heavily sampled, while
in other areas few or no lakes are tested. Thus, the available
data do not provide representative coverage at a national
level.
It is important to track water clarity through time, because
lakes and reservoirs in different regions have different degrees
of natural clarity. By tracking clarity over time, it will
be possible to identify areas with declining or improving
clarity and to distinguish these from naturally cloudy or
clear areas.
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