What Is Normal Distribution?
A normal distribution is a bell-shaped
frequency distribution curve. Most of the data values in a normal
distribution tend to cluster around the mean. The further a data
point is from the mean, the less likely it is to occur. There are
many things, such as intelligence, height, and blood pressure, that
naturally follow a normal distribution. For example, if you took
the height of one hundred 22-year-old women and created a
histogram by plotting height on the x-axis, and
the frequency at which each of the heights occurred on the y-axis,
you would get a normal distribution.
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10/21/2020, 7:39:32 PM
What Is Normal Distribution?
A normal distribution is a bell-shaped
frequency distribution curve. Most of the data values in a normal
distribution tend to cluster around the mean. The further a data
point is from the mean, the less likely it is to occur. There are
many things, such as intelligence, height, and blood pressure, that
naturally follow a normal distribution. For example, if you took
the height of one hundred 22-year-old women and created a
histogram by plotting height on the x-axis, and
the frequency at which each of the heights occurred on the y-axis,
you would get a normal distribution.
Characteristics of Normal Distribution
Here, we see the four characteristics of a normal distribution.
Normal distributions are symmetric,
unimodal, and asymptotic, and the
mean, median, and
mode are all equal.
A normal distribution is perfectly symmetrical around its
center. That is, the right side of the center is a mirror image of
the left side. There is also only one mode, or peak, in a normal
distribution. Normal distributions are continuous and have tails
that are asymptotic, which means that they approach but never touch
the x-axis. The center of a normal distribution is
located at its peak, and 50% of the data lies above the mean, while
50% lies below. It follows that the mean, median, and mode are all
equal in a normal distribution.
- U.S. and Global Temperature. Average
temperatures have risen across the contiguous 48 states since 1901,
with an increased rate of warming over the past 30 years. Eight of
the top 10 warmest years on record have occurred since 1998.
Average global temperatures show a similar trend, and all of the
top 10 warmest years on record worldwide have occurred since 1998.
Within the United States, temperatures in parts of the North, the
West, and Alaska have increased the most.
- High and Low Temperatures. Many extreme
temperature conditions are becoming more common. Since the 1970s,
unusually hot summer days (highs) have become more common over the
last few decades in the United States. Unusually hot summer nights
(lows) have become more common at an even faster rate. This trend
indicates less “cooling off” at night. Although the United States
has experienced many winters with unusually low temperatures,
unusually cold winter temperatures have become less
common—particularly very cold nights (lows). Record-setting daily
high temperatures have become more common than record lows. The
decade from 2000 to 2009 had twice as many record highs as record
lows.
- U.S. and Global Precipitation. Total annual
precipitation has increased over land areas in the United States
and worldwide. Since 1901, precipitation has increased at an
average rate of 0.08 inches per decade over land areas worldwide.
However, shifting weather patterns have caused certain areas, such
as the Southwest, to experience less precipitation than usual.
- Heavy Precipitation. In recent years, a higher
percentage of precipitation in the United States has come in the
form of intense single-day events. The prevalence of extreme
single-day precipitation events remained fairly steady between 1910
and the 1980s but has risen substantially since then. Nationwide,
nine of the top 10 years for extreme one-day precipitation events
have occurred since 1990. The occurrence of abnormally high annual
precipitation totals (as defined by the National Oceanic and
Atmospheric Administration) has also increased.
- Tropical Cyclone Activity. Tropical storm
activity in the Atlantic Ocean, the Caribbean, and the Gulf of
Mexico has increased during the past 20 years. Storm intensity is
closely related to variations in sea surface temperature in the
tropical Atlantic. However, changes in observation methods over
time make it difficult to know for sure whether a longer-term
increase in storm activity has occurred. Records collected since
the late 1800s suggest that the actual number of hurricanes per
year has not increased.
- River Flooding. Increases and decreases in the
frequency and magnitude of river flood events vary by region.
Floods have generally become larger across parts of the Northeast
and Midwest and smaller in the West, southern Appalachia, and
northern Michigan. Large floods have become more frequent across
the Northeast, Pacific Northwest, and parts of the northern Great
Plains, and less frequent in the Southwest and the Rockies.
- Drought. Average drought conditions across the
nation have varied since records began in 1895. The 1930s and 1950s
saw the most widespread droughts, while the last 50 years have
generally been wetter than average. However, specific trends vary
by region. A more detailed index developed recently shows that over
the period from 2000 through 2015, roughly 20 to 70 percent of the
U.S. land area experienced conditions that were at least abnormally
dry at any given time. However, this index has not been in use for
long enough to compare with historical drought patterns.
- A Closer Look: Temperature and Drought in the
Southwest. The southwestern United States is particularly
sensitive to changes in temperature and thus vulnerable to drought,
as even a small decrease in water availability in this already arid
region can stress natural systems and further threaten water
supplies.