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Geo introduction
Weather
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Cards (161)
Weather
The atmospheric
conditions
of a given place over a
short
period of time
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Elements
of weather
Temperature
Humidity
Precipitation
Atmospheric
pressure
Sunshine
Cloud
cover
Wind
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Weather
station
A place set aside for the observing,
measuring
and
recording
of various weather elements
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Locations
of weather stations
Colleges
Schools
Agricultural institutions
Meteorological departments
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Stevenson
screen
Directs
sunlight
away
Provides
shade
conditions for
accurate
temperature readings
Allows free
air
circulation to measure
actual
air temperature
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The
Stevenson
screen is made of
wood
to prevent absorption of heat
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Factors
for siting a weather station
Open, away from trees and buildings to allow
free
flow of
air
Gentle
, fairly
level
land with wide view of the sky
Away from
paved
surfaces to avoid
splashing
water
Properly
fenced
for security
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Types
of records kept in a weather station
Daily
records
Monthly
records
Graphical
record book for annual
graphs
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Sunshine
The direct rays of the sun reaching the earth's
surface
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Factors
affecting sunshine
Cloud
cover
Aspect
(slope facing the sun)
Latitude
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Sunshine recorder
An instrument that measures the duration of
sunshine
by burning a trace on a
card
as the sun moves across the sky
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Temperature
The degree of
hotness
or
coldness
of an object or place
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Types
of thermometers
Minimum
thermometer
Maximum
thermometer
Six's
thermometer (minimum and maximum)
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Minimum
thermometer
Measures the
lowest
temperature of the day
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Maximum thermometer
Measures the
highest
temperature of the day
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Six
's thermometer
Measures both the
minimum
and
maximum
temperature of the day
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Mean
daily temperature
The average daily temperature, calculated by adding the daily maximum and minimum and dividing by
2
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Daily
diurnal range of temperature
The difference between the
daily maximum
and
minimum
temperature
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Mean
monthly temperature
The
average
temperature for the month, calculated by adding the daily
mean
temperatures and dividing by the number of days
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Mean annual temperature
The average temperature for the whole year, calculated by adding the
mean
monthly temperatures and dividing by
12
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Factors
influencing temperature
Altitude
Distance from
large water body
Aspect
Cloud
cover
Amount of
water vapour
Latitude
Winds
Human
activities
Position of the
midday
sun
Transparency
of the atmosphere
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Temperatures
are higher near the earth's surface due to terrestrial
radiation
, greenhouse gases, and the presence of air molecules and living organisms
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Air cools
as it rises due to expansion and rarefaction at
higher
altitudes
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Clear skies at
night allow
terrestrial
radiation
to escape, leading to low temperatures
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Greenhouse gases
Gases such as
chlorofluorocarbons
that trap
heat
in the atmosphere and increase temperatures
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Thick
cloud cover at night
Traps
heat
into the atmosphere below, bringing
warmer
nights
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Humidity
Amount of
water vapour
in the atmosphere
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Humid air
Absorbs
heat
during the day and retains it at
night
, increasing temperature
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Latitude
Distance from the
equator
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Increase in latitude
Decrease in temperature
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Equator
Receives high temperatures due to
shorter
distance and
90
degree angle of sun's rays
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Polar regions
Receive
low
temperatures due to
longer
distance and acute angle of sun's rays
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Tropic
of Cancer
When the sun is overhead, the
Northern
hemisphere receives
longer
daylight hours and more heat
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Inter
-tropical convergence zone (ITCZ)
Area within the tropics where temperatures are
highest
when the
midday
sun is overhead at the equator
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Cold
ocean currents
Bring a
cooling
effect on adjacent lands,
lowering
temperatures
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Warm
ocean currents
Bring a
warming
effect on adjacent lands,
increasing
temperatures
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Warm winds
Bring a
warming
effect,
increasing
temperatures
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Cold
winds
Bring a
cooling
effect,
lowering
temperatures
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Vegetation
Creates
shade
which
lowers
temperatures
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Industrial activities produce
greenhouse gases
that
increase
temperatures
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