María Jesús Campos
learningfromgeography.wikispaces.com
Climate
It is the usual state of the atmosphere in a
place over a long period of time. The sum up
of weather in a place during more than 30
years give rise to climate.
 It is studied by Climatology.





The combination of
meteorological
phenomena.
Meteorological
phenomena
(temperature,
atmospheric pressure,
wind, air masses,
precipitation) give rise to
weather. The average
pattern of that
combination on a place
during more than 30
years determines
Climate.
Atmospheric
Pressure and
Wind

Precipitation

Temperature

Air Masses

Weather

Average weather during more
than 30 years

CLIMATE
The earth’s has got different types of climate distributed
according to latitude and altitude:






Warm zone: located between the Tropic of Cancer
and the Tropic of Capricorn. All of its climates have
an average annual temperature above 18ºC.
Temperate zones: there are 2 temperate zones
located between the Tropics and the Polar Circles. Its
climates have an average annual temperature around
15ºC and different seasons.
Cold zones: there are 2 cold zones located within
the polar circles and in mountains higher than 2,500
metres. The temperatures are very cold, usually
below 0ºC.








Within those climate zones
we can find at least 12
different types of climate.
Each of them is grouped in a
category according to the
characteristics that they
share and the area in which
they are found.
Climate changes over time
but very slowly.
The Earth has experienced
many different climates over
its 4.54 billion years.
Tropical or
Hot
Climates

Temperate
or Moderate
Climates

Cold
Climates

Equatorial
Climate

Humid
Subtropical
Climate

Polar Climate

Arid or Hot
Dessert

Humid Tropical
Climate

Mediterranean
Climate

Tundra Climate

Semiarid

Dry Tropical
Climate

Maritime/Oceanic
Climate

Alpine Climate

Continental
Climate
Location
• Along the
Equator, usually
within 25º of
the Equator

Temperature Precipitation
• These areas
receive constant
direct sunlight
so temperatures
are high and
stay the same
throughout
most of the
year.
•The mean
annual
temperature is
over 25ºC

• Abundant and
regular rainfall
throughout the
year. The
regular warm
temperatures
evaporate water
and keep
humidity high
allowing it to
rain almost
every day.
• Precipitation is
over 1500 mm
annually.

Seasons
• Only 1 season
because these
area always
receive direct
sunlight
throughout the
entire year.
Location
• Near the
Equator, on the
outer edges of
Equatorial
climate.

Temperature Precipitation
• Temperatures
are high
throughout the
year.

• Abundant
rainfall but
under 1500 mm
annually.

•The mean
annual
temperature is
over 20ºC

• Precipitation
only falls during
the summer
monts, usually
from May to
August with
June and July
having the
heaviest rain.
•

Seasons
• 2 seasons, wet
(summer) and
dry (winter).
Usually the dry
season is
longer.
Location
• Near the
Equator, on the
outer edges of
Equatorial
climate.

Temperature Precipitation
• Temperatures
are high
throughout the
year. But they
are mild in
winter and hot
in summer.
•The mean
annual
temperature is
over 18ºC

• Precipitation is
scarce, although
more than 250
mm annually.

Seasons
• 2 seasons, wet
(summer) and
dry (winter).
Usually the dry
season is
longer.
Location

Temperature

Precipitation

Seasons

• On the east
coast of
continents
between 20º
and 40º north
and south of the
Equator

• Hot humid
summers and
mild winters as
these areas
receive direct
sunlight for a
large part of the
years.

• The rain falls
throughout the
year, but more
in summer. This
is because the
regularly high
temperatures
evaporate water
causing
humidity and
precipitation.

• 2 seasons,
summer and
winter. However
winter is not a
cold winter.

•The mean
annual
temperature
varies between
10ºC and 20ºC

• Precipitation is
over 1000 mm
annually.

• Summer
season lasts
longer.
Location

Temperature

Precipitation

Seasons

• Between 30º
and 45º
latitudes (N-S).
On the western
sides of
continents. It
gets its name
from the climate
found around
the
Mediterranean
Sea.

• Warm to hot,
dry summers
and mild to cool,
wet winters.

• Precipitation is
irregular. Most
precipitation
falls in spring
and autumn.
Summers have
little or no
precipitation.

• Mild climate. It
has 4 seasons
but only 2 of
them are really
clear: summer
and winter.

•The mean
annual
temperature
varies between
12º to 18º.
Temperatures
during the
summer can
reach 30º.

• Precipitation is
irregular and
varies between
300mm to 800
mm anually.

• Summers are
longer than
winters, and
winters are
usually mild.
Location
• Along the west
coast of mid-latitude
continents. Midway
between the tropics
and the
Artic/Antartic circles.
•It is stopped by the
presence of
mountains so this
climate covers more
land in Europe than
in North America
where mountains
block the humid air
from moving farther
inland.

Temperatur Precipitation
e
• Mild climate
with few
extremes in
temperature.
•The ocean’s
influence
keeps the air
over the land
cool in
summer and
warm in
winter.

•Temperatures
vary between
10º to 20º.

• Precipitation
is regular and
abundant.
• Precipitation
between 1000
and 1500 mm
annually.

Seasons
•
Temperatures
do not vary
much during
the year so
we only
distinguish 2
seasons
clearly:
summer and
winter.
Location
• In the interior
of continents
between 30º
and 60º latitude
(N-S), but
usually above
the 40º line.
•Mainly in the
Northen
Hemisphere
since there are
no major
landmasses in
the Southern
Hemisphere.

Temperature

Precipitation

• A wide range of • Marked
temperatures
contrast
because of
between warm,
latitude (less
rainy summers
direct sunlight
and dry cold
and warmth).
winters.
•Temperatures
are high in
summer(20ºC)
and low in
winter (less than
5ºC)

• Precipitation is
between 300
and 1000 mm
annually.
•Almost all the
regions of this
climate
experience
snow.

Seasons
• 4 seasons:
warm and humid
summer; cool
and dry autumn;
cold and harsh
winter; and
warm and wet
spring.
Location
• Located
near the
poles.
•It covers a
20% of the
Earth.
•It is the
most
extreme
climate of
the Earth.

Temperature

Precipitation

Seasons

• It is the coldest
climate on Earth
because of its
latitude.
•It receives
indirect sunligh
during part of
the year while in
“winter” the area
is in total
darkness.
•Temperatures
are never higher
than 5ºC, and
may fall to
-50ºC.

• Scarce
precipitation ,
less than 300
mm because its
too cold to
evaporate the
water, so the
humidity in the
air is too low to
create
precipitation.

• There is not
traditional summer
but we can
distinguish 2
seasons determined
by the amount of
light.
•“Summer”:nearly
24 hours of light
(the pole is pointed
towards the sun)
•“Winter”: nearly
24hrs of total
darkness (the pole is
facing away from the
sun)

•Precipitation
falls as snow.
Location
• Between
60-75º
latitude,
along the
coast of the
Artic Ocean.

Temperature

Precipitation

Seasons

•Because of the high
latitude, indirect
sunlight delivers light
but little heat.
•Winters are very
harsh while summers
are cool.
•Although snow melts
in summer, the deeper
parts of the soil stay
frozen, is a layer
called permafrost.

• Low levels of
precipitation as
temperatures
are too low to
cause
evaporation.
•It can be
considered a
“desert”

•Winters are
very harsh and
summers are
cool.
Location
•In high
mountain
areas.
•In sinle
mountains
such as
Mount
Kilimanjaro
and also in
large areas
such as the
Plateau of
Tibet.

Temperature
•This climate changes
as you move up to the
mountain.
Temperature depends
on the elevation.

Precipitation

Seasons

• Precipitation
•No seasons
depends also on
elevation.
• Sometimes
the base of the
mountain may
•As you move up it will be dry while
get colder and snow
there is snow in
may appear.
the top of the
•Temperature drops
mountain. This
about 6,5º degrees
happens
every 1000 m in
because high
elevation as you move mountains force
up a mountain.
warm air to
rise, so
precipitation
falls at the top.
Location

Temperature

• Arid means
dry. Most
deserts are
found along
the 30º
latitude or in
the center of
the
continents or
in the rain
shadow of
large
mountain
ranges.

•The temperatures will
depend on the latitude
of the desert. The
farther from the
Equator the colder
they will be.
•There are warm and
cold arid climates.
•Warm deserts have
an average annual
temperature above
18ºC with significant
oscillations between
day and night that can
exceed 20ºC or more.

Precipitation

Seasons

• Precipitation is •They don’t
infrequent and
have regular
irregular.
seasons.
•Less than 150
mm per year.
Location

Temperature

Precipitation

Seasons

•On the edge
of Arid
climate
areas.

•The temperatures will
depend on the latitude
of the area.

• Precipitation is
infrequent and
irregular. But
they receive
more
precipitation
than arid areas.
•Precipitation
may occur in
«winter».

•They don’t
have regular
seasons. Some
difference
between
summer and
winter.
Developed by María Jesús Campos
Chusteacher
Wikiteacher

Thanks to «Climate Types for Kids»

Climate

  • 1.
  • 2.
    Climate It is theusual state of the atmosphere in a place over a long period of time. The sum up of weather in a place during more than 30 years give rise to climate.  It is studied by Climatology. 
  • 4.
      The combination of meteorological phenomena. Meteorological phenomena (temperature, atmosphericpressure, wind, air masses, precipitation) give rise to weather. The average pattern of that combination on a place during more than 30 years determines Climate.
  • 5.
  • 6.
    The earth’s hasgot different types of climate distributed according to latitude and altitude:    Warm zone: located between the Tropic of Cancer and the Tropic of Capricorn. All of its climates have an average annual temperature above 18ºC. Temperate zones: there are 2 temperate zones located between the Tropics and the Polar Circles. Its climates have an average annual temperature around 15ºC and different seasons. Cold zones: there are 2 cold zones located within the polar circles and in mountains higher than 2,500 metres. The temperatures are very cold, usually below 0ºC.
  • 9.
        Within those climatezones we can find at least 12 different types of climate. Each of them is grouped in a category according to the characteristics that they share and the area in which they are found. Climate changes over time but very slowly. The Earth has experienced many different climates over its 4.54 billion years.
  • 10.
    Tropical or Hot Climates Temperate or Moderate Climates Cold Climates Equatorial Climate Humid Subtropical Climate PolarClimate Arid or Hot Dessert Humid Tropical Climate Mediterranean Climate Tundra Climate Semiarid Dry Tropical Climate Maritime/Oceanic Climate Alpine Climate Continental Climate
  • 11.
    Location • Along the Equator,usually within 25º of the Equator Temperature Precipitation • These areas receive constant direct sunlight so temperatures are high and stay the same throughout most of the year. •The mean annual temperature is over 25ºC • Abundant and regular rainfall throughout the year. The regular warm temperatures evaporate water and keep humidity high allowing it to rain almost every day. • Precipitation is over 1500 mm annually. Seasons • Only 1 season because these area always receive direct sunlight throughout the entire year.
  • 13.
    Location • Near the Equator,on the outer edges of Equatorial climate. Temperature Precipitation • Temperatures are high throughout the year. • Abundant rainfall but under 1500 mm annually. •The mean annual temperature is over 20ºC • Precipitation only falls during the summer monts, usually from May to August with June and July having the heaviest rain. • Seasons • 2 seasons, wet (summer) and dry (winter). Usually the dry season is longer.
  • 15.
    Location • Near the Equator,on the outer edges of Equatorial climate. Temperature Precipitation • Temperatures are high throughout the year. But they are mild in winter and hot in summer. •The mean annual temperature is over 18ºC • Precipitation is scarce, although more than 250 mm annually. Seasons • 2 seasons, wet (summer) and dry (winter). Usually the dry season is longer.
  • 17.
    Location Temperature Precipitation Seasons • On theeast coast of continents between 20º and 40º north and south of the Equator • Hot humid summers and mild winters as these areas receive direct sunlight for a large part of the years. • The rain falls throughout the year, but more in summer. This is because the regularly high temperatures evaporate water causing humidity and precipitation. • 2 seasons, summer and winter. However winter is not a cold winter. •The mean annual temperature varies between 10ºC and 20ºC • Precipitation is over 1000 mm annually. • Summer season lasts longer.
  • 19.
    Location Temperature Precipitation Seasons • Between 30º and45º latitudes (N-S). On the western sides of continents. It gets its name from the climate found around the Mediterranean Sea. • Warm to hot, dry summers and mild to cool, wet winters. • Precipitation is irregular. Most precipitation falls in spring and autumn. Summers have little or no precipitation. • Mild climate. It has 4 seasons but only 2 of them are really clear: summer and winter. •The mean annual temperature varies between 12º to 18º. Temperatures during the summer can reach 30º. • Precipitation is irregular and varies between 300mm to 800 mm anually. • Summers are longer than winters, and winters are usually mild.
  • 21.
    Location • Along thewest coast of mid-latitude continents. Midway between the tropics and the Artic/Antartic circles. •It is stopped by the presence of mountains so this climate covers more land in Europe than in North America where mountains block the humid air from moving farther inland. Temperatur Precipitation e • Mild climate with few extremes in temperature. •The ocean’s influence keeps the air over the land cool in summer and warm in winter. •Temperatures vary between 10º to 20º. • Precipitation is regular and abundant. • Precipitation between 1000 and 1500 mm annually. Seasons • Temperatures do not vary much during the year so we only distinguish 2 seasons clearly: summer and winter.
  • 23.
    Location • In theinterior of continents between 30º and 60º latitude (N-S), but usually above the 40º line. •Mainly in the Northen Hemisphere since there are no major landmasses in the Southern Hemisphere. Temperature Precipitation • A wide range of • Marked temperatures contrast because of between warm, latitude (less rainy summers direct sunlight and dry cold and warmth). winters. •Temperatures are high in summer(20ºC) and low in winter (less than 5ºC) • Precipitation is between 300 and 1000 mm annually. •Almost all the regions of this climate experience snow. Seasons • 4 seasons: warm and humid summer; cool and dry autumn; cold and harsh winter; and warm and wet spring.
  • 25.
    Location • Located near the poles. •Itcovers a 20% of the Earth. •It is the most extreme climate of the Earth. Temperature Precipitation Seasons • It is the coldest climate on Earth because of its latitude. •It receives indirect sunligh during part of the year while in “winter” the area is in total darkness. •Temperatures are never higher than 5ºC, and may fall to -50ºC. • Scarce precipitation , less than 300 mm because its too cold to evaporate the water, so the humidity in the air is too low to create precipitation. • There is not traditional summer but we can distinguish 2 seasons determined by the amount of light. •“Summer”:nearly 24 hours of light (the pole is pointed towards the sun) •“Winter”: nearly 24hrs of total darkness (the pole is facing away from the sun) •Precipitation falls as snow.
  • 27.
    Location • Between 60-75º latitude, along the coastof the Artic Ocean. Temperature Precipitation Seasons •Because of the high latitude, indirect sunlight delivers light but little heat. •Winters are very harsh while summers are cool. •Although snow melts in summer, the deeper parts of the soil stay frozen, is a layer called permafrost. • Low levels of precipitation as temperatures are too low to cause evaporation. •It can be considered a “desert” •Winters are very harsh and summers are cool.
  • 29.
    Location •In high mountain areas. •In sinle mountains suchas Mount Kilimanjaro and also in large areas such as the Plateau of Tibet. Temperature •This climate changes as you move up to the mountain. Temperature depends on the elevation. Precipitation Seasons • Precipitation •No seasons depends also on elevation. • Sometimes the base of the mountain may •As you move up it will be dry while get colder and snow there is snow in may appear. the top of the •Temperature drops mountain. This about 6,5º degrees happens every 1000 m in because high elevation as you move mountains force up a mountain. warm air to rise, so precipitation falls at the top.
  • 31.
    Location Temperature • Arid means dry.Most deserts are found along the 30º latitude or in the center of the continents or in the rain shadow of large mountain ranges. •The temperatures will depend on the latitude of the desert. The farther from the Equator the colder they will be. •There are warm and cold arid climates. •Warm deserts have an average annual temperature above 18ºC with significant oscillations between day and night that can exceed 20ºC or more. Precipitation Seasons • Precipitation is •They don’t infrequent and have regular irregular. seasons. •Less than 150 mm per year.
  • 33.
    Location Temperature Precipitation Seasons •On the edge ofArid climate areas. •The temperatures will depend on the latitude of the area. • Precipitation is infrequent and irregular. But they receive more precipitation than arid areas. •Precipitation may occur in «winter». •They don’t have regular seasons. Some difference between summer and winter.
  • 36.
    Developed by MaríaJesús Campos Chusteacher Wikiteacher Thanks to «Climate Types for Kids»