1. ATMOSPHERE
The atmosphere is the layer of gases that surrounds the Earth
and makes life possible on the planet. It extends for thousands
of kilometres. Its composition is mainly nitrogen and oxygen,
but also argon, carbon dioxide and other gases (hydrogen,
ozone, methane and water vapour).
The atmosphere is divided into layers. These layers include the
troposphere, stratosphere, mesosphere, thermosphere and
exosphere. The temperature, thickness and composition of
each layer is different.

2. LAYERS OF THE ATMOSPHERE
https://es.tiching.com/link/15864?v=1
Animation

3. Weather describes the condition of the atmosphere. It might be sunny, hot,
windy or cloudy, raining or snowing.
Climate means the average weather conditions in a particular location
based on the average weather experienced there over 30 years or more.
The weather takes into account the temperature, precipitation, atmospheric
pressure and wind of the part of atmosphere (air) closest to the surface of the
earth.

4. TEMPERATURE
• It is the amount of heat in the atmosphere
• We measure it with the thermometer.
• It is expressed in degrees centigrade.
THERMOMETER
Fuente: Banco de imágenes del
CNICE

6. Factors affecting temperature are:
Latitude or distance from the equator
Latitude is the main factor affecting global
climate - the further you go from the equator,
the cooler it gets. This is because the earth in
curved which means that the sun's energy is
more concentrated at the equator. This, and
the thinner atmosphere at the equator, means
that the earth gets hotter here.
Altitude or height above sea level
Temperatures decrease by 0,6 degrees
celsius for every 100 metres increase in
altitude. Mountainous areas are therefore
cooler.

7. Distance from the sea
Oceans heat up and cool down much more slowly
than land. This means that coastal locations tend
to be cooler in summer and warmer in winter than
places inland at the same latitude and altitude.
Glasgow, for example, is at a similar latitude to
Moscow, but is much milder in winter because it is
nearer to the coast than Moscow.
Prevailing winds and ocean currents
The prevailing wind is the most frequent
wind direction a location experiences.
Winds take on the characteristics of their
source region.
Ocean currents can be warm or cold, and
they affect the temperature of coastal
areas.

8. Air Masses
http://www.metoffice.gov.uk/education/secondary/students/airmasses.html

10. DISTRIBUTION IN THE EARTH

11. RAINFALL
• It is water from the atmosphere that
falls into the Earth s surface in the
form of rain, snow, sleet or hail.
• We use a rain gauge or pluviometer
to measure the precipitation
• The amount of precipitation is
expressed in mm.
pluviometer

12. The atmosphere contains water vapour. The amount
of water vapour in the air is called the humidity. Low
humidity means that the air is dry and high humidity
means that the air is moist.
When humid air rises, it cools and it produces
condensation, forming small droplets of water, which
form clouds. For precipitation to occur, the droplets
must become bigger and heavier. When this happens,
thet fall (precipitation) onto the Earth s surface.

13. We get rain because of rising air.
Cloud (liquid water)
Condensation level
Water vapour
Altitude at which temperatures reach
dew point and therefore air starts to
condensate
Warm, moist air rises and it cools. As cool air can't hold as
much water vapour as warm air, the water vapour condenses
and turns into water droplets.
http://www.curriculumbits.com/prodimages/details/geography/types-of-rainfall.html

14. The amount of precipitation varies from one zone to another,
depending on factors as latitude, altitude, and proximity to
the sea.

16. Relief Rainfall
With relief rainfall, it is the presence of hills or mountains that leads to the warm aid
rising.
The winds pick up moisture from the sea as they pass over it, and this makes the air
moist. As the air rises to pass over the higher land, it cools and the water vapour
condenses, forming clouds. The droplets then fall as rain, sleet, hail, or snow,
depending on the atmospheric conditions.
On the leeward side of the mountain (the side not facing the wind), it is much drier. This
area is said to be in the 'rainshadow'. There is little rain here as the air is descending
and warming up.
http://www.youtube.com/watch?v=BVykQf
RC_aI&feature=player_embedded

18. Convectional Rainfall
This is very common in areas where ground is heated by the hot sun, such as the
Tropics.
The sun heats up the ground, which heats the air above it. This then rises and cools,
and the water vapour condenses into water droplets, forming clouds. The droplets
falls as rain under the influence of gravity.
http://www.youtube.com/watch?v=RkgThul2El8&feature=player_embedded

20. Frontal Rainfall
Frontal rainfall is associated with depressions. It happens when two air masses (a warm
one and a cold one) meet. The warm air is pushed upwards over the cold air, and, as it
rises, it cools down. The water vapour condenses to form clouds, which give rain.
http://www.youtube.com/watch?v=D88dYNFyBq8&feature=
player_embedded

22. AIR PRESSURE
•Air pressure is the force exerted by air particles. The air around us
pushes on us and every other thing (but our bodies and objects push
back with equal force so we don't notice it).
•We measure pressure with a barometer
•Pressure is expressed in milibars (mbar). Normal pressure at sea level
is 1013 mbar.

23. A low pressure system,
or "low," is an area where
the atmospheric pressure
is lower than that of the
area surrounding it.
Cold front
represented
with blue
triangles
(cold sector)
Warm front
represented
with red
semicricles
(waarm sector)
A high pressure system, or
"high," is an area where the
atmospheric pressure is greater
than that of the surrounding
area.

24. L
Lows are usually associated with high
winds, warm air, and air rising. Because
of this, lows normally produce clouds,
precipitation, and other bad weather
such as tropical storms and cyclones.
H
They are associated with dry, bright
and settled weather.
http://www.juicygeography.co.uk/downloads/flash/lowpressure.swf
http://www.juicygeography.co.uk/downloads/flash/highpressure.swf

26. Areas of equal pressure are connected using isobars. They
never cross.

27. Isobars also show us the direction of the air.
Lows: inspiraling, upspiraling,counterclockwise in north, clockwise in south; stormy
weather
Highs: outspiraling, downspiraling,
clockwise in north, counter-clockwise in
south; fair weather

29. Air moves from a high pressure area toward a low pressure area.
L
H
H

31. Closely-spaced isobars =
strong winds
Widely spaced isobars =
light winds

32. Pressure-Gradient Force

33. How depressions form?
•Depression is a low-pressure system.
•A depression forms when cold polar air meets warm tropical air at a front. The
less dense warm air starts to rise over the colder air, and this starts to lower the air
pressure.
The boundary between the two masses is called a front. There are 2 fronts in a
typical depression:
1. the warm front - this passes first, and has the warm air behind it (i.e. it is
the front of the warm air). It is where the advancing warm air is forced to rise
over the cold air
2. the cold front - this follows, and has the cold air behind it (i.e. it is the front
of the cold air). This is where the advancing cold air undercuts the warm air in
front of it. http://www.phschool.com/atschool/phsciexp/active_art/weather_fronts/

34. •Describe the weather through a depression

36. On a weather map, the warm front is shown as red semi-circles and the cold
front as blue triangles.

37. How anticyclones form?
•Anticyclones are areas of high pressure caused by air sinking towards the ground.
• Once anticyclones develop, they tend to remain for several days, bringing dry,
bright and settled weather.
This image shows an anticyclone over Spain on 31st January 1999.

38. Summer Anticyclones
Summer anticyclones bring hot and sunny
weather due to clear skies (because of the
descending air). The days are long and the
sun high in the sky, which gives plenty of
opportunity for the land to be heated up.
These conditions could therefore lead to
convectional rainfall occurring.
Winter
Winter Anticyclones
Winter anticyclones bring clear days too. However
the sun is low in the sky and the days are short,
meaning you get cool days. Clear skies on a
winter’s night will allow frost to form. The land
quickly loses heat during the night, as there is no
cloud cover to act as insulation. The rapidly cooling
ground cools and condenses any moisture in the air
above it, forming droplets of ice when the
temperature falls below freezing. This is frost.
Fogs are also caused by clear winter nights. The
ground loses heat. This cools the air above it
causing moisture to condensate around dust
particles in the layer of air closest to the ground
surface. This is fog.
Summer
Pressure
High
High
Temperature
Very cold
Very warm
Clouds/Rainfall
No
No
Wind
Calm
Calm
Other weather
conditions
Frost/fog
Heat waves/drought

39. •Two different views of a depression NW of UK with an anticyclone
to the SE

41. https://www.youtube.com/watch?v=bd7DcVnrSL8
OCCLUDED FRONT
L
L
L
C
L
C
W
W
COLD FRONTS
C
WARM FRONTS
W
H
ISOBAR
L
L

43. rain
rain
Heavy
rain
rain
Heavy
rain
Heavy
rain
rain

44. WIND
• It is the movement of air from areas of
high pressure to areas of low pressure.
• We measure wind with the wind gauge
(anemometer) in metres per second m/s
or km/hour. A weather vane shows the
direction of the wind.
a) Anemometre
b)- Weather vane

45. Most common types of winds
Prevailing winds always blow in the
same direction. For exmple, trade winds
always blow from the tropics toward the
equator.
PREVAILING WINDS
East winds
Westerlies
Trade winds
http://cienciasnaturales.es/CIRCULACIONATMOSFERICA.swf

46. PERIODIC WINDS, such as the monsoons in south and south-east Asia.
Monsoons change direction seasonally. In
summer, they blow from the Indian Ocean towards
the continent and bring abundant rain. In winter,
monsoons blow from the continent towards the sea
and bring dry stable weather.

47. SYNOPTIC WINDS, change daily, such as sea breezes
WARM
BREEZE
COOLER
Sea breezes blow from the sea
towards the land by day. At
noght, they blow from the land
towards the sea.
COOLER
BREEZE
WARM

48. How do weather and climate affect peoples' lives?
Weather and climate can have a major
effect on people's lives, for example:
Farming –
there is a direct link between the type of agriculture
and climate. For example, inland Spain has a drier
climate than coastal, with more contrasted
temperatures between winter and summer.
Northern Spain has a much wetter climate. Arable
crops tend to be rain-fed in centered areas, and
pastoral farming dominates in the north. Irrigated
crops grow in the east.
Sources of energy –
particularly windy areas have plenty of potential for
wind farms.
Water supply – for example, most of the UK s
population live in the south and east, which is
relatively dry. Water has to be transferred from
reservoirs in the wetter west.
Housing –
in particularly hot climates, buildings may be painted
white to reflect the heat. Houses in cold climates are
often built on stilts to insulate them from the freezing
ground.
Sport and leisure opportunities –
The Jamaican bobsled team of the film Cool
Runnings weren't too successful!
Why might this be?
http://www.youtube.com/watch?v=aaov7DNICPg&fe
ature=player_embedded
Snow and Ice - in areas where snow and ice are
rare, even a small snowfall can lead to chaos on the
roads. Schools may even be closed for the day!

49. How do weather and climate affect peoples' lives?
Tourism
Holidays in the Mediterranean
The graph shows the percentage of outbound
visitors to visit the top 10 destinations in 2003.
This graph shows the average temperatures in the UK and
Costa Blanca, and the average number of hours of sunshine.
To what extent do you think UK travel agents are justified in
using the slogan 'Come to Benidorm for your winter
break!'.
How does the Mediterranean climate differ from the UK
climate?

52. Where do we find temperatures?
Where do we find rainfall?
Unit of
measurement is
Celsius
Rainfall is
represented with
blue columns and
can be read in
this axis
Temperatures
are represented
with the red line
and can be read
in this axis
dryness
Example to read the
rainfall in August.
Precipitation in August is 5 mm. We
can say the climate in this place is
very dry.
Example to read the
temperatures in August.
Temperature in August is 27ºC. This month
is the hottests month of the year.
When the line of temperature is above the columns of rainfall, it
marks a period of dryness, as it is shown in this graph.

53. Climate Graphs
Climate graphs are a combination of a bar graph and a line graph. Temperature is shown on a line graph,
with the figures being shown on the right side of the graph. Rainfall is shown by a bar graph, with the figures
being shown down the left side of the graph.
The climate graph below shows average annual rainfall and temperature throughout the year for a particular
area.
Interpreting climate graphs
http://www4.uwsp.edu/geO/faculty/ritter/interactive_climat
e_map/climate_map.html
Temperature data
Is the temperature the same all year round? If it is different, how
many seasons does the location experience?
Which season is the warmest? Is it warm (10 to 20 C), hot (20 to
30 C) or very hot (above 30 C)?
Which season is the coolest? Is it mild (0 to 10 C), cold (-10 to 0 C)
or very cold (below -10 C)?
What is the range of temperature? (Subtract the minimum
temperature from the maximum temperature).
Rainfall data
Does the rainfall occur all year round?
What is the pattern of the rainfall? Check which season(s) is/are drier
or wetter than others.
What is the total annual rainfall? Add each month's total together to
get the annual total.
Then put the rainfall and temperature information together - what
does it tell you about this area?
Describe the patterns in temperature and rainfall, including how they relate
to each other. You now have a description of the climate.

54. TYPE
OF
CLIMATE
TEMPERATURES
PRECIPITATIONS
VEGETATION
Temperatures are high
throughout the year
(around 26 C in January
and 24 C in July)
Low temperature range
from 3 to 5 ºC
Abundant throughout
the year, + 1.500 mm
annually. There is no
dry season.
Rainforest. Dense forest
of evergreen trees
Average temperatures +
18ºC
Low temperature range
from 5 to 10 ºC
There are two seasons
humid/dry
(750-1.500 mm
annually)
Savannah. Very tall grass
in the rainy season,
which dries up in the dry
season.
Steppes (short thinly
scattered grass) in the
areas where the dry
season lasts longer.
Temperature range + 10
ºC
Temperatures very high
(+25ºC)
Precipitation is very
rare. (less than 250
mm annually)
Short, widely spaced
grass, thorny shrubs,
cactus. In the oases there
are palm trees.
EQUATORIAL
TROPICAL
DESSERT

55. TYPE OF
CLIMATE
TEMPERATURES
PRECIPITATIONS
VEGETATION
MARITIME
Moderate throughout the
year, mild in winter, cool in
summer.
Temparature range 10ºC
Abundant thoughout
the year.
(+
1.000
mm
annually)
Deciduous
forest
(beeches, oaks, lime
trees, etc) that lose their
leaves in autumn and
winter. Moors in nonforested
areas
and
grasslands.
CONTINENT
AL
Very
contrasting Between 300-1000
temperatures (cold winters, mm annually, mainly
and hot summers )
in summer
Temperature range + 20ºC
Coniferous forest (taiga)
with trees like pines and
firs,
grasslands
and
steppes.
MEDITERRA
NEAN
Temperatures are mild in Summers are very
winter and hot in summer. dry.
Precipitation
more abundant in
spring and fall
(300-1.000 mm)
Maditerranean
forest
(holm oaks and cork
oaks) and scrubland. Also
pines.

56. TYPE OF
CLIMATE
TEMPERATURES
PRECIPITATION
S
VEGETATION
POLAR
Very cold thorughout the Precipitation is very Tundra, moss, lichen and
year
rare (less than 250 dwarf shrubs
(not exceeding 0ºC)
mm a year)
ALPINE
Temperature falls with Precipitation
altitude. Winters cold, increases
summers cool
altitude
(+
1000
annually)
Varies with altitude
with
mm

57. HOT CLIMATES

58. TEMPERATE CLIMATES

59. COLD CLIMATES
• POLAR
• ALPINE

60. Low-latitude Landscapes:
RAINFOREST
SAVANNAH
DESERT
Mid-latitude Landscapes :
DEIDUOUSFOREST
MEDITERRANEAN
STEPPE
High-latitude Landscapes :
TAIGA
TUNDRA
ALPINE