Unit 5

UNIT 5.
ATMOSPHERE:
WEATHER AND
CLIMATE
1. The Earth´s Atmosphere.
2. The properties of air.
3. Atmospheric dynamics: weather and climate.
4. The Earth´s climates

1. THE EARTH´S
ATMOSPHERE Remember: the Earth´s atmosphere is a gaseous layer that surrounds
the planet, provides oxygen and protects us from solar radiation.
The atmosphere is divided into
different layers:
1. Troposphere
2. Stratosphere
3. Mesosphere
4. Thermosphere (Ionosphere)
5. Exosphere.
Most meteorological
phenomena, such as cloud
formation, wind and rain occur
in Troposphere.

The layers of the atmosphere
1. Troposphere (0-12 Km)
 The main meteorological phenomena happen here.
 It is the closest layer to Earth's surface.
 It is the layer we live in.
 higher altitude=colder temps (temperatures drop by 65 ºC for every 100 m of altitude).
2. Stratosphere (12-50 km).
 Ozone layer is here. It absorbs ultraviolet radiation from the sun.
 Higher altitude=warmer temps.
3. Mesosphere (50-100 km)
 Where meteors and comets are destroyed
 higher altitude=colder temps (temperatures sometimes reach -100 ºC).
4. Thermosphere (Ionosphere) (85-600 km)
 Solar radiation produces electrically-charged.
 Borealis auroras are here.
 Higher altitude=warmer temps (reach up to 1500 ºC).
5. Exosphere (600-10.000 km).
 The outermost layer, where satellites orbit Earth.

2. THE PROPERTIES OF AIR
Composition of gases. Air is a mixture of gases: 78% nitrogen,
21% oxygen and various other components such as water vapour.
Temperature. The properties of air are affected by heat from the
Earth’s surface. When air is heated it expands, becomes lighter and
rises. Air temperature becomes colder as it gets further from the
Earth’s surface. When it is cooler, the air begins to fall back towards
the surface.
Atmospheric pressure. Is the term used to describe the pressure
exerted on Earth by the weight of the air. It is measured with a
barometer.
Both altitude and temperature determine atmospheric pressure.
Relatively humidity. It refers to the amount of water vapour that air
contains. Warmer air can hold more water vapour.

 The most important properties of air

3. ATMOSPHERIC DYNAMICS
3.1. WEATHER AND CLIMATE
 The Sun´s rays warm up the atmosphere and our planet´s surface.
The energy from the Sun is responsible for the Earth´s weather and
climate.
 You have to distinguish these two concepts:
 Weather is the state of the lower layers of the atmosphere at a
certain time and place on Earth.
 The science that deals with predicting what the weather will be like in a
certain zone is called Meteorology.
 Climate refers to the state of the weather in a certain region of the
planet over a long period of time. It is necessary to analyze a
region in 30 years intervals to establish the climate of a region.
 The science that studies different types of climate is referred to
as Climatology.

3.2.FACTORS THAT INFLUENCE
WEATHER
 Weather can be determined by many factors:
A. ATMOSPHERIC PRESSURE.
B. TEMPERATURE.
C. WIND.
D. HUMIDITY AND PRECIPITATION
 https://study.com/academy/lesson/temperature-clouds-wind-humidity-on-
the-atmospheric-cycle.html
 https://www.youtube.com/watch?v=E7DLLxrrBV8

A. ATMOSPHERIC
PRESSURE
 Atmospheric pressure is the weight of air over a particular Earth´s
surface. It is measured in millibars (mb) or hectopascals (hPa) by a
barometer. It varies from one place to another and depends on:
 Altitude: atmospheric pressure is lower at higher altitudes. For
example, the amount of air at the top of a mountain is less than at
the base.
 Temperature: warm air weighs less than cold air. As a result, warm
air rises and exerts less pressure on the Earth´s surface while cold
air descends and exerts more pressure.
 The measurement of atmospheric pressure can be represented on a
map, where the points of equal atmospheric pressure are joined through
a few lines: isobars. When isobars are close together, in this area is very
windy.

Weather maps
 You can see A (Anticiclón. In English language H: high pressure
area) and B (Borrasca. In English language L: low pressure area
or depressions). In Spain there is an area of high pressure (more
than 1013 hPa), so the weather is stable. However, in Northern
Europe there is an area of low pressure (less than 1013 pHa), so
the weather is unstable.
Anticyclones (H): are areas of high pressure (more than 1013 hPa). They form when a mass of cold air descends and the pressure
increases. They produce stable weather.
Depressions (L): are areas of low pressure (less than 1013 hPa). They form when a mass of warm air rises and the pressure decreases.
They produce unstable weather.

B. TEMPERATURE
 It is measured in degrees on the Fahrenheit (ºF) or Celsius
(ºC) scales.
 Temperature varies according to:
 Altitude: temperatures decreases with elevation
 Latitude: the farther away from the Equator the colder it gets.
 Distance from the sea: temperature of the land near large
bodies of water is often milder, with no big variations in
temperature.

C. WIND
 Masses of air move around in the atmosphere. This movement
causes wind. There are different types of wind:
 Prevailing winds, such as trade winds, always blow in the same
direction and in the same regions.
 Periodic winds, such as monsoons, vary depending on the season.
 Local winds are found in small areas. They usually blow in the
same direction. For example, Tramontana (Islas Baleares), Galerna
(Mar Cantábrico) and Cierzo (Aragón).

D. HUMIDITY AND
PRECIPITATION
 All air masses contain a certain amount of water vapour or
atmospheric humidity.
 As a mass of warm air rises, its temperature decreases. The
humidity it contains is transformed into a liquid state and falls to
the Earth’s surface in the form of precipitation.
 There are three main causes of precipitation (page 87):
 Frontal rainfall:
 Storms:
 Relief rainfall:

INTERACTIVE EXERCISES
 WEATHER FORESCAST:
http://repositorio.educa.jccm.es/portal/odes/ingles/weather/cont
enido/contenido/oa05.html
 WEATHER AND CLIMATE:
 WEATHER:

4. THE EARTH´S CLIMATES
Climatologists divide the Earth into different climate zones. This
division is based on similar temperatures and precipitation across
large areas.
4.1. THE EARTH´S CLIMATES ZONES.
We can identify three major climates zones: cold, hot and temperate.

COLD ZONES
 There is very little sunshine and annual average temperatures are
below 0 ºC.
 There are two cold climate zones located within the polar circles:
 One in the Northern Hemisphere, made up of the Arctic Ocean,
Greenland and the northern coasts of Asia, Europe and America.
 One in the Southern Hemisphere, made up of the Antarctic.

HOT ZONES
 There is a single hot climate zone, which is known as the
intertropical zone. It is located between the two tropics. The
intense sunshine in this region produces annual average
temperatures of above 18 ºC.

TEMPERATE ZONES
 There are two temperate climate zones which are located between
the tropics and the polar circles. In these regions, annual average
temperatures are between 0 ºC and 18 ºC. The amount of
sunshine varies throughout the year, resulting in four seasons. In
the Northern hemisphere, the hot season coincides with the
summer months. In the Southern hemisphere, it coincides with the
winter months.

4.2. THE EARTH´S CLIMATES TYPES
 Within climates zones there are regions with different types of
climates. The combination of annual temperature and
precipitation data results in nine different climate types:
CLIMATE
TYPES
TEMPERATE
CLIMATES
Mediterranean Continental Oceanic
Humid
Subtropical
HOT CLIMATES
Equatorial Tropical Desert
COLD CLIMATES
Polar Alpine

MAP OF THE EARTH´S CLIMATES
TYPES

WHAT IS A CLIMOGRAPH?
 Temperature and precipitation make it possible to identify a
climate.
Both elements can be shown graphically using a
climograph which allows us to observe the annual change
in temperature and precipitation in a specific place on the
planet.
This information is represented using a combination chart
with two systems of coordinates.
 Activity: How to make a climopraph (page 96-97)

Unit 5

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