SlideShare une entreprise Scribd logo
1  sur  31
Theme 2 - Weather and Climate
Weather
Is the conditions of the atmosphere in
the short term - over a day or a week.
It is made up of temperature, rainfall,
humidity, wind speed, wind direction,
air pressure and other characteristics of
the air around us.
Climate
Is the generalised conditions of the
precipitation and temperature over a
year. The figures are averaged out
over a long period of time - this is
normally a minimum of 30 years.
Weather is …
It includes …
It involves changes in the …
Climate is …
It includes …
It involves changes in the …
Condition High or Low Pressure
Cold and warm fronts
Sinking air
High level of
condensation
Low precipitation
Sunny conditions in
summer
Cold and frosty
conditions in winter
Condition High or Low Pressure
Warm air rising over
cold air
Thunderstorms in the
afternoon in Summer.
Very stable conditions
for a number of days
or weeks
Low levels of
condensation.
Rain, followed by few
hours of dry, followed
by heavy rain.
Storm conditions and
isobars that are close
together.
High or Low Pressure?
High
High
Low
High
High
Low
High
High
High
Low
Low
Low
Pm
Pc
TcTm
Am
The Importance of Air Masses
An air mass is a block of air that has similar temperature and moisture
characteristics. Where the ‘air comes from’ has a big impact on our weather
and climate.
The Importance of Air Masses
An air mass is a block of air that has similar temperature and moisture
characteristics. Where the ‘air comes from’ has a big impact on our weather
and climate.
Link - 1’10” in
Link 2 Link 3
Sandstorms in the Sahara Desert in Northern Africa
collect and transport lots of sand and dust into the
atmosphere. This is picked up by the wind moving
clockwise in the high pressure.
Air in a high
pressure
(anticyclone)
moves in a
clockwise
direction. This
creates an air
mass moving over
the UK from the
South.
The Tropical
Continental Air Mass
(Tc) is full of dust and
sand which have
been picked up from
the storms in the
Sahara
Air in a high
pressure sinks
creating very
stable conditions.
Wind speeds tend
to be light and
calm.
Sinking air with calm conditions
means that levels of pollution in
the atmosphere can build up. The
air mass affecting the UK crosses
some of the big industrial regions
of Europe - Northern France,
Belgium and Germany.
High Pressure
Stretch and Challenge
•High pressure systems block other
weather systems, especially low
pressures and so can last for
several days, even weeks. This
means the weather conditions can
remain similar for some time.
•Isobars in High Pressure systems
tend to be spread out; the
pressure gradient is low.
•Sinking air means the chance of
condensation is low, and thus
precipitation levels are low. This
means there is little or no rainfall
to wash pollutants and dust out of
the atmosphere.
•Microclimates in urban areas
mean that high pressure
conditions trap pollution emitted
by transport and industrial sources
in the local area. This combines
with pollutants transported from
further afield.
• Moves from East to West
• Crosses three countries -
Philippines 26-27 September,
Vietnam 29th September, and
Laos/Cambodia on 30th
September.
• Turns from a tropical depression,
into a Tropical Storm, into Typhoon
and then back into a Tropical
Storm.
• Begins in the Philippine Sea, and
moves west across the South China
Sea.
• North of the Equator but South of
the Tropic of Cancer.
• Highest number of deaths in the
Philippines.
• Whereas lowest number of deaths
in Cambodia.
• Deaths in Vietnam and Cambodia
together are less than those in the
Philippines.
• Damage is greatest in Vietnam.
• Damage is lowest in Philippines.
• Damage in the Philippines and
Cambodia together is less than
that in Vietnam.
• Homelessness is highest in
Philippines.
• In contrast Cambodia has the
lowest homelessness.
• Similarly Vietnam had a high level
of evacuation - although this isn’t
the same as homelessness.
Cause of floods:
• Impermeable surfaces - lack of
infiltration, so rapid run-off.
• Poor drainage in informal
settlements - rapid population
growth led to poor level of
infrastructure.
• High population density - lots of
people affected in a small area.
Impact on Quality life
• Economic:
• Social:
• Environmental:
People can’t get to work easily. Many
businesses shut. People will see a fall
in income which could increase poverty
when people are already ‘on the edge’.
Emergency services cannot access those
who need help - rise in diseases and ill
health. Communities are cut off - people
cannot access food and clean water.
Sanitation systems are flooded - dirty and contaminated
water in many areas. Spreads disease very easily - young
people, the sick and the old very vulnerable.
You’ve been given some case study revision notes about the
impact of low pressure weather systems. However, they need
improving - your challenge is to mark them and indicate where
improvements need to be made, and to make them.
Check for:
• Detailed information.
• Specific evidence and facts.
• Clear structure and small chunks of information.
• Complex ideas and understanding - stretch yourself and apply ‘BIG’
ideas.
For a period of weather caused by high or low pressure.
• Name and locate the area affected by the weather.
• Describe the main features of the weather.
• Explain how the weather affected different groups of people.
[8 marks]
Name:
• UK - high levels of rain and flooding in 2012.
Describe:
• Higher than average rainfall
• Caused by higher air temperatures linked to Global Warming
• Caused by change in the position of the Jet Stream - air masses created
conditions for high rainfall
• Ground became quickly saturated - flooding in many drainage basins across the
UK
• Higher populations on flood plains - more people at risk of flooding
Explain impacts on different groups:
• Homeowners
• Farmers
• Insurance Companies
• People in General
Challenge
What does warm air rise?
Your answer?
Describe
Explain
10
o
C, 8 oktas of cloud,
drizzle, Force 5 Wind from
the SSW.
Located at the warm front.
In the next few hours it will
get warmer and the drizzle
will stop.
Warm air is rising over cold
air. As the air rises it
cools, and this means
water vapour condenses to
form clouds. This causes
the rainfall, along with the
TM air that is warm and
moist which comes from
the SSW.
Describe
Explain
11
o
C, 8 oktas of cloud,
rain, Force 5 Wind from the
W.
Located at the warm front.
In the next few hours it will
briefly get warmer and then
it will rain heavily as the
cold front arrives.
Warm air is rising over cold
air. As the air rises it
cools, and this means
water vapour condenses to
form clouds. This causes
the rainfall, along with the
TM air that is warm and
moist which comes from
the W.
Describe
Explain
13
o
C, 3 oktas of cloud,
rain, Force 3 Wind from the
SW.
Located in the warm
sector. In the next few
hours it will begin to rain
heavily as the cold front
arrives and temperatures
will fall.
In between the warm and
cold fronts is a block of
warm air. This creates an
area of more stable and
calmer weather. However
as the cold front
approaches, warm air will
once again rise over cold
creating the conditions for
rainfall.
The weather at Point A is wet and
windy. Temperatures are 9oC,
and the wind is blowing from the
South West, and is Force 4.
There is quite a lots of cloud, and
there is drizzle.
This is the warm front where a
warm air mass is meeting a cold
air mass. They don’t mix because
they are different densities.
Condensation leads to
precipitation and this is why it is
raining.
The weather at Point A is wet and
windy. Temperatures are 9oC,
and the wind is blowing from the
South West, and is Force 4.
There are 7 okras of cloud cover
and it is drizzling.
This is the warm front. Warm air
is being forced over cold air
because it is less dense. As it
rises it cools, which lets water
vapour condense to form clouds.
As the clouds build up eventually
it will rain. This frontal system is a
low pressure as the different air
masses have different densities
and one rises over the other.
Answer A Answer B

Contenu connexe

Tendances

Climate: Hurricane Basic Detail
Climate: Hurricane Basic DetailClimate: Hurricane Basic Detail
Climate: Hurricane Basic Detailgeomillie
 
Cyclone Nikhil & Mazar
Cyclone Nikhil & MazarCyclone Nikhil & Mazar
Cyclone Nikhil & Mazarsubzero64
 
Severe Weather - Lightning, Tornadoes, & Hurricanes
Severe Weather -  Lightning, Tornadoes, & HurricanesSevere Weather -  Lightning, Tornadoes, & Hurricanes
Severe Weather - Lightning, Tornadoes, & HurricanesBantay's Earth Science!
 
Cyclones and anticyclones
Cyclones and anticyclonesCyclones and anticyclones
Cyclones and anticyclonesNaveenpadukone
 
3. Anticyclones
3. Anticyclones3. Anticyclones
3. Anticyclonestudorgeog
 
Cyclones - Understanding Storm Systems
Cyclones - Understanding Storm SystemsCyclones - Understanding Storm Systems
Cyclones - Understanding Storm SystemsJohn Johnston
 
Global and Local Winds
Global and Local WindsGlobal and Local Winds
Global and Local Windsrebelbrindley
 
CAMBRIDGE GEOGRAPHY A2 REVISION - TROPICAL ENVIRONMENTS: TROPICAL CLIMATES
CAMBRIDGE GEOGRAPHY A2 REVISION - TROPICAL ENVIRONMENTS: TROPICAL CLIMATESCAMBRIDGE GEOGRAPHY A2 REVISION - TROPICAL ENVIRONMENTS: TROPICAL CLIMATES
CAMBRIDGE GEOGRAPHY A2 REVISION - TROPICAL ENVIRONMENTS: TROPICAL CLIMATESGeorge Dumitrache
 
Notes - Air Masses, Fronts, Global Winds
Notes - Air Masses, Fronts, Global WindsNotes - Air Masses, Fronts, Global Winds
Notes - Air Masses, Fronts, Global WindsBantay's Oceanography
 
Natural Science: Weather and Storms
Natural Science: Weather and StormsNatural Science: Weather and Storms
Natural Science: Weather and StormsShamie Garcia
 
Weather disturbances
Weather disturbancesWeather disturbances
Weather disturbancesAaron Lopez
 
Cyclone and its types
Cyclone and its typesCyclone and its types
Cyclone and its typesMicrobiology
 
Lesson 6: Weather and Climate Topic Revision
Lesson 6: Weather and Climate Topic RevisionLesson 6: Weather and Climate Topic Revision
Lesson 6: Weather and Climate Topic RevisionTyler Tonna
 
Lesson 2: Winter and Summer Anticyclones
Lesson 2: Winter and Summer AnticyclonesLesson 2: Winter and Summer Anticyclones
Lesson 2: Winter and Summer AnticyclonesTyler Tonna
 

Tendances (20)

Fronts
FrontsFronts
Fronts
 
Climate: Hurricane Basic Detail
Climate: Hurricane Basic DetailClimate: Hurricane Basic Detail
Climate: Hurricane Basic Detail
 
Cyclone Nikhil & Mazar
Cyclone Nikhil & MazarCyclone Nikhil & Mazar
Cyclone Nikhil & Mazar
 
Severe Weather - Lightning, Tornadoes, & Hurricanes
Severe Weather -  Lightning, Tornadoes, & HurricanesSevere Weather -  Lightning, Tornadoes, & Hurricanes
Severe Weather - Lightning, Tornadoes, & Hurricanes
 
Cyclones and anticyclones
Cyclones and anticyclonesCyclones and anticyclones
Cyclones and anticyclones
 
3. Anticyclones
3. Anticyclones3. Anticyclones
3. Anticyclones
 
Cyclones - Understanding Storm Systems
Cyclones - Understanding Storm SystemsCyclones - Understanding Storm Systems
Cyclones - Understanding Storm Systems
 
Cloud Development & Classification
Cloud Development & ClassificationCloud Development & Classification
Cloud Development & Classification
 
Global and Local Winds
Global and Local WindsGlobal and Local Winds
Global and Local Winds
 
CYCLONE
CYCLONECYCLONE
CYCLONE
 
CAMBRIDGE GEOGRAPHY A2 REVISION - TROPICAL ENVIRONMENTS: TROPICAL CLIMATES
CAMBRIDGE GEOGRAPHY A2 REVISION - TROPICAL ENVIRONMENTS: TROPICAL CLIMATESCAMBRIDGE GEOGRAPHY A2 REVISION - TROPICAL ENVIRONMENTS: TROPICAL CLIMATES
CAMBRIDGE GEOGRAPHY A2 REVISION - TROPICAL ENVIRONMENTS: TROPICAL CLIMATES
 
Notes - Air Masses, Fronts, Global Winds
Notes - Air Masses, Fronts, Global WindsNotes - Air Masses, Fronts, Global Winds
Notes - Air Masses, Fronts, Global Winds
 
Cyclones
CyclonesCyclones
Cyclones
 
Natural Science: Weather and Storms
Natural Science: Weather and StormsNatural Science: Weather and Storms
Natural Science: Weather and Storms
 
Weather disturbances
Weather disturbancesWeather disturbances
Weather disturbances
 
Cyclones
CyclonesCyclones
Cyclones
 
Cyclone and its types
Cyclone and its typesCyclone and its types
Cyclone and its types
 
Lesson 6: Weather and Climate Topic Revision
Lesson 6: Weather and Climate Topic RevisionLesson 6: Weather and Climate Topic Revision
Lesson 6: Weather and Climate Topic Revision
 
Lesson 2: Winter and Summer Anticyclones
Lesson 2: Winter and Summer AnticyclonesLesson 2: Winter and Summer Anticyclones
Lesson 2: Winter and Summer Anticyclones
 
Storm Surges
Storm SurgesStorm Surges
Storm Surges
 

En vedette

Coastal Landforms Revision
Coastal Landforms RevisionCoastal Landforms Revision
Coastal Landforms Revisiondouglasgreig
 
OS Mapping and Industrial Location
OS Mapping and Industrial LocationOS Mapping and Industrial Location
OS Mapping and Industrial Locationdouglasgreig
 
Savannah Problem Solving (Unit 2 2011)
Savannah Problem Solving (Unit 2 2011)Savannah Problem Solving (Unit 2 2011)
Savannah Problem Solving (Unit 2 2011)douglasgreig
 
Patrones Hipoxicos
Patrones HipoxicosPatrones Hipoxicos
Patrones Hipoxicosjenniefer
 
Edisi5novnas
Edisi5novnasEdisi5novnas
Edisi5novnasepaper
 
12jan N As
12jan N As12jan N As
12jan N Asepaper
 
Waspada Nasional 2 September 2009
Waspada Nasional 2 September 2009Waspada Nasional 2 September 2009
Waspada Nasional 2 September 2009epaper
 
Universiteit Antwerpen Europese Handelspartners Ken Lawrence
Universiteit Antwerpen Europese Handelspartners Ken LawrenceUniversiteit Antwerpen Europese Handelspartners Ken Lawrence
Universiteit Antwerpen Europese Handelspartners Ken LawrenceThisco
 
Edisi 6 Des Nas
Edisi 6 Des NasEdisi 6 Des Nas
Edisi 6 Des Nasepaper
 
Edisi16oktnasional
Edisi16oktnasionalEdisi16oktnasional
Edisi16oktnasionalepaper
 
Edisi 15 Nov
Edisi 15 NovEdisi 15 Nov
Edisi 15 Novepaper
 
Edisi 4 Des Nas
Edisi 4 Des NasEdisi 4 Des Nas
Edisi 4 Des Nasepaper
 
Waspada Nasional3 Sep
Waspada Nasional3 SepWaspada Nasional3 Sep
Waspada Nasional3 Sepepaper
 
Edisi 12 Aceh Sep
Edisi 12 Aceh SepEdisi 12 Aceh Sep
Edisi 12 Aceh Sepepaper
 
Waspada Aceh3sep
Waspada Aceh3sepWaspada Aceh3sep
Waspada Aceh3sepepaper
 
Edisi 22 Feb Aceh
Edisi 22 Feb AcehEdisi 22 Feb Aceh
Edisi 22 Feb Acehepaper
 
Finding the right legal process management tools
Finding the right legal process management toolsFinding the right legal process management tools
Finding the right legal process management toolssarahbrown1
 
08jan Aceh
08jan Aceh08jan Aceh
08jan Acehepaper
 

En vedette (20)

Coastal Landforms Revision
Coastal Landforms RevisionCoastal Landforms Revision
Coastal Landforms Revision
 
OS Mapping and Industrial Location
OS Mapping and Industrial LocationOS Mapping and Industrial Location
OS Mapping and Industrial Location
 
Savannah Problem Solving (Unit 2 2011)
Savannah Problem Solving (Unit 2 2011)Savannah Problem Solving (Unit 2 2011)
Savannah Problem Solving (Unit 2 2011)
 
Patrones Hipoxicos
Patrones HipoxicosPatrones Hipoxicos
Patrones Hipoxicos
 
Edisi5novnas
Edisi5novnasEdisi5novnas
Edisi5novnas
 
12jan N As
12jan N As12jan N As
12jan N As
 
Waspada Nasional 2 September 2009
Waspada Nasional 2 September 2009Waspada Nasional 2 September 2009
Waspada Nasional 2 September 2009
 
Universiteit Antwerpen Europese Handelspartners Ken Lawrence
Universiteit Antwerpen Europese Handelspartners Ken LawrenceUniversiteit Antwerpen Europese Handelspartners Ken Lawrence
Universiteit Antwerpen Europese Handelspartners Ken Lawrence
 
Edisi 6 Des Nas
Edisi 6 Des NasEdisi 6 Des Nas
Edisi 6 Des Nas
 
Edisi16oktnasional
Edisi16oktnasionalEdisi16oktnasional
Edisi16oktnasional
 
Edisi 15 Nov
Edisi 15 NovEdisi 15 Nov
Edisi 15 Nov
 
Edisi 4 Des Nas
Edisi 4 Des NasEdisi 4 Des Nas
Edisi 4 Des Nas
 
World 2.0
World 2.0World 2.0
World 2.0
 
Waspada Nasional3 Sep
Waspada Nasional3 SepWaspada Nasional3 Sep
Waspada Nasional3 Sep
 
Edisi 12 Aceh Sep
Edisi 12 Aceh SepEdisi 12 Aceh Sep
Edisi 12 Aceh Sep
 
Waspada Aceh3sep
Waspada Aceh3sepWaspada Aceh3sep
Waspada Aceh3sep
 
Edisi 22 Feb Aceh
Edisi 22 Feb AcehEdisi 22 Feb Aceh
Edisi 22 Feb Aceh
 
Rm3-A Device
Rm3-A DeviceRm3-A Device
Rm3-A Device
 
Finding the right legal process management tools
Finding the right legal process management toolsFinding the right legal process management tools
Finding the right legal process management tools
 
08jan Aceh
08jan Aceh08jan Aceh
08jan Aceh
 

Similaire à Weather Systems Revision 2014

Weather elements and factors
Weather elements and factorsWeather elements and factors
Weather elements and factorsShabana Yasmin
 
Weather and climate 7C
Weather and climate 7CWeather and climate 7C
Weather and climate 7Cchives
 
Unit 3. climate and living beings.ppt
Unit 3. climate and living beings.pptUnit 3. climate and living beings.ppt
Unit 3. climate and living beings.pptalzambra
 
Weather & climate project by Matthew Ben Hamed 3.02
Weather & climate project  by Matthew Ben Hamed 3.02Weather & climate project  by Matthew Ben Hamed 3.02
Weather & climate project by Matthew Ben Hamed 3.02geographystudents
 
Geo: Chapter Three, Section One
Geo: Chapter Three, Section OneGeo: Chapter Three, Section One
Geo: Chapter Three, Section OneMr. Philen
 
Weather And Climate
Weather And ClimateWeather And Climate
Weather And ClimateMrs. Henley
 
Weather and climate
Weather and climateWeather and climate
Weather and climateAra Lucas
 
Geography revision weather and climate
Geography revision   weather and climateGeography revision   weather and climate
Geography revision weather and climateBrittany Farrant
 
Tropical cyclone 2015
Tropical cyclone 2015Tropical cyclone 2015
Tropical cyclone 2015Henry Hollis
 
Class 7th science chapter 8. Winds, Storms and Cyclones
Class 7th science chapter 8. Winds, Storms and CyclonesClass 7th science chapter 8. Winds, Storms and Cyclones
Class 7th science chapter 8. Winds, Storms and CyclonesSwayam Khobragade
 
Unit3 climateandlivingbeings-ppt-110306065855-phpapp02
Unit3 climateandlivingbeings-ppt-110306065855-phpapp02Unit3 climateandlivingbeings-ppt-110306065855-phpapp02
Unit3 climateandlivingbeings-ppt-110306065855-phpapp02deewoodard
 
Grade 12 notes (CLIMATE AND WEATHER).pdf
Grade 12 notes (CLIMATE AND WEATHER).pdfGrade 12 notes (CLIMATE AND WEATHER).pdf
Grade 12 notes (CLIMATE AND WEATHER).pdfBRYAN SHINGANGE
 
Introduction to GCSE Weather
Introduction to GCSE WeatherIntroduction to GCSE Weather
Introduction to GCSE Weatherjacksonthree
 
Temperate Cyclones
Temperate CyclonesTemperate Cyclones
Temperate CyclonesJohn Lanser
 

Similaire à Weather Systems Revision 2014 (20)

Weather elements and factors
Weather elements and factorsWeather elements and factors
Weather elements and factors
 
Weather and climate 7C
Weather and climate 7CWeather and climate 7C
Weather and climate 7C
 
Weather
WeatherWeather
Weather
 
Unit 3. climate and living beings.ppt
Unit 3. climate and living beings.pptUnit 3. climate and living beings.ppt
Unit 3. climate and living beings.ppt
 
Weather & climate project by Matthew Ben Hamed 3.02
Weather & climate project  by Matthew Ben Hamed 3.02Weather & climate project  by Matthew Ben Hamed 3.02
Weather & climate project by Matthew Ben Hamed 3.02
 
Geo: Chapter Three, Section One
Geo: Chapter Three, Section OneGeo: Chapter Three, Section One
Geo: Chapter Three, Section One
 
Weather And Climate
Weather And ClimateWeather And Climate
Weather And Climate
 
Weather
WeatherWeather
Weather
 
Weather and climate
Weather and climateWeather and climate
Weather and climate
 
Geography revision weather and climate
Geography revision   weather and climateGeography revision   weather and climate
Geography revision weather and climate
 
Tropical cyclone 2015
Tropical cyclone 2015Tropical cyclone 2015
Tropical cyclone 2015
 
Class 7th science chapter 8. Winds, Storms and Cyclones
Class 7th science chapter 8. Winds, Storms and CyclonesClass 7th science chapter 8. Winds, Storms and Cyclones
Class 7th science chapter 8. Winds, Storms and Cyclones
 
Unit3 climateandlivingbeings-ppt-110306065855-phpapp02
Unit3 climateandlivingbeings-ppt-110306065855-phpapp02Unit3 climateandlivingbeings-ppt-110306065855-phpapp02
Unit3 climateandlivingbeings-ppt-110306065855-phpapp02
 
Grade 12 notes (CLIMATE AND WEATHER).pdf
Grade 12 notes (CLIMATE AND WEATHER).pdfGrade 12 notes (CLIMATE AND WEATHER).pdf
Grade 12 notes (CLIMATE AND WEATHER).pdf
 
Introduction to GCSE Weather
Introduction to GCSE WeatherIntroduction to GCSE Weather
Introduction to GCSE Weather
 
Unit 1 (2) (1).pptx
Unit 1 (2) (1).pptxUnit 1 (2) (1).pptx
Unit 1 (2) (1).pptx
 
Lec 10.ppt
Lec 10.pptLec 10.ppt
Lec 10.ppt
 
Weather.Climate.Notes.ppt
Weather.Climate.Notes.pptWeather.Climate.Notes.ppt
Weather.Climate.Notes.ppt
 
world climates finale
world climates finaleworld climates finale
world climates finale
 
Temperate Cyclones
Temperate CyclonesTemperate Cyclones
Temperate Cyclones
 

Plus de douglasgreig

Swanage power point presentation (reduced)
Swanage power point presentation (reduced)Swanage power point presentation (reduced)
Swanage power point presentation (reduced)douglasgreig
 
Thermo Powder Presentation - Catalytic Learning Day 2014
Thermo Powder Presentation - Catalytic Learning Day 2014Thermo Powder Presentation - Catalytic Learning Day 2014
Thermo Powder Presentation - Catalytic Learning Day 2014douglasgreig
 
Reciprocal Reading
Reciprocal ReadingReciprocal Reading
Reciprocal Readingdouglasgreig
 
Habits of mind launch
Habits of mind launchHabits of mind launch
Habits of mind launchdouglasgreig
 
Weather under high and low pressure
Weather under high and low pressureWeather under high and low pressure
Weather under high and low pressuredouglasgreig
 
Players practice question modelling exercise
Players practice question modelling exercisePlayers practice question modelling exercise
Players practice question modelling exercisedouglasgreig
 
Literacy focus fortnight
Literacy focus fortnightLiteracy focus fortnight
Literacy focus fortnightdouglasgreig
 
Meeting the needs of deaf students practical tips for teachers
Meeting the needs of deaf students   practical tips for teachersMeeting the needs of deaf students   practical tips for teachers
Meeting the needs of deaf students practical tips for teachersdouglasgreig
 
Excellence through creativity
Excellence through creativityExcellence through creativity
Excellence through creativitydouglasgreig
 
Inset post 16 (reduced)
Inset post 16 (reduced)Inset post 16 (reduced)
Inset post 16 (reduced)douglasgreig
 
Communication training 2013 a
Communication training 2013 aCommunication training 2013 a
Communication training 2013 adouglasgreig
 
Developing questioning for learning
Developing questioning for learningDeveloping questioning for learning
Developing questioning for learningdouglasgreig
 
Tectonic Hazards Global Trends Overview
Tectonic Hazards Global Trends OverviewTectonic Hazards Global Trends Overview
Tectonic Hazards Global Trends Overviewdouglasgreig
 
Formation of the Grand Canyon Starter
Formation of the Grand Canyon StarterFormation of the Grand Canyon Starter
Formation of the Grand Canyon Starterdouglasgreig
 
What makes a good Unit 4 Essay Answer?
What makes a good Unit 4 Essay Answer?What makes a good Unit 4 Essay Answer?
What makes a good Unit 4 Essay Answer?douglasgreig
 
Proof of Progress Minibite (zs)
Proof of Progress Minibite (zs)Proof of Progress Minibite (zs)
Proof of Progress Minibite (zs)douglasgreig
 
Deaf awareness minibites
Deaf awareness minibitesDeaf awareness minibites
Deaf awareness minibitesdouglasgreig
 
Starting your lesson with talk
Starting your lesson with talkStarting your lesson with talk
Starting your lesson with talkdouglasgreig
 

Plus de douglasgreig (20)

Swanage power point presentation (reduced)
Swanage power point presentation (reduced)Swanage power point presentation (reduced)
Swanage power point presentation (reduced)
 
Thermo Powder Presentation - Catalytic Learning Day 2014
Thermo Powder Presentation - Catalytic Learning Day 2014Thermo Powder Presentation - Catalytic Learning Day 2014
Thermo Powder Presentation - Catalytic Learning Day 2014
 
Reciprocal Reading
Reciprocal ReadingReciprocal Reading
Reciprocal Reading
 
Habits of mind launch
Habits of mind launchHabits of mind launch
Habits of mind launch
 
Weather under high and low pressure
Weather under high and low pressureWeather under high and low pressure
Weather under high and low pressure
 
Players practice question modelling exercise
Players practice question modelling exercisePlayers practice question modelling exercise
Players practice question modelling exercise
 
Literacy focus fortnight
Literacy focus fortnightLiteracy focus fortnight
Literacy focus fortnight
 
Meeting the needs of deaf students practical tips for teachers
Meeting the needs of deaf students   practical tips for teachersMeeting the needs of deaf students   practical tips for teachers
Meeting the needs of deaf students practical tips for teachers
 
Excellence through creativity
Excellence through creativityExcellence through creativity
Excellence through creativity
 
Inset post 16 (reduced)
Inset post 16 (reduced)Inset post 16 (reduced)
Inset post 16 (reduced)
 
Communication training 2013 a
Communication training 2013 aCommunication training 2013 a
Communication training 2013 a
 
What is autism
What is autismWhat is autism
What is autism
 
Blooms taxonomy
Blooms taxonomyBlooms taxonomy
Blooms taxonomy
 
Developing questioning for learning
Developing questioning for learningDeveloping questioning for learning
Developing questioning for learning
 
Tectonic Hazards Global Trends Overview
Tectonic Hazards Global Trends OverviewTectonic Hazards Global Trends Overview
Tectonic Hazards Global Trends Overview
 
Formation of the Grand Canyon Starter
Formation of the Grand Canyon StarterFormation of the Grand Canyon Starter
Formation of the Grand Canyon Starter
 
What makes a good Unit 4 Essay Answer?
What makes a good Unit 4 Essay Answer?What makes a good Unit 4 Essay Answer?
What makes a good Unit 4 Essay Answer?
 
Proof of Progress Minibite (zs)
Proof of Progress Minibite (zs)Proof of Progress Minibite (zs)
Proof of Progress Minibite (zs)
 
Deaf awareness minibites
Deaf awareness minibitesDeaf awareness minibites
Deaf awareness minibites
 
Starting your lesson with talk
Starting your lesson with talkStarting your lesson with talk
Starting your lesson with talk
 

Weather Systems Revision 2014

  • 1.
  • 2. Theme 2 - Weather and Climate Weather Is the conditions of the atmosphere in the short term - over a day or a week. It is made up of temperature, rainfall, humidity, wind speed, wind direction, air pressure and other characteristics of the air around us. Climate Is the generalised conditions of the precipitation and temperature over a year. The figures are averaged out over a long period of time - this is normally a minimum of 30 years. Weather is … It includes … It involves changes in the … Climate is … It includes … It involves changes in the …
  • 3. Condition High or Low Pressure Cold and warm fronts Sinking air High level of condensation Low precipitation Sunny conditions in summer Cold and frosty conditions in winter Condition High or Low Pressure Warm air rising over cold air Thunderstorms in the afternoon in Summer. Very stable conditions for a number of days or weeks Low levels of condensation. Rain, followed by few hours of dry, followed by heavy rain. Storm conditions and isobars that are close together. High or Low Pressure? High High Low High High Low High High High Low Low Low
  • 5. The Importance of Air Masses An air mass is a block of air that has similar temperature and moisture characteristics. Where the ‘air comes from’ has a big impact on our weather and climate.
  • 6.
  • 7. The Importance of Air Masses An air mass is a block of air that has similar temperature and moisture characteristics. Where the ‘air comes from’ has a big impact on our weather and climate.
  • 8. Link - 1’10” in Link 2 Link 3
  • 9.
  • 10.
  • 11.
  • 12.
  • 13.
  • 14.
  • 15. Sandstorms in the Sahara Desert in Northern Africa collect and transport lots of sand and dust into the atmosphere. This is picked up by the wind moving clockwise in the high pressure. Air in a high pressure (anticyclone) moves in a clockwise direction. This creates an air mass moving over the UK from the South. The Tropical Continental Air Mass (Tc) is full of dust and sand which have been picked up from the storms in the Sahara Air in a high pressure sinks creating very stable conditions. Wind speeds tend to be light and calm. Sinking air with calm conditions means that levels of pollution in the atmosphere can build up. The air mass affecting the UK crosses some of the big industrial regions of Europe - Northern France, Belgium and Germany. High Pressure Stretch and Challenge •High pressure systems block other weather systems, especially low pressures and so can last for several days, even weeks. This means the weather conditions can remain similar for some time. •Isobars in High Pressure systems tend to be spread out; the pressure gradient is low. •Sinking air means the chance of condensation is low, and thus precipitation levels are low. This means there is little or no rainfall to wash pollutants and dust out of the atmosphere. •Microclimates in urban areas mean that high pressure conditions trap pollution emitted by transport and industrial sources in the local area. This combines with pollutants transported from further afield.
  • 16.
  • 17. • Moves from East to West • Crosses three countries - Philippines 26-27 September, Vietnam 29th September, and Laos/Cambodia on 30th September. • Turns from a tropical depression, into a Tropical Storm, into Typhoon and then back into a Tropical Storm. • Begins in the Philippine Sea, and moves west across the South China Sea. • North of the Equator but South of the Tropic of Cancer.
  • 18. • Highest number of deaths in the Philippines. • Whereas lowest number of deaths in Cambodia. • Deaths in Vietnam and Cambodia together are less than those in the Philippines. • Damage is greatest in Vietnam. • Damage is lowest in Philippines. • Damage in the Philippines and Cambodia together is less than that in Vietnam. • Homelessness is highest in Philippines. • In contrast Cambodia has the lowest homelessness. • Similarly Vietnam had a high level of evacuation - although this isn’t the same as homelessness.
  • 19. Cause of floods: • Impermeable surfaces - lack of infiltration, so rapid run-off. • Poor drainage in informal settlements - rapid population growth led to poor level of infrastructure. • High population density - lots of people affected in a small area. Impact on Quality life • Economic: • Social: • Environmental: People can’t get to work easily. Many businesses shut. People will see a fall in income which could increase poverty when people are already ‘on the edge’. Emergency services cannot access those who need help - rise in diseases and ill health. Communities are cut off - people cannot access food and clean water. Sanitation systems are flooded - dirty and contaminated water in many areas. Spreads disease very easily - young people, the sick and the old very vulnerable.
  • 20. You’ve been given some case study revision notes about the impact of low pressure weather systems. However, they need improving - your challenge is to mark them and indicate where improvements need to be made, and to make them. Check for: • Detailed information. • Specific evidence and facts. • Clear structure and small chunks of information. • Complex ideas and understanding - stretch yourself and apply ‘BIG’ ideas.
  • 21. For a period of weather caused by high or low pressure. • Name and locate the area affected by the weather. • Describe the main features of the weather. • Explain how the weather affected different groups of people. [8 marks] Name: • UK - high levels of rain and flooding in 2012. Describe: • Higher than average rainfall • Caused by higher air temperatures linked to Global Warming • Caused by change in the position of the Jet Stream - air masses created conditions for high rainfall • Ground became quickly saturated - flooding in many drainage basins across the UK • Higher populations on flood plains - more people at risk of flooding Explain impacts on different groups: • Homeowners • Farmers • Insurance Companies • People in General
  • 22. Challenge What does warm air rise? Your answer?
  • 23.
  • 24.
  • 25.
  • 26.
  • 27.
  • 28. Describe Explain 10 o C, 8 oktas of cloud, drizzle, Force 5 Wind from the SSW. Located at the warm front. In the next few hours it will get warmer and the drizzle will stop. Warm air is rising over cold air. As the air rises it cools, and this means water vapour condenses to form clouds. This causes the rainfall, along with the TM air that is warm and moist which comes from the SSW.
  • 29. Describe Explain 11 o C, 8 oktas of cloud, rain, Force 5 Wind from the W. Located at the warm front. In the next few hours it will briefly get warmer and then it will rain heavily as the cold front arrives. Warm air is rising over cold air. As the air rises it cools, and this means water vapour condenses to form clouds. This causes the rainfall, along with the TM air that is warm and moist which comes from the W.
  • 30. Describe Explain 13 o C, 3 oktas of cloud, rain, Force 3 Wind from the SW. Located in the warm sector. In the next few hours it will begin to rain heavily as the cold front arrives and temperatures will fall. In between the warm and cold fronts is a block of warm air. This creates an area of more stable and calmer weather. However as the cold front approaches, warm air will once again rise over cold creating the conditions for rainfall.
  • 31. The weather at Point A is wet and windy. Temperatures are 9oC, and the wind is blowing from the South West, and is Force 4. There is quite a lots of cloud, and there is drizzle. This is the warm front where a warm air mass is meeting a cold air mass. They don’t mix because they are different densities. Condensation leads to precipitation and this is why it is raining. The weather at Point A is wet and windy. Temperatures are 9oC, and the wind is blowing from the South West, and is Force 4. There are 7 okras of cloud cover and it is drizzling. This is the warm front. Warm air is being forced over cold air because it is less dense. As it rises it cools, which lets water vapour condense to form clouds. As the clouds build up eventually it will rain. This frontal system is a low pressure as the different air masses have different densities and one rises over the other. Answer A Answer B