SlideShare a Scribd company logo
1 of 26
CLIMATE, WEATHER,
WEATHER FRONTS,

AND THE WEATHER MAP
Weather is what conditions of the atmosphere are
over a short period of time.
Climate is how the atmosphere "behaves" over long
periods of time.
Weather forecasting is predicting what the weather
will be like at a certain time in the near future, in a
given location.
The weather map tells the distribution patterns of
atmospheric pressure, wind, temperature and
humidity at the different levels of the atmosphere.
The Weather Symbols:
Air Pressure- This is the weight or pressure the air
exerts on the ground and is measured in millibars.
An air mass is a large body of air that has similar
temperature and moisture properties throughout.
A weather front is a boundary separating two
masses of air of different densities, and is the main
cause of different wheather conditions.
The 4 types of weather fronts:
Cold front- a front in which cold air is replacing warm
air at the surface.
Some of the characteristics of cold fronts include the following:
•
The slope of a typical cold front is 1:100 (vertical to horizontal).
•
Cold fronts tend to move faster than all other types of fronts.
•
Cold fronts tend to be associated with the most violent weather among
all types of fronts.
•
Cold fronts tend to move the farthest while maintaining their intensity.
•
Cold fronts tend to be associated with cirrus well ahead of the front,
strong thunderstorms along and ahead of the front, and a broad area of
clouds immediately behind the front (although fast movingfronts may be
mostly clear behind the front).
•
Cold fronts can be associated with squall lines (a line of strong
thunderstorms parallel to and ahead of the front).
•
Cold fronts almost always are easier to locate on a weather map than
are warm fronts, primarily because of the strength of the high pressure
system to the north and west of the cold front compared to that north of
a warm front.
•
•

Cold fronts usually bring cooler weather, clearing skies, and a sharp
change in wind direction.
Warm front- a front in which warm air replaces cooler
air at the surface.
Some of the characteristics of warm fronts include the
following:
• The slope of a typical warm front is 1:200 (more gentle than
cold fronts).
• Warm fronts tend to move slowly.
• Warm fronts are typically less violent than cold fronts.
• Although they can trigger thunderstorms, warm fronts are more
likely to be associated with large regions of gentle ascent
(stratiform clouds and light to moderate continuous rain).
• Warm fronts are usually preceded by cirrus first (1000 km
ahead), then altostratus or altocumulus (500 km ahead), then
stratus and possibly fog.
• Behind the warm front, skies are relatively clear (but change
gradually).
• Warm fronts are associated with a frontal inversion(warm air
overrunning cooler air).
Stationary front- a front that does not move or barely
moves.
•

Stationary front- a front that does not move or barely
moves.

•
•

Stationary fronts behave like warm fronts, but are more
quiescent.

•
•

Many times the winds on both sides of a stationary front
are parallel to the front.

•
•

Typically stationary fronts form when polar air masses are
modified significantly so as to lose their character (e.g.,
cold fronts which stall).
Occluded Front- forms when a faster cold front overtakes a
warm front.
•

•
•

Because cold fronts move faster than warm fronts, they can
catch up to and overtake their related warm front. When they
do, an occluded front is formed.
Occluded fronts are indicative of mature storm systems (i.e.,
those about to dissipate).
The most common type of occlusion in North America is called
a cold-front occlusion and it occurs when the cold front forces
itself under the warm front.The weather ahead of the cold
occlusion is similar to that of a warm front while that along and
behind the cold occlusion is similar to that of a cold front.














Note the three different kinds of front shown on the map - a cold front, a warm front and an
occluded front.
Fronts occur where two different air masses meet.
Warm fronts are formed when warm air rises over a mass of cold air. As theair lifts into
regions of lower pressure, it expands, cools and condenses the water vapour as wide, flat
sheets of cloud.
Warm fronts are shown on synoptic charts by a solid line with semicircles pointing towards
the colder air and in the direction of movement. On colouredweather maps, a warm front is
drawn with a solid red line with red semicircles.
Cold fronts are usually associated with depressions. A cold front is thetransition
zone where a cold air mass is replacing the warmer air mass. The cold air is following the
warm air and gradually moves underneath the warmer air. When the warm air is pushed
upwards it will rain heavily. Often more rain will fall in the few minutes the cold front passes
than it will during the whole passage of a warm front. As the cold front passes, the clouds
roll by and the air temperature is cooler.
Cold fronts are shown on synoptic charts by a solid line with triangles along the front
pointing towards the warmer air and in the direction of movement. On coloured weather
maps, a cold front is drawn with a solid blue line with blue triangles.
Occluded fronts occur at the point where a cold front takes over a warm front or the other
way around. If a cold front undercuts a warm front it is known as a cold occlusion and if the
cold front rises over the warm front it is called a warm occlusion. Occluded fronts bring
changeable weather conditions.
On a synoptic chart occluded fronts are represented by semicircles and triangles
positioned next to each other. The triangles are in blue and the semicircles are in red, or
both are purple (mixing both red and blue colours together).
Isobars are lines on a weather map joining together places of equal atmospheric
pressure. On the map the isobar marked 1004 represents an area of high
pressure, while the isobar marked 976 represents an area of low pressure.
Example of a weather map:
EXERCISE A. Match the meanings with the correct symbols. Write the
letters on the spaces.
a. Rain with sunny
intervals
b. Thunderstorm

c. Temperature (oC)
d. Wind and speed
direction
e. Sunny Interval
f. Sunshine
g. Rain
h. Fair weather cloud
interval
i. Dull weather cloud
j. Snow
EXERCISE B. Write the symbols to make a weather map. Use the description given.
(Exercise should be printed on a paper for the students to write on.)

1.) Chiang Mai
- Fair weather
- temperature- 15 oC
2.) Udon Thani
- Dull weather
- temperature – 18 oC
3.) A cold front passes through
Doi Inthanon, Lampang,
Sukhothai, Nakhon Pathom
and Surat Thani
4.) Bangkok
- Rainy with sunny intervals
- Winds = 25, east
5.) Phuket
- Thunderstorm
- 21 oC

More Related Content

What's hot

Changes in the atmosphere
Changes in the atmosphereChanges in the atmosphere
Changes in the atmosphere
cdenef
 
Weather and Climate
Weather and ClimateWeather and Climate
Weather and Climate
tcooper66
 
Atmospheric circulation
Atmospheric circulationAtmospheric circulation
Atmospheric circulation
Sarah Zurcaled
 
Circulation of the Atmosphere
Circulation of the AtmosphereCirculation of the Atmosphere
Circulation of the Atmosphere
ZBTHS
 

What's hot (20)

Pressure And Winds
Pressure And WindsPressure And Winds
Pressure And Winds
 
Meteorology and Climate
Meteorology and ClimateMeteorology and Climate
Meteorology and Climate
 
Map Projections
Map ProjectionsMap Projections
Map Projections
 
Weather and climate: basic concepts
Weather and climate: basic conceptsWeather and climate: basic concepts
Weather and climate: basic concepts
 
Changes in the atmosphere
Changes in the atmosphereChanges in the atmosphere
Changes in the atmosphere
 
Climatology scope and principles
Climatology scope and principlesClimatology scope and principles
Climatology scope and principles
 
Lesson 17: Weather and Climate
Lesson 17: Weather and ClimateLesson 17: Weather and Climate
Lesson 17: Weather and Climate
 
Air Masses and Fronts
Air Masses and FrontsAir Masses and Fronts
Air Masses and Fronts
 
seasons and insolation presentation
seasons and insolation presentationseasons and insolation presentation
seasons and insolation presentation
 
Shape, size and motions of the earth 1
Shape, size and motions of the earth 1Shape, size and motions of the earth 1
Shape, size and motions of the earth 1
 
3. Atmospheric circulation
3. Atmospheric circulation3. Atmospheric circulation
3. Atmospheric circulation
 
Atmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology ChapterAtmospheric circulation-Climatology Chapter
Atmospheric circulation-Climatology Chapter
 
AIR MASSES AND FRONT
AIR MASSES AND FRONTAIR MASSES AND FRONT
AIR MASSES AND FRONT
 
Weather and Climate
Weather and ClimateWeather and Climate
Weather and Climate
 
Atmospheric circulation
Atmospheric circulationAtmospheric circulation
Atmospheric circulation
 
Jet stream
Jet streamJet stream
Jet stream
 
Lecture Atmospheric Temperature
Lecture Atmospheric TemperatureLecture Atmospheric Temperature
Lecture Atmospheric Temperature
 
Circulation of the Atmosphere
Circulation of the AtmosphereCirculation of the Atmosphere
Circulation of the Atmosphere
 
Local Wind
Local WindLocal Wind
Local Wind
 
Introduction to atmospheric science
Introduction to atmospheric scienceIntroduction to atmospheric science
Introduction to atmospheric science
 

Viewers also liked

Are you smarter than a 6th grader (unit 1 math)
Are you smarter than a 6th grader (unit 1 math)Are you smarter than a 6th grader (unit 1 math)
Are you smarter than a 6th grader (unit 1 math)
Steven Gabrys
 
Reading a Weather Map
Reading a Weather MapReading a Weather Map
Reading a Weather Map
dumouchelle
 
Depressions and anticyclones synoptic charts
Depressions and anticyclones synoptic chartsDepressions and anticyclones synoptic charts
Depressions and anticyclones synoptic charts
lesliehome
 
Weather and Climate by Andrea Bellizzi, 3.01
Weather and Climate by Andrea Bellizzi, 3.01Weather and Climate by Andrea Bellizzi, 3.01
Weather and Climate by Andrea Bellizzi, 3.01
geographystudents
 
Hurricanes & Tropical depressions 2011 cloutier
Hurricanes & Tropical depressions 2011 cloutierHurricanes & Tropical depressions 2011 cloutier
Hurricanes & Tropical depressions 2011 cloutier
Annie C. Cloutier
 
Cyclone and anticyclone
Cyclone and anticycloneCyclone and anticyclone
Cyclone and anticyclone
Yenyen H
 

Viewers also liked (20)

Are you smarter than a 6th grader (unit 1 math)
Are you smarter than a 6th grader (unit 1 math)Are you smarter than a 6th grader (unit 1 math)
Are you smarter than a 6th grader (unit 1 math)
 
How to read a weather map
How to read a weather mapHow to read a weather map
How to read a weather map
 
Weather and Climate
Weather and ClimateWeather and Climate
Weather and Climate
 
Synoptic chart.
Synoptic chart.Synoptic chart.
Synoptic chart.
 
Weather map
Weather mapWeather map
Weather map
 
Reading a Weather Map
Reading a Weather MapReading a Weather Map
Reading a Weather Map
 
Depressions and anticyclones synoptic charts
Depressions and anticyclones synoptic chartsDepressions and anticyclones synoptic charts
Depressions and anticyclones synoptic charts
 
Weather and Climate by Andrea Bellizzi, 3.01
Weather and Climate by Andrea Bellizzi, 3.01Weather and Climate by Andrea Bellizzi, 3.01
Weather and Climate by Andrea Bellizzi, 3.01
 
Hurricanes & Tropical depressions 2011 cloutier
Hurricanes & Tropical depressions 2011 cloutierHurricanes & Tropical depressions 2011 cloutier
Hurricanes & Tropical depressions 2011 cloutier
 
Introduction to GCSE Weather
Introduction to GCSE WeatherIntroduction to GCSE Weather
Introduction to GCSE Weather
 
Reading synoptic charts
Reading synoptic chartsReading synoptic charts
Reading synoptic charts
 
Anticyclone Case Study
Anticyclone Case StudyAnticyclone Case Study
Anticyclone Case Study
 
fronts and mid latitude cyclones
fronts and mid latitude cyclonesfronts and mid latitude cyclones
fronts and mid latitude cyclones
 
10- weather notes
 10-  weather notes 10-  weather notes
10- weather notes
 
Cyclone and anticyclone
Cyclone and anticycloneCyclone and anticyclone
Cyclone and anticyclone
 
ANTICYCLONES QUESTIONS
ANTICYCLONES QUESTIONSANTICYCLONES QUESTIONS
ANTICYCLONES QUESTIONS
 
form-1-science-chapter-5-part2
 form-1-science-chapter-5-part2 form-1-science-chapter-5-part2
form-1-science-chapter-5-part2
 
BI - ANTICYCLONES
BI - ANTICYCLONES BI - ANTICYCLONES
BI - ANTICYCLONES
 
10- ppt notes- severe weather
 10- ppt notes- severe weather 10- ppt notes- severe weather
10- ppt notes- severe weather
 
Mapwork Basic Skills.ppt
Mapwork Basic Skills.pptMapwork Basic Skills.ppt
Mapwork Basic Skills.ppt
 

Similar to Understanding the Weather Map

Ghs Depression
Ghs DepressionGhs Depression
Ghs Depression
neilgood
 
period 3 group 4
period 3 group 4period 3 group 4
period 3 group 4
wmasd
 
Notes - Air Masses, Fronts, Global Winds
Notes - Air Masses, Fronts, Global WindsNotes - Air Masses, Fronts, Global Winds
Notes - Air Masses, Fronts, Global Winds
Bantay's Oceanography
 
Chapter 16 & 17-weather and climate
Chapter 16 & 17-weather and climateChapter 16 & 17-weather and climate
Chapter 16 & 17-weather and climate
Steven_iannuccilli
 
Winds Air Masses Fronts
Winds Air Masses FrontsWinds Air Masses Fronts
Winds Air Masses Fronts
william seng
 
Weather and climate
Weather and climateWeather and climate
Weather and climate
Ara Lucas
 
Chapter 19
Chapter 19Chapter 19
Chapter 19
basdsci
 

Similar to Understanding the Weather Map (20)

FRONTS AND AIR MASSES.pptx
FRONTS AND AIR MASSES.pptxFRONTS AND AIR MASSES.pptx
FRONTS AND AIR MASSES.pptx
 
GEOGRAPHY IGCSE: WEATHER SYSTEMS
GEOGRAPHY IGCSE: WEATHER SYSTEMSGEOGRAPHY IGCSE: WEATHER SYSTEMS
GEOGRAPHY IGCSE: WEATHER SYSTEMS
 
Ghs Depression
Ghs DepressionGhs Depression
Ghs Depression
 
Pertemuan 03 front
Pertemuan 03 frontPertemuan 03 front
Pertemuan 03 front
 
period 3 group 4
period 3 group 4period 3 group 4
period 3 group 4
 
fronts- their formation and kinds
fronts- their formation and kindsfronts- their formation and kinds
fronts- their formation and kinds
 
Meteorology -Weather acloutier 2011 power point
Meteorology -Weather acloutier 2011 power pointMeteorology -Weather acloutier 2011 power point
Meteorology -Weather acloutier 2011 power point
 
Presentation1 module 2
Presentation1 module 2Presentation1 module 2
Presentation1 module 2
 
Notes - Air Masses, Fronts, Global Winds
Notes - Air Masses, Fronts, Global WindsNotes - Air Masses, Fronts, Global Winds
Notes - Air Masses, Fronts, Global Winds
 
Chapter 16 & 17-weather and climate
Chapter 16 & 17-weather and climateChapter 16 & 17-weather and climate
Chapter 16 & 17-weather and climate
 
Air Masses, Global Winds, and Fronts
Air Masses, Global Winds, and FrontsAir Masses, Global Winds, and Fronts
Air Masses, Global Winds, and Fronts
 
Winds Air Masses Fronts
Winds Air Masses FrontsWinds Air Masses Fronts
Winds Air Masses Fronts
 
Climate & weather T1 GR12.pptx
Climate & weather T1 GR12.pptxClimate & weather T1 GR12.pptx
Climate & weather T1 GR12.pptx
 
6th Grade Chapter 18 Part 2
6th Grade Chapter 18 Part 26th Grade Chapter 18 Part 2
6th Grade Chapter 18 Part 2
 
Weather and climate
Weather and climateWeather and climate
Weather and climate
 
Weather
WeatherWeather
Weather
 
Ch 19 v2
Ch 19 v2Ch 19 v2
Ch 19 v2
 
Chapter 19
Chapter 19Chapter 19
Chapter 19
 
Chapter 19notes
Chapter 19notesChapter 19notes
Chapter 19notes
 
How do scientists predict weather (the whole lesson )
How do scientists predict weather (the whole lesson )How do scientists predict weather (the whole lesson )
How do scientists predict weather (the whole lesson )
 

Recently uploaded

1029 - Danh muc Sach Giao Khoa 10 . pdf
1029 -  Danh muc Sach Giao Khoa 10 . pdf1029 -  Danh muc Sach Giao Khoa 10 . pdf
1029 - Danh muc Sach Giao Khoa 10 . pdf
QucHHunhnh
 
1029-Danh muc Sach Giao Khoa khoi 6.pdf
1029-Danh muc Sach Giao Khoa khoi  6.pdf1029-Danh muc Sach Giao Khoa khoi  6.pdf
1029-Danh muc Sach Giao Khoa khoi 6.pdf
QucHHunhnh
 
The basics of sentences session 2pptx copy.pptx
The basics of sentences session 2pptx copy.pptxThe basics of sentences session 2pptx copy.pptx
The basics of sentences session 2pptx copy.pptx
heathfieldcps1
 
Seal of Good Local Governance (SGLG) 2024Final.pptx
Seal of Good Local Governance (SGLG) 2024Final.pptxSeal of Good Local Governance (SGLG) 2024Final.pptx
Seal of Good Local Governance (SGLG) 2024Final.pptx
negromaestrong
 

Recently uploaded (20)

1029 - Danh muc Sach Giao Khoa 10 . pdf
1029 -  Danh muc Sach Giao Khoa 10 . pdf1029 -  Danh muc Sach Giao Khoa 10 . pdf
1029 - Danh muc Sach Giao Khoa 10 . pdf
 
APM Welcome, APM North West Network Conference, Synergies Across Sectors
APM Welcome, APM North West Network Conference, Synergies Across SectorsAPM Welcome, APM North West Network Conference, Synergies Across Sectors
APM Welcome, APM North West Network Conference, Synergies Across Sectors
 
Z Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot GraphZ Score,T Score, Percential Rank and Box Plot Graph
Z Score,T Score, Percential Rank and Box Plot Graph
 
Ecological Succession. ( ECOSYSTEM, B. Pharmacy, 1st Year, Sem-II, Environmen...
Ecological Succession. ( ECOSYSTEM, B. Pharmacy, 1st Year, Sem-II, Environmen...Ecological Succession. ( ECOSYSTEM, B. Pharmacy, 1st Year, Sem-II, Environmen...
Ecological Succession. ( ECOSYSTEM, B. Pharmacy, 1st Year, Sem-II, Environmen...
 
Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..Sports & Fitness Value Added Course FY..
Sports & Fitness Value Added Course FY..
 
1029-Danh muc Sach Giao Khoa khoi 6.pdf
1029-Danh muc Sach Giao Khoa khoi  6.pdf1029-Danh muc Sach Giao Khoa khoi  6.pdf
1029-Danh muc Sach Giao Khoa khoi 6.pdf
 
Unit-V; Pricing (Pharma Marketing Management).pptx
Unit-V; Pricing (Pharma Marketing Management).pptxUnit-V; Pricing (Pharma Marketing Management).pptx
Unit-V; Pricing (Pharma Marketing Management).pptx
 
SECOND SEMESTER TOPIC COVERAGE SY 2023-2024 Trends, Networks, and Critical Th...
SECOND SEMESTER TOPIC COVERAGE SY 2023-2024 Trends, Networks, and Critical Th...SECOND SEMESTER TOPIC COVERAGE SY 2023-2024 Trends, Networks, and Critical Th...
SECOND SEMESTER TOPIC COVERAGE SY 2023-2024 Trends, Networks, and Critical Th...
 
How to Give a Domain for a Field in Odoo 17
How to Give a Domain for a Field in Odoo 17How to Give a Domain for a Field in Odoo 17
How to Give a Domain for a Field in Odoo 17
 
Web & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdfWeb & Social Media Analytics Previous Year Question Paper.pdf
Web & Social Media Analytics Previous Year Question Paper.pdf
 
The basics of sentences session 2pptx copy.pptx
The basics of sentences session 2pptx copy.pptxThe basics of sentences session 2pptx copy.pptx
The basics of sentences session 2pptx copy.pptx
 
Seal of Good Local Governance (SGLG) 2024Final.pptx
Seal of Good Local Governance (SGLG) 2024Final.pptxSeal of Good Local Governance (SGLG) 2024Final.pptx
Seal of Good Local Governance (SGLG) 2024Final.pptx
 
Holdier Curriculum Vitae (April 2024).pdf
Holdier Curriculum Vitae (April 2024).pdfHoldier Curriculum Vitae (April 2024).pdf
Holdier Curriculum Vitae (April 2024).pdf
 
Unit-IV; Professional Sales Representative (PSR).pptx
Unit-IV; Professional Sales Representative (PSR).pptxUnit-IV; Professional Sales Representative (PSR).pptx
Unit-IV; Professional Sales Representative (PSR).pptx
 
Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...
Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...
Presentation by Andreas Schleicher Tackling the School Absenteeism Crisis 30 ...
 
Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1Código Creativo y Arte de Software | Unidad 1
Código Creativo y Arte de Software | Unidad 1
 
Measures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SDMeasures of Dispersion and Variability: Range, QD, AD and SD
Measures of Dispersion and Variability: Range, QD, AD and SD
 
This PowerPoint helps students to consider the concept of infinity.
This PowerPoint helps students to consider the concept of infinity.This PowerPoint helps students to consider the concept of infinity.
This PowerPoint helps students to consider the concept of infinity.
 
Measures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and ModeMeasures of Central Tendency: Mean, Median and Mode
Measures of Central Tendency: Mean, Median and Mode
 
Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"
Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"
Mattingly "AI & Prompt Design: Structured Data, Assistants, & RAG"
 

Understanding the Weather Map

  • 2. Weather is what conditions of the atmosphere are over a short period of time. Climate is how the atmosphere "behaves" over long periods of time. Weather forecasting is predicting what the weather will be like at a certain time in the near future, in a given location. The weather map tells the distribution patterns of atmospheric pressure, wind, temperature and humidity at the different levels of the atmosphere.
  • 4.
  • 5.
  • 6.
  • 7.
  • 8. Air Pressure- This is the weight or pressure the air exerts on the ground and is measured in millibars.
  • 9.
  • 10. An air mass is a large body of air that has similar temperature and moisture properties throughout. A weather front is a boundary separating two masses of air of different densities, and is the main cause of different wheather conditions.
  • 11. The 4 types of weather fronts:
  • 12. Cold front- a front in which cold air is replacing warm air at the surface.
  • 13. Some of the characteristics of cold fronts include the following: • The slope of a typical cold front is 1:100 (vertical to horizontal). • Cold fronts tend to move faster than all other types of fronts. • Cold fronts tend to be associated with the most violent weather among all types of fronts. • Cold fronts tend to move the farthest while maintaining their intensity. • Cold fronts tend to be associated with cirrus well ahead of the front, strong thunderstorms along and ahead of the front, and a broad area of clouds immediately behind the front (although fast movingfronts may be mostly clear behind the front). • Cold fronts can be associated with squall lines (a line of strong thunderstorms parallel to and ahead of the front). • Cold fronts almost always are easier to locate on a weather map than are warm fronts, primarily because of the strength of the high pressure system to the north and west of the cold front compared to that north of a warm front. • • Cold fronts usually bring cooler weather, clearing skies, and a sharp change in wind direction.
  • 14. Warm front- a front in which warm air replaces cooler air at the surface.
  • 15. Some of the characteristics of warm fronts include the following: • The slope of a typical warm front is 1:200 (more gentle than cold fronts). • Warm fronts tend to move slowly. • Warm fronts are typically less violent than cold fronts. • Although they can trigger thunderstorms, warm fronts are more likely to be associated with large regions of gentle ascent (stratiform clouds and light to moderate continuous rain). • Warm fronts are usually preceded by cirrus first (1000 km ahead), then altostratus or altocumulus (500 km ahead), then stratus and possibly fog. • Behind the warm front, skies are relatively clear (but change gradually). • Warm fronts are associated with a frontal inversion(warm air overrunning cooler air).
  • 16. Stationary front- a front that does not move or barely moves.
  • 17. • Stationary front- a front that does not move or barely moves. • • Stationary fronts behave like warm fronts, but are more quiescent. • • Many times the winds on both sides of a stationary front are parallel to the front. • • Typically stationary fronts form when polar air masses are modified significantly so as to lose their character (e.g., cold fronts which stall).
  • 18. Occluded Front- forms when a faster cold front overtakes a warm front.
  • 19. • • • Because cold fronts move faster than warm fronts, they can catch up to and overtake their related warm front. When they do, an occluded front is formed. Occluded fronts are indicative of mature storm systems (i.e., those about to dissipate). The most common type of occlusion in North America is called a cold-front occlusion and it occurs when the cold front forces itself under the warm front.The weather ahead of the cold occlusion is similar to that of a warm front while that along and behind the cold occlusion is similar to that of a cold front.
  • 20.
  • 21.         Note the three different kinds of front shown on the map - a cold front, a warm front and an occluded front. Fronts occur where two different air masses meet. Warm fronts are formed when warm air rises over a mass of cold air. As theair lifts into regions of lower pressure, it expands, cools and condenses the water vapour as wide, flat sheets of cloud. Warm fronts are shown on synoptic charts by a solid line with semicircles pointing towards the colder air and in the direction of movement. On colouredweather maps, a warm front is drawn with a solid red line with red semicircles. Cold fronts are usually associated with depressions. A cold front is thetransition zone where a cold air mass is replacing the warmer air mass. The cold air is following the warm air and gradually moves underneath the warmer air. When the warm air is pushed upwards it will rain heavily. Often more rain will fall in the few minutes the cold front passes than it will during the whole passage of a warm front. As the cold front passes, the clouds roll by and the air temperature is cooler. Cold fronts are shown on synoptic charts by a solid line with triangles along the front pointing towards the warmer air and in the direction of movement. On coloured weather maps, a cold front is drawn with a solid blue line with blue triangles. Occluded fronts occur at the point where a cold front takes over a warm front or the other way around. If a cold front undercuts a warm front it is known as a cold occlusion and if the cold front rises over the warm front it is called a warm occlusion. Occluded fronts bring changeable weather conditions. On a synoptic chart occluded fronts are represented by semicircles and triangles positioned next to each other. The triangles are in blue and the semicircles are in red, or both are purple (mixing both red and blue colours together).
  • 22. Isobars are lines on a weather map joining together places of equal atmospheric pressure. On the map the isobar marked 1004 represents an area of high pressure, while the isobar marked 976 represents an area of low pressure.
  • 23.
  • 24. Example of a weather map:
  • 25. EXERCISE A. Match the meanings with the correct symbols. Write the letters on the spaces. a. Rain with sunny intervals b. Thunderstorm c. Temperature (oC) d. Wind and speed direction e. Sunny Interval f. Sunshine g. Rain h. Fair weather cloud interval i. Dull weather cloud j. Snow
  • 26. EXERCISE B. Write the symbols to make a weather map. Use the description given. (Exercise should be printed on a paper for the students to write on.) 1.) Chiang Mai - Fair weather - temperature- 15 oC 2.) Udon Thani - Dull weather - temperature – 18 oC 3.) A cold front passes through Doi Inthanon, Lampang, Sukhothai, Nakhon Pathom and Surat Thani 4.) Bangkok - Rainy with sunny intervals - Winds = 25, east 5.) Phuket - Thunderstorm - 21 oC