Higher Higher Atmosphere Atmosphere

Slides:



Advertisements
Similar presentations
Seasonal Shift of the ICTZ
Advertisements

The Inter-Tropical Convergence Zone. The greatest amount of rain falls across the coast of West Africa. Here rainfall can exceed 2000mm per year. The.
16.2 Changing weather.
ITCZ ITCZ.
Higher Atmosphere. Higher Atmosphere Higher Atmosphere An isohyet is a line on a map connecting points having the same amount of rainfall in a given.
Outline Further Reading: Chapter 10 of the text book - wet tropical climate - coastal trade wind climate - dry tropical climate Natural Environments: The.
International Tropical Convergence Zone
1 Valley Breeze Example ©1997 Prentice-Hall, Inc..
* The relative measure of the amount of water vapor in the air * Psychrometer * Water vapor affects the density of the air. * Cold air is heavier than.
Air Masses and Air Mass Weather
Chapter 8: Air Masses, Fronts Mid-Latitude Cyclones Air Masses  large body of air whose properties of temperature and humidity are fairly similar in any.
1 By the end of this topic you should be able to:  explain with the aid of an annotated diagram, why Tropical latitudes receive more of the sun’s energy.
INTER-TROPICAL CONVERGENCE ZONE (ITCZ).
Air Masses What is an air mass?. Air Mass  An air mass is a large volume of air defined by its temperature and water vapor content. air temperaturewater.
Study Guide Chapter 7 1.  Define the following air mass symbols: mE, MT, cT, mP, cP, and cA. 2.    What are the 5 air masses that influence the weather.
Shuddle and Atmosphere  Lego Shuttle reached an altitude of 35,000 meters. Which layers of the atmosphere did the shuttle reach before descending back.
Air Masses. Air Mass Descriptors: Continental: Originates over land- Dry Continental: Originates over land- Dry Maritime: Originates over ocean -Moist.
TYPES OF AIR MASSES. TEMPERATURE TEMPERATURE HUMIDITY.
Mr. Fetch’s Earth Science Classroom Air Masses A large body of air with similar -TEMPERATURE - HUMIDITY Warm Cold Temperature Moist Dry Humidity.
Chapter 29 Air Masses and Fronts. Air Masses A huge section of the lower troposphere that has the same kind of weather throughout.
* The measure of the amount of water vapor in the air * Psychrometer * Water vapor affects the density of the air. * Cold air is more dense than warm.
Air Masses Air masses- huge body of air that has similar temperature, humidity, and air pressure at any given height. 1 air mass can spread over millions.
Aim : How do we describe air mass characteristics? Air masses are uniquely classified according to; The nature of the surface in the source region The.
Air Masses. Air- What’s the Difference? Incoming solar radiation heats the air Not all places on Earth get the same amounts of solar radiation. Unequal.
Chapter 20: Air Masses Section Agenda Origins of an Air Mass Types of Air Masses -Continental Artic -Continental Polar -Maritime Polar -Continental.
Air Masses and ITCZ. Topic 4: Air Masses and ITCZ Global wind circulation and ocean currents are important in determining climate patterns. These are.
Air Masses Earth Science Mr. Margetan. Air Masses  Air Mass – A stationary or slow moving body of air with uniform temperature and humidity –Can be thousands.
Weather National 5 supported study
Air Masses Air masses are large bodies of air where temperature and moisture content are constant throughout. Moisture content and temperature of a mass.
Air masses get their characteristics based on
©Mark Place, Air Masses.
Aim: How do air masses differ?
describe and interpret climate maps, diagrams and graphs
Weather & Storms.
The Inter-Tropical Convergence Zone
Air masses & the UK climate
Gairloch High School / Invergordon Academy
Cloud Formation and Air Masses
Cloud Formation and Air Masses
Air Masses and Fronts.
Wednesday 3/7/17 Notebook Entry: Describe what you think is happening in this picture. I took this picture a few years ago driving between Townsend and.
Bell Ringer Describe general air temperature on a cloudy night. Compare this to a clear night. Describe the type of weather expected with each of the following:
Air Masses.
24-1 Air Masses.
Air Masses.
Air Masses A huge body of air
Air Masses.
©Mark Place, Air Masses.
Climate Classification
What is an air mass. Large area of air floating above us
Climate Classification
An Introduction to Types and Formation
Air Masses Chapter 21 Section 1.
Gairloch High School / Invergordon Academy
What is an air mass. Large area of air floating above us
Air Masses Air masses are large bodies of air where temperature and moisture content are constant throughout. Moisture content and temperature of a mass.
Air Masses and Weather.
HIGHER GEOGRAPHY PHYSICAL CORE ATMOSPHERE.
Air Masses.
©Mark Place, Air Masses.
Air Masses and Weather.
Rapid movement Gradual movement
6.9: Air Masses Unit 6: Meteorology March 13, 2012 Sanders.
©Mark Place, Air Masses.
©Mark Place, Air Masses.
©Mark Place, Air Masses.
Air Masses and Weather.
Please find this page in your notes toward the end
Air Masses Air masses are large bodies of air where temperature and moisture content are constant throughout. Moisture content and temperature of a mass.
An Introduction to Types and Formation
Presentation transcript:

Higher Higher Atmosphere Atmosphere The Inter-Tropical Convergence Zone [Date] Today I will: Be introduced to the ITCZ Be able to describe the characteristics of the air masses which come together to form the ITCZ

Higher Atmosphere

Higher Atmosphere [Task One] Mark on the countries in West Africa. [Task Two] Neatly add in the Equator, Tropics and Oceans.

Higher Atmosphere

Higher Higher Atmosphere Atmosphere Describe the origin, nature and characteristics of the Maritime Tropical and Continental Tropical air masses. [6 marks] Maritime Tropical (mT) Name of Wind – South Western Monsoon Origin – Atlantic Ocean, in tropical latitudes Weather characteristics – hot, high humidity, warm Nature – unstable Continental Tropical (cT) Name of Wind - Harmattan Origin – Sahara Desert, in tropical latitudes Weather characteristics – hot/very hot, dry, low humidity, warm Nature – stable