Weather Lesson Seven Air Masses and Fronts.

Slides:



Advertisements
Similar presentations
Weather. Meteorology Meteorology is the study of processes that govern the Earth’s atmosphere. Meteorology helps make weather predictions possible.
Advertisements

* 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 mass - large body of air that has similar temp. and moisture - move by prevailing winds and upper air currents Front - boundary between 2 different.
Air Masses & Fronts. Air Masses Objective: to identify the different types of air masses & where they originate from.
* The relative measure of the amount of water vapor in the air * Psychrometer – measures the humidity * Water vapor affects the density of the air. * Cold.
Air Masses.
Air Masses & Fronts Chapter 17 Section 1 Pages Chapter 17 Section 1 Pages
What Causes Our Daily Weather To Change? Change in our weather is a result of a change in air masses.
Weather Chapter 21 1.
Air Masses and Fronts.
Air Masses and Fronts.
Air Masses and Fronts. An air mass is a large volume of air in the troposphere with similar characteristics of temperature, pressure and moisture as the.
Air Masses cont.  A large body of air with the same temperature and moisture content  When air is stationary or moves slowly it takes on uniform characteristics.
Air Masses & Fronts.
Air Masses  Areas of air that have about the same density, temperature, humidity, and pressure.  Cold air masses usually move south towards the equator.
What is an Air Mass?  Air masses are large bodies of air which have similar temperature and moisture characteristics.  Air masses form when air stays.
AIR MASSES AND FRONTS. AIR MASSES A section of air that has similar characteristics (temperature, weather, humidity, etc.) throughout it from the area.
Air Masses & Fronts.
Weather Patterns and Maps
©Mark Place, Air Masses.
Sit somewhere Pick up a weather sheet and complete.
Weather Fronts and Storms
Air Masses and Weather Video
AIR MASSES AND FRONTS Chapter 16 Section 2.
Air Masses and Fronts Page
Chapter 20: Air Masses, Fronts, and Instruments
Chapter 2 UNDERSTANDING WEATHER
AIR MASSES AND FRONTS Chapter 16 Section 2.
Air Masses, Fronts.
24-1 Air Masses.
Weather Part II Revised 2010 Revised 2010 ©Mark Place,
Air Masses and Fronts.
AIR MASSES AND FRONTS Chapter 16 Section 2.
Journal #46 What do the following symbols mean? c m P T
Air Masses - Jet Stream - Pressure Systems
©Mark Place, Air Masses.
AIR MASSES AND FRONTS Chapter 16 Section 2.
AIR MASSES AND FRONTS Chapter 16 Section 2.
AIR MASSES AND FRONTS Chapter 16 Section 2.
Air Masses and Fronts.
Air masses and fronts 1. An air mass is a wide-spread section of the troposphere with uniform temperature and humidity (moisture) 2. The source region.
Air Masses Chapter 21 Section 1.
AIR MASSES AND FRONTS.
Air Masses, Fronts.
©Mark Place, Air Masses.
AIR MASSES Chapter 16 Section 2.
Unit 8 Lesson 4 Air Masses Identify the characteristics of different air masses Predict how air masses affect weather in the US.
Air Masses and Fronts.
AIR MASSES Air mass- a large body of air that has the same properties as the surface over which it develops. Global air masses.
Air Masses & Fronts Earth Science Mr. Cloud.
Air Masses and Fronts.
Warm Cold Moist Dry Air Masses A large body of air with similar
©Mark Place, Air Masses.
Air Masses and Fronts Notes Entry 25 11/28/18
AIR MASSES AND FRONTS.
Rapid movement Gradual movement
Air Masses, Fronts.
Air Masses and Fronts Page 21 Air mass
Air Masses and Fronts.
©Mark Place, Air Masses.
©Mark Place, Air Masses.
©Mark Place, Air Masses.
AIR MASSES Large parcel of air with the same characteristics of temperature and moisture throughout. Lower case “c” indicates a continental air mass. These.
Fronts and Air Masses By Brian Fontaine.
AIR MASSES AND FRONTS Chapter 16 Section 2.
Thanks to University or Minnesota
Fronts and Air Masses By Brian Fontaine.
Mrs. Wharton’s Science Class
Air Masses and Weather Fronts
Presentation transcript:

Weather Lesson Seven Air Masses and Fronts

AIR MASSES Large bodies of air in the troposphere with similar temperature, moisture and pressure characteristics. Forms over large areas called source regions. Air mass stays over an area for a while to pick up characteristics of that region.

AIR MASS SOURCE REGIONS 1. POLAR (P) - cool air from the north (Canada or Arctic). 2. TROPICAL (T) - warm air from the south. 3. CONTINENTAL (c) - air mass formed over land - DRY. 4. MARITIME (m) - air mass formed over water - MOIST.

m c P T cT - dry and warm cP - dry and cold mT - moist and warm mP - moist and cold

cA mP mP cP cT mT mT

FRONTS The boundary between two air mass. Little mixing of air occurs at fronts. Unstableness of fronts is the cause of precipitation. 4 types of fronts and they are . . .

COLD FRONT The boundary between an advancing air mass pushing a warmer air mass. Underlying cold air pushes warm up and over like a plow. A fast moving front. Symbol used on maps is

WARM FRONT The boundary between an advancing warm air mass on a retreating wedge of a cold air mass. Warm air rises up and over as its advances because it is less dense. A slow moving front. Symbol used on maps is

OCCLUDED FRONT Occurs when a cold front overtakes a warm front and pushes the warm air between them up off the ground. Symbol used on maps is

STATIONARY FRONT Boundary between two adjacent air masses of different characteristics remaining in approximately the same position. Symbol used on maps is

Symbols point in the direction the air mass is moving.

WAVE CYCLONE The typical pattern of storms (or low pressure systems) as they travel across the United States. Storms have a low pressure center with a wedge of a cold front and a warm front extending from the center.

L

STORM TRACKS Low pressure storms generally track (move) to the east (or northeast) across the United States. Due to the wind belt in which the United States is located.

WEATHER PREDICTION Weather prediction is based on probability. A few days predictions are more accurate and reliable than long term predictions. Computer analysis and satellite images have improved forecasting in recent years.