Air masses/Atmospheric conditions

Slides:



Advertisements
Similar presentations
Weather Maps & Fronts Refers to the state of the atmosphere at a specific time and place. Influenced by pressure systems (high and low) and fronts. Describes.
Advertisements

Weather review! 2013.
Chapter 6 Study Guide Review Power Point.
Severe Weather Some Meteorology Basics. Atmospheric Heating  Atmosphere is heated from the bottom  Solar energy absorbed by the Earth is re- radiated.
Watch the video below. Describe your observations and possible causes of such events. /watch?v=SZcBlAjf2NE Activating Strategy:
Meteorology.
Air Masses and Fonts Chapter 8 Section 3.
Weather: The state of the atmosphere at a given time and place, with respect to variables such as temperature, moisture, wind velocity and direction,
Weather Patterns.
ATMOSPHERE Air Circulation
The Sun’s Effect on Weather. Contents The Sun’s Key Roles The Sun’s Key Roles n Effects on Earth’s weather n Moving Air: The Wind n Evaporation n Hurricanes.
Miss Nelson SCIENCE ~ CHAPTER 8 WEATHER. Air Masses and Fronts SECTION 3.
* 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.
Meteorology: Weather and Climate Hot, Cold, and Everything in between!
Weather Patterns (57) An air mass is a large body of air that has properties similar to the part of Earth’s surface over which it develops. Six major air.
Weather Variables and Forecasting Modified from National Weather Service
Chapter 6 Biogeography: Climate, Biomes, and Terrestrial Biodiversity.
Atmosphere. Atmosphere structure Tropopause Troposphere 20 km 40 km 10 mi 20 mi 30 mi Weather zone Water Vapor Dry Ozone Stratosphere Stratopause Mesosphere.
The Earth’s Atmosphere: Factors That Affect the Weather SOL 6.6.
Low Pressure Systems vs High Pressure Systems. Let’s Compare Low Pressure Systems (L) High Pressure Systems (H)
The Role of Solar Energy (continued)
Section 1.2 The Causes of Weather
Chapter 38 Weather.
UNIT 1: Weather Dynamics Chapter 1: Inquiring about Weather The Causes of Weather Chapter 2: Weather Forecasting.
Weather Patterns. Weather Changes Because of the movement of air and moisture in the atmosphere weather constantly changes.
Earth’s Atmosphere And Weather. Composition of the Atmosphere 78% nitrogen: little effect on weather 21% oxygen: component necessary for human life Argon:
Earth’s Atmosphere And Weather. Composition of the Atmosphere 78% Nitrogen 21% Oxygen 0.9% Argon 0.04% Carbon Dioxide Water Vapor 0 – 4% % Ozone.
Classwork Students will take turns reading a paragraph and another student will summarize for the group what was just read. After reading the section,
Atmospheric Pressure. What Is Weather? (continued) Humid air (air containing more water vapour) has lower pressure than dry air.  the more H 2 O vapour.
An air mass is a large body of air that has properties similar to the part of Earth’s surface over which it develops. Weather Changes—Air Masses Six major.
Weather and Climate Notes Part 6. Identify factors affecting seawater density and salinity. When water becomes colder and when it has a high salinity.
Weather: Temperature, winds, air masses, moisture, air pressure, and weather maps.
Unit 7 Meteorology 2014… Mrs. Knowlton. Weather describes the conditions in the atmosphere (mostly the troposphere the lowest layer of the atmosphere)
Chapter: The Atmosphere in Motion
III. Water and Climate.
Fronts Front The Boundary between two different air masses.
Activating Strategy:
UK Weather Systems Aim:
The Course of Synoptic Meteorology
Section 1.2 The Causes of Weather
Air Masses and Fronts.
Air Masses Air masses are large bodies of air where temperature and moisture content are constant throughout. Moisture content and temperature of a mass.
Mr. Foley presents Weather.
AICE EM: Atmosphere Key Content 2
What kind of weather would a continental tropical air mass that formed over northern Mexico bring to the southwestern U.S?
Weather.
Under Pressure As we know, the air in the atmosphere is made up of a number of gases. These gases press down on the Earth’s surface, exerting a force.
Science 10 Weather Dynamics
Weather Systems Outcome:
Weather: Chapter 14 Sec 14.1 Meteorology Meteorologist
Solar-Weather-Ocean Unit Notes
Weather.
AIR MASSES & FRONTS.
Weather and how it affects us….
Unit 4: Weather Dynamics
Air Masses and Weather Fronts
WEATHER Unit 1b.
WEATHER #1 flashcard answers
Unit 2 Lesson 1 Influences on Weather
Weather Vocabulary.
Chapter 5 Weather.
Weather The present state in the atmosphere at a given location for a short period of time.
Precipitation.
Air masses and Air fronts
Air Masses What are major air masses?
Air Masses and Severe Weather
16: Severe Weather Unit 6: Meteorology March 13, 2012 Sanders.
The Atmosphere.
Air Masses Air masses are large bodies of air where temperature and moisture content are constant throughout. Moisture content and temperature of a mass.
Presentation transcript:

Air masses/Atmospheric conditions

What is an air mass? -wikipedia. In meteorology, an air mass is a volume of air defined by its temperature and water vapor content. Air masses cover many hundreds or thousands of square miles, and adopt the characteristics of the surface below them -wikipedia.

What happens when air masses collide? From sciences360.com When two air masses collide, they tend to stay separate in the first instance, as oil remains separate from water. What happens when two masses collide relates to the differing characteristics of each mass.

In other words, warm air rises! Warm air is lighter than cool air, therefore when a mass of warm air meets a mass of cooler air, it tends to rise up over it. How quickly this rising takes place will be affected by the type of collision between the masses. In other words, warm air rises!

If a warm air mass collides with a cool or cold mass, it will ride gradually up and over it. The line which separates the warmer air from the cooler air is called a front and the front will rise from the ground at an angle with the warmer air above the cooler air. Normally, if it is warm air which approaches the cooler air the front will form a gentle angle and the warmer air will consequently rise gently upwards. However, if cooler air approaches and collides with warmer air, the heavy, denser cool air will tend to undercut the warmer air, pushing it rather like a bulldozer, forming a steeply rising front.

The name of each front is derived from the type of air which follows behind it at ground level. For example when warm air is approaching cool air, the passing of the front will presage a rise in temperature as an observer passes from the cool mass to the warm mass, and consequently this is a warm front, marked with red semi-circles on a weather map.

On the other hand, if cool air is approaching a warmer air mass the front will mark a fall in temperature and be called a cold front, marked with blue triangles on a weather map.

How clouds and rain form In each case, with warm air rising over cool air, the air will expand and cool as it rises. If the rising air contains a large amount of moisture, this moisture will tend to condense into water droplets when the temperature of the rising air reaches dew point. This is not a fixed temperature, but varies due to different meteorological characteristics. The formation of water droplets will cause clouds to develop, and if the clouds grow to a sufficient extent, rain will fall. In general terms, the faster the air rises, the taller will be the clouds, and the heavier will be the rain.

https://www.youtube.com/watch?v=ukZilXnSj6c

Atmospheric circulation The large-scale movement of air, and the means (together with the smaller ocean circulation) by which thermal energy is distributed on the surface of the Earth.

Factors that affect atmospheric circulation There are 5 major factors affecting global air circulation - uneven heating of earth's surface - seasonal changes in temperature and precipitation - rotating of earth on its axis - properties of air and water - long term variation in the amount of solar energy striking the earth

The coriolis effect

Anticyclones and depressions Most air masses move horizontally, however it is also possible that they move vertically. When air cools, the particles do not collide as frequently, and the pressure tends to fall. To compensate, the particles move together and the air density increases. The air mass thus becomes heavier and sinks toward the ground, compressing the particles beneath it and creating an area of HIGH PRESSURE, called an ANTICYCLONE.

Depressions when air warms, its density decreases, the air mass becomes lighter and rises, leaving an empty space beneath it. The space becomes an area of low pressure called a...

Cyclones. When strong depressions develop over over warm waters of tropical oceans, a huge spiral forms stretching as far as 800 km in diameter, inside the wind blows at speeds up to 360 km. These storms are called cyclones, hurricanes or typhoons.

How hurricanes are formed https://www.youtube.com/watch?v=7qym7b-qvkE