January History Great Flood of 1937 70% of Louisville was submerged 3.3 billion in damages Crest - 85.4 ft. (Flood Stage – 55 ft.) 15 inches of rain in.

Slides:



Advertisements
Similar presentations
What we now know: Difference between weather and climate.
Advertisements

Forecasting Weather
WEATHER Fronts and Mapping
Pressure systems, air masses & fronts
Prentice Hall EARTH SCIENCE
Weather, Winds, and Fronts
Weather vs. Climate “Weather tells you what to wear each day, but the climate helps you figure out what should be in your closet”
A cold front moving in brings stormy weather
Topic VI “Meteorology”
Why Do We Have Weather? An Introduction Take good notes! There will be a quiz at the end of this presentation.
Understanding Weather
Weather Maps Isolines- Lines which connect points
Chapter 16 – Understanding Weather
Study Guide Test 12/16 Topics Include: Relative Humidity Dew Point Cloud Formation Air Masses Fronts.
Introduction to Meteorology
Weather Patterns and Severe Storms Chapter 20
Air Masses and Fronts – II. Brief review An air mass is a large body of air whose properties of temperature and humidity are fairly similar in any horizontal.
Weather Patterns.
AMS Weather Studies Introduction to Atmospheric Science, 5th Edition
Chapter 20 Test Review Place these notes into your Meteorology Notebook.
What properties of air do we look at when we study weather? Temperature Wind Speed and Direction Humidity Air Pressure.
Study Notes for 3-2 TEST. 1 The type of weather associated with an incoming _____ pressure system would be cloudy, chance of ______. low storms.
Objectives: Identify two types of pressure systems. Identify two types of pressure systems. Identify and describe what causes weather patterns. Identify.
Air masses and Fronts.
Chapter 13 Section 3 Air Masses and Fronts.
What is weather? 1 Weather Factors
A weather instrument that measures the wind speed.
January History Great Flood of % of Louisville was submerged 3.3 billion in damages Crest was 85.4 feet and flood stage is only 55 feet. 15 inches.
Clouds and Humidity.
Chapter 1 Monitoring The Weather Weather Studies Introduction to Atmospheric Science American Meteorological Society Credit: This presentation was prepared.
United States Weather Maps. How to Read a Surface Map Surface maps depict the large-scale elements of the weather. These elements include high and low.
Guided Notes for Weather Systems
Chapter 5 Weather. 5.1 A. What is weather? The state of the atmosphere at a specific time and place.
Water and Weather Chapter Six: Weather and Climate 6.1 Introduction to Weather 6.2 Weather Patterns 6.3 Climates and Biomes.
Pressure, Fronts, air masses
Miss Nelson SCIENCE ~ CHAPTER 8 WEATHER. Air Masses and Fronts SECTION 3.
Weather State Objectives 4.c, 4.e, 4.h..
Weather
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 Patterns Air Mass: A large body of air that has properties similar to the part of Earth’s surface over which it develops. Air masses cover thousands.
FRONTS AND AIR MASSES (also the 6 important cloud types)
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.
ES 20.2 Weather Fronts Fronts. ES 20.2 Weather Fronts Formation of Fronts:  Recall that air masses have different temperatures and amounts of moisture,
“Weather Basics” Michael J Passow Kathleen Murphy AMS Teachers Workshop Austin, TX Jan 8, 2013.
End of Year – Science Study Guide Earth Systems and Structures.
Air Masses and Weather 17 Air Masses  Air Masses An air mass is an immense body of air that is characterized by similar temperatures and amounts of moisture.
Table of Contents 6.3 Masses and Their Movements Weather Patterns.
by Brent Rivenbark and Rosalind Byrd
Lesson 3: Air Masses. What is an Air Mass? Air masses are large areas of air with similar temperature, humidity, and pressure.
Clouds
Section 1.2 The Causes of Weather
Objectives 1) Describe the weather conditions associated with different types of fronts. 2) Describe the “life cycle” of a mid-latitude low.
Introduction to Weather Chapter 1. A basic understanding of weather and the atmosphere. TV, radio, newspapers, the internet and NOAA Weather Radio.
Introduction to Weather Chapter 1. High Pressure 1.Also called an anticyclone 2.Winds blow clockwise and away (diverge) from the center 3.Associated with.
Weather Fronts and Pressure Systems 7 th Grade Science Mr. Bombick.
State Objectives 4.c, 4.e, 4.h.. Discussion What are some ways in which weather affects your everyday life?
Key Concepts 1 Weather is the atmospheric conditions, along with short-term changes, of a certain place at a certain time. Variables used to describe weather.
Water in the Air Chapter 3 Section 1 pg. 76 The Water Cycle  The continuous movement of water from sources on Earth’s surface—such as lakes, oceans,
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.
AMS Weather Studies Introduction to Atmospheric Science, 4th Edition
January History Great Flood of % of Louisville was submerged
Air Masses and Fronts.
AMS Weather Studies Introduction to Atmospheric Science, 4th Edition
Warm-up What is weather?.
Water and Weather. Water and Weather Chapter Six: Weather and Climate 6.1 Introduction to Weather 6.2 Weather Patterns 6.3 Climates and Biomes.
2006 Prentice Hall Science Explorer-Earth Science
Chapter 5 Weather.
Monitoring the Weather
January History Great Flood of 1937
Presentation transcript:

January History Great Flood of % of Louisville was submerged 3.3 billion in damages Crest ft. (Flood Stage – 55 ft.) 15 inches of rain in 12 days

Chapter 1: Monitoring the Weather (Basics) One of the Deepest Extratropical Cyclones Ever Recorded

Difference between Weather and Climate Weather is the state of the atmosphere at some place and time – Described with quantitative variables Temperature, humidity, cloudiness, precipitation, wind speed, wind direction – Meteorology is the study of the atmosphere and the processes that cause weather Climate is weather conditions at some locality averaged over a specified time period – Climate is an average of the weather, figured over the last 30- years and updated every decade – A locale’s climate also includes weather extremes

Look at Climatological Information

Sources of Weather Information Television – The Weather Channel and local newscasts Radio – NOAA Weather Radio Continuous broadcasts repeated every minutes Interrupted with warnings and watches The Internet (Ag Weather) What about now? Survey of Farmers at the 2013 National Farm Machinery Show

Retrieving Weather Information & Maps Weather info received via TV, radio, or the Internet includes – Weather maps National Regional – Satellite/radar images – Data on current/past conditions – Weather forecasts Short-term – 24 – 48 hours Long-term – Up to 7 days or longer

Two Types of Pressure Systems High Pressure Systems, or “Anticyclones” Low Pressure Systems, or “Cyclones”

Pressure Systems Cont. High and low refer to air pressure – High pressure area is relatively high compared to surrounding air – Low pressure area is relatively low compared to surrounding air Highs – Fair weather – Clockwise rotation of sinking air (in Northern Hemisphere) – Generally track toward the east and southeast Lows – Stormy weather – Counterclockwise rotation of rising air (in Northern Hemisphere) – Generally track toward the east and northeast – Lows tracking across the northern U.S. or southern Canada produce less moisture than lows tracking across the southern U.S. – Weather to the west and north – usually cold – Weather to the south and east – usually warm

Pressure Systems Cont. (High and Low Pressure Centers) Arrows indicate surface horizontal winds

Pressure Systems Cont. (What’s the weather like?) 1. Tallahassee, FL 2. Greenville, NC 3. Duluth, MN 4. Scranton, PA Wind Direction? Cloudy/Wet, Clear/Dry?

Air Masses Huge volume of air covering thousands of square kilometers Horizontally relatively uniform in characteristics – Temperature – Humidity Gathers characteristics from its source region – Cold, dry air masses form at higher latitudes over continents – Cold, humid air masses form at higher latitudes over maritime surfaces – Warm, dry air masses form over continents in subtropical regions – Warm, humid air masses form near the equator or in the subtropics over maritime surfaces

Air Masses Across North America Old Saying in the Ohio Valley: “Don’t like the weather today? It will change tomorrow!”

Fronts “Transition Zones between Air Masses” Warm Air Rising Warm Front Cold Front

Fronts – Boundary Between Air Masses 1.Cold Front a.Generally, a narrow band of precipitation along or just ahead of the surface front, where precipitation is brief (couple of minutes to a few hours) b.Precipitation can be severe c.Boundary between advancing cold air and retreating warm air d.Plotted on a map as a blue line with triangles pointed in the direction of motion e.Sharp Temperature Change

Fronts – Boundary Between Air Masses 2. Warm Front a.Generally, a wide band of precipitation along or just ahead of the surface warm front, where precipitation can be persistent (12-24 hours) b.Precipitation is generally light to moderate c.Boundary between advancing warm air and retreating cold air d.Plotted on a map as a red line with semi-circles pointed in the direction of motion

Fronts – Boundary Between Air Masses Right - A cyclone with the warm and cold fronts extending outward from the low pressure center. Showers generally form along the warm front, while more severe weather can occur along the cold front. Left - Shows how the warm and cold fronts act as boundaries between different air masses. Notice how the wind directions are different on either side of the fronts, and that the flow is counterclockwise and convergent.

Ways to Locate a Front on a Surface Weather Map 1.Precipitation 2.Cloud Cover 3.Wind Shift 4.Temperature Difference 5.Dew Point Difference

Other Types of Frontal Boundaries 1.Stationary – a non-moving front where winds on either side blow in opposite directions. Can become a cold or warm front based on advection. 2. Occluded – when the air behind the cold front overtakes the air ahead of the warm front

Characteristics of Air Masses & Fronts Wind directions are different on the two sides of a front Some fronts have no clouds or precipitation. Passage indicated by wind shift, and temperature/humidity changes In summer, temperature can be nearly the same on both sides of a cold front Difference will be humidity Fronts are anchored to lows on a weather map. Counterclockwise flow brings contrasting air masses together to form fronts Thunderstorms/severe weather often occur in the warm, humid air mass located between the cold and warm front

Describing the State of the Atmosphere What do Forecasters Tell Us? Maximum Temperature – Usually occurs in early to mid-afternoon Minimum temperature – Usually occurs around sunrise Dewpoint (frost point) – The temperature at which air must be cooled at constant pressure to become saturated with water vapor and for dew (or frost) to form Relative humidity – A percentage; the ratio of the actual concentration of the water vapor component of air compared to the concentration the air would have if saturated with water vapor Relative humidity will change throughout the day as the temperature varies Generally highest around sunrise and lowest when warmest Precipitation amounts – General rule – 10” of snow = 1” of precipitation

Example: What do forecasters tell us? Dew Point Temp FHuman PerceptionR. Humidity 75 +Extremely uncomfortable, oppressive62% 70-74Very Humid, quite uncomfortable52-60% 65-69Somewhat uncomfortable for most people44-52% 60-64OK for most37-46% 55-59Comfortable31-41% 50-54Very comfortable31-37% 49 or lowerFeels like the western US30% Livestock Cold Stress? None Danger Emergency

Describing the State of the Atmosphere Cont. What do Forecasters Tell Us? Air Pressure – And its tendency (rising or falling) – Falling may indicate approaching cold front Wind direction and speed – Wind direction is the direction wind is blowing from Example; a west wind is blowing from the west, toward the east Sky cover – Fraction of the sky covered in clouds NWS Weather watch – issued when hazardous weather is considered possible NWS Weather warning – issued when hazardous weather is imminent or actually taking place

Weather Satellite Imagery Two major types of satellite orbits – Geostationary High orbits – 36,000 km (22,300 miles) high Orbits planet at same rate as Earth’s rotation and in same eastward direction Currently 2 of these provide a complete view of much of N. America and adjacent oceans to latitudes of about 60 degrees – Positioned over equator at 75 0 W longitude, W longitude – Low angle in polar regions – Polar orbiting Low orbits – km (~ miles) high (Much more detailed info) Provides overlapping north-south strips of images Passes over the same point twice every 24 hours

Orbits of Each Type of Satellite Geostationary Satellite Polar Orbiting Satellite

Weather Satellite Imagery Visible Black and white photograph of the planet Only available during daylight hours Highly reflective surfaces appear bright white and less reflective surfaces are darker

Weather Satellite Imagery Infrared Available anytime, not just during daylight Provides temperature comparison of features within image Whiter = colder Higher cloud tops appear whiter, because they are colder

Weather Satellite Imagery Water vapor imagery Enables tracking of plumes of moisture Shades of white = increasing moisture Upper-level clouds appear milky to bright white

Weather Radar Complements satellite surveillance Doppler radar detects movement Excellent tool to forecast tornadoes

Sky Watching You can determine much about the weather by watching the sky Clouds are aggregates of tiny water droplets, ice crystals, or some combination of both – A cloud in contact with the ground is fog – Cloud forms: Stratiform clouds are sheet-like clouds formed in horizontal layers – Form where air ascends gradually over a broad region Cumuliform clouds are puffy, like cotton balls – More vigorous ascent of air over a smaller area – Under the right conditions can build vertically into a cumulonimbus (thunderstorm) cloud The appearance of high, wispy, feather-like clouds (composed of ice) in the western sky is often the first sign of an approaching warm front

Cloud Forms These high thin cirrus clouds appear fibrous because they are composed of mostly tiny ice crystals

Cloud Forms These relatively low clouds are composed of tiny water droplets and have more sharply defined edges than ice-crystal clouds

Clouds Forms Fog, stratus clouds in contact with the ground, reduces visibility

Cloud Forms Fair weather cumulus clouds are most common during the warmest time of day and then vaporize after sunset

Cloud Forms Clouds of vertical development – Merging and vertically-growing cumulus clouds Can become Cumulonimbus clouds – Nimbo, nimbus prefix or suffix = rain producing – These clouds always produce lightning and sometimes heavy rain, hail, or strong and gusty surface winds

Cloud Forms Clouds may move in different directions at different altitudes – Indicates horizontal wind shifts with altitude

Understanding UTC Time Weather observations are taken across the world based on a standard time. In doing so, a 24 hour clock is used, similar to military time. UTC (Coordinated Universal Time or Universal Time Coordinated) Also called “Z Time” To get local time in the United States, you have to subtract a certain number of hours based on time zone. Daylight Savings Time does make a difference

Understanding UTC Time UTC Time = 1200 UTC Daylight Savings Time? (Not until March 8 th ) No -5 Hours for EST = 7 AM 18 UTC = 18Z = ? 00 UTC = 0Z = ? 06 UTC = 6Z = ?