basic weather concepts part one lifelong learning ... · specific objectives • atmosphere:...
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Weather Weather BASIC WEATHER CONCEPTS
PART ONE LIFELONG LEARNING INSTITUTE
OCTOBER 24, 2019
COURSE INSTRUCTOR
NORM SCHROEDER
Home: 920-497-2363
Cell: 920-366-0001
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Weather
S/V Valhalla
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FUTURE LLI WEATHER COURSES
• Spring 2020 LLI Feb. 20, 2020
– Water, Humidity, Fog, Atmospheric Stability,
Clouds, Precipitation
• Future Classes to cover these topics
– Thunderstorms, Tornadoes, Lightning, Optical
Effects
– Mid-latitude weather and storms
– Tropical Weather and Storms, Hurricanes
– Weather forecasting processes and resources
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Weather
NWS WEATHER BALLOON LAUNCH
• DATE: WEDNESDAY OCTOBER 30, 2019
• TIME: 2400 GMT (6 pm DST). Be at NWS Office at 5:45 pm.
• LOCATION: NATIONAL WEATHER SERVICE OFFICE
• 2485 SOUTH POINT ROAD
• GREEN BAY, WI
• The NWS Weather Office is immediately across the street from Austin Straubel Airport. Park in the visitor parking lot and enter building front entrance. The Balloon Launch will take place outdoors, rain or shine, and this will be followed by a tour of the NWS facilities.
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Credit Where Credit Is Due
• CREDITS TO THE UNITED STATES
POWER SQUADRON NOW KNOWN AS
AMERICA’S BOATING CLUB
• 8 week course of Weather with an
accompanying textbook.
• Modified extensively by me with added
videos, additional materials and removal
of slides related to boating more
appropriate for the LLI Audience
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Weather
Chapter 1 General Objectives
• Understand the Sun is the source of all weather in the Earth
• Understand heat energy and how it is transferred.
• Know that insolation heats the Earth’s surface unevenly, creating different air masses.
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Weather
Chapter 1 Specific Objectives
• Atmosphere: Temperature and Heat • This course focuses on the weather that exists in the lowest level of the atmosphere. • The first chapter, however, begins with a big picture look at the entire atmosphere – the
mixture of gases that surround the Earth.
• Be familiar with the atmospheric layers.
• Recognize lapse rates and inversions.
• Appreciate the importance of water vapor in the air.
• Understand the difference between temperature and heat.
• Convert the Fahrenheit and Celsius Scales.
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Weather
Origins of Meteorology • Aristotle 340 BC wrote Meteorlogica a natural philosophy text
summarizing what was known about weather and climate
• Meteoros-meaning “high in the air”
• Milestones in development of meteorology as a genuine natural science: – Invention of hygrometer in 1400s measures humidity
– Invention of thermometer 1500s measures temperature
– Invention of telegraph, allowed real time transmission of weather observations
– 1920s Norwegian scientists postulate air masses and weather fronts
– 1940’s daily upper air weather balloon observations of temp., pressure, humidity----3 dimensional view of weather
– Other Developments: weather satellites, numerical (computational) weather forecasting, the internet allows widespread distribution of weather forecasting, etc. etc.
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Weather
Weather and Climate
• Weather – State of atmosphere at any given time and place
• Climate – Average weather over a period of years,
usually decades, in same place
• Atmospheric Science – Study of weather and climate (meteorology)
• Climate is what we expect, Weather is what we get!
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Weather
What causes “Weather?”
•The source of all weather on Earth is
unequal heating of the Earth’s surface by the
Sun. 10
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Weather
11
What Causes Weather?
• It’s all about the sun – Heat from the sun is absorbed:
• by the air • by the water • by the land
• and, Water vapor…
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Weather
12
Heating happens unevenly
– Absorption of Heat differs with air, ice, water, and land
– Amount of heating at the poles is far lower than at the equator
– This causes differing temperatures
– This, in turn, causes air to migrate
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Weather
13
Heating at Poles & Equator
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Weather
Events in Layers of the Atmosphere
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Courtesy NOAA
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Weather
17 Courtesy NOAA
Lapse
Rate
Chart
of the
Atmosphere
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Weather
Courtesy NASA
Composition of Air
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Weather
Water Vapor
• Water exists in the atmosphere in three different states: – a solid (e.g. ice crystals);
– a liquid (e.g. water droplets); and
– a gas - water vapor.
• The amount of water vapor in the air varies from about 1% (very dry) to 4% (very moist).
• Water vapor is the source of: – clouds and precipitation;
– an absorber and transporter of heat;
– a source of energy for powering storms.
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Weather
Temperature
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Molecules
move
slower
In cold air
Mercury
doesn’t
rise
COLD WARM
More kinetic
energy
Less kinetic
energy
Molecules
move rapidly
in warm air
causing
mercury
to rise
© 1992, USA Today. Reprinted with permission
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Weather
Temperature Scales
21
D
water boils
ice melts 0
°
32
°
100
°
212°
Degrees
Farhenheit Degrees
Celsius
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Weather
Temperature Conversion
• Temperature Conversion Equations:
• These are the equations for converting temperatures from one scale to the other.
– ° F = ( °C x 9/5 ) + 32
– ° C = ( °F - 32 ) x 5/9
• The 32 accounts for Fahrenheit freezing being 320 higher than Celsius freezing.
• The fractions – 9/5 and 5/9 – account for there being 180 degrees between freezing and boiling on the Fahrenheit scale but only 100 degrees on the Celsius scale.
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Weather
Temperature and Heat • Temperature is the measure of the average
kinetic energy of molecules in an object
• Thermal energy is the total kinetic energy of molecules in an object
• Heat is the thermal energy being transferred from one object to another
• Heat always flows from the the hotter object to the colder one
• Heat is what we FEEL, Temperature is what we MEASURE
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Weather
Mechanisms for Heat Transfer
• CONDUCTION: transfer of heat by molecular activity from one substance to another. ALWAYS from hotter to colder.
• CONVECTION: transfer of heat by actual movement of fluids (liquids and gases). In Meteorology vertical movement of heat.
• ADVECTION: is horizontal movement of heat.
• RADIATION: transfer of heat, light, other kinds of electromagnetic waves through space.
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Weather
© 1992, USA Today. Reprinted with permission
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Weather
Heat Transfer - Conduction
26
Heat flows through the medium from the action of molecules.
Hot
Spoon
Hot
Liquid
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Weather
Heat Transfer - Convection
27
• transfer of heat by actual
movement of heated material - meteorologists use “convection”
referring to up and down motions
of air and “advection” to describe
the horizontal movement of air
As water in the bottom of the pan heats up, it rises.
If the water gets hot enough, some of it also vaporizes forming bubbles that rise.
Cooler water sinks from the top to replace the rising water and bubbles.
This up and down movement eventually heats all the water.
© 1992, USA Today. Reprinted with permission
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Weather
Heat Transfer - Convection
28
Heat makes fluid medium circulate and carry heat along with it.
Heat Source
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Weather
Heat Transfer - Radiation
29
• transfer of heat by wave motion
- heat, light and other
kinds of waves radiate
through the near
vacuum of outer space
from the sun to the
Earth
Even though air conducts very
little heat, you can feel the heat
coming from the hot stove and the
pan. It’s radiating through the air.
© 1992, USA Today. Reprinted with permission
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Weather
Heat Transfer - Radiation
30
Energy waves move through space without a medium.
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Weather
Specific Heat
• Specific Heat is the measure of the amount of heat it takes to change the temperature of a substance.
– number of calories it takes to warm 1 gram of a substance 10 C
– the specific heat of water is 1 (1cal/g/0C) (by Definition)
• Land has a lower specific heat than water thus, Land warms up and cools off more quickly than bodies of water. Water “retains heat” longer than land.
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Weather
Specific Heats of Common Materials
• Dry Air 0.24
• Dry Soil 0.19
• Wet Soil 0.35
• Aluminum 0.21
• Copper 0.09
• Iron 0.11
• Ice/Snow 0.50
• Water 1.00 (by Definition)
• Note the pattern: metals conduct heat readily and have a low specific heat. Water is a very poor conductor of heat and has a high specific heat. Air also is poor heat conductor.
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Weather
Insolation-Incoming Solar Radiation
33 © 1992, USA Today. Reprinted with permission
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Weather
Insolation can lead to unequal heating of Earth’s surface
34
IIncoming solar radiation
Sun’s Rays
Insolation is “INcoming SOLar radiATION”
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Weather
Insolation Varies with Latitude and also with Seasons
• In kW-hrs/m2/day
• 0 deg Latitude (Equator) = 10
• 60 deg Latitude = 5
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Weather
Reflected Solar Energy varies by type of material
36
© 1992, USA Today. Reprinted with
permission
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Weather
Earth’s Year Around Sun
37
Dec. 21
Sept. 21
June 21
March 21
© 1992, USA Today. Reprinted with permission
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Weather
Sun Angles
38 © 1992, USA Today. Reprinted with permission
Summer Solstice Spring or Fall Equinox Winter Solstice
June 21
longest day
March 21
September 21
day & night
almost equal
December 21
shortest day
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Weather
Air Masses-large body of air with permanent uniform horizontal temp and humidity
Temp---Humidity
cP Continental Polar cold - dry
mP Maritime Polar cool - moist
mT Maritime Tropical warm - wet
cT Continental Tropical hot - dry
A Arctic very cold
E Equatorial warm - moist
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Weather
Major Air Masses
41 Courtesy NOAA
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Weather
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Uneven temperatures
– Air rises over heated areas
• Leaves lower pressure behind
– Air falls over cooler areas
• Creates higher pressure
– Winds develop toward the lower pressure
– Wind moves weather
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Weather
Key Points to Remember about Heat and Pressure
• Heat: energy (heat) is always transferred from WARM to COLD
• Pressure: pressure always flows from HIGH to LOW
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Weather
48
Regions of Cold and Warm
• Regions form Globally
– Cold Air Masses
– Warm Air Masses
• Weather systems form along the boundaries (fronts)
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Weather
Air Masses
49
© 1992, USA Today. Reprinted with permission
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Weather
Air Masses at Boundary A FRONT is the boundary between two air
masses
50
© 1992, USA Today. Reprinted with permission
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Weather
Lapse Rate: the rate at which atmospheric temp decreases with
increased altitude
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Weather
Ocean Surface Currents
54 © 1992, USA Today. Reprinted with permission
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Weather
Chapter 1 Summary pg 1.
• Temperature generally decreases as altitude increases throughout the lower atmosphere.
• Temperature is a measure of relative hotness or coldness and is a very important factor in weather.
• The equations for converting Fahrenheit and Celsius degrees.
• Heat is energy transferred from a warmer to a cooler body.
• Heat is transferred in three ways: conduction, convection, and radiation.
• The term lapse rate is the observed temperature change as altitude changes in the atmosphere.
• Inversions are important factors in determining atmospheric conditions often contributing to haze and smog.
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Weather
Chapter 1 Summary pg.2
• Most weather phenomena result from uneven heating of the Earth’s surface and the circulatory processes that transport heat.
• Air masses that remain stationary for a period of time take on the properties of the surface below them (hot or cold; dry or moist).
• Heat is transferred vertically by convection and horizontally by advection as the winds push different air masses.
• The ocean currents and global winds transport heat from the tropics towards the poles.
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Weather
END of CHAPTER 1
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