slide1 l.
Download
Skip this Video
Loading SlideShow in 5 Seconds..
Chapter 14 – The Atmosphere PowerPoint Presentation
Download Presentation
Chapter 14 – The Atmosphere

Loading in 2 Seconds...

play fullscreen
1 / 65

Chapter 14 – The Atmosphere - PowerPoint PPT Presentation


  • 404 Views
  • Uploaded on

Chapter 14 – The Atmosphere The modern atmosphere Two most abundant gases: 78% N 2 21% O 2 Less abundant gases (< 1%) Argon Water vapor CO 2 (only about .035%) Non-gaseous components water droplets dust, pollen, soot and other particulates Fig. 17.6, p.437

loader
I am the owner, or an agent authorized to act on behalf of the owner, of the copyrighted work described.
capcha
Download Presentation

PowerPoint Slideshow about 'Chapter 14 – The Atmosphere' - issac


An Image/Link below is provided (as is) to download presentation

Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author.While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server.


- - - - - - - - - - - - - - - - - - - - - - - - - - E N D - - - - - - - - - - - - - - - - - - - - - - - - - -
Presentation Transcript
the modern atmosphere
The modern atmosphere
  • Two most abundant gases:
    • 78% N2
    • 21% O2
  • Less abundant gases (< 1%)
    • Argon
    • Water vapor
    • CO2 (only about .035%)
  • Non-gaseous components
    • water droplets
    • dust, pollen, soot and other particulates
thermal structure of atmosphere lower layer
Thermal Structure of Atmosphere: Lower Layer
  • Troposphere –
    • to about 12 km (40,000 ft) elevation
    • All clouds & water vapor and most weather
    • Temperature decreases as elevation increases, because chief source of heat is radiated heat from the earth’s surface
    • Environmental Lapse rate: 6.4°C/1000m
thermal structure of atmosphere upper layers
Thermal Structure of Atmosphere: Upper Layers
  • Stratosphere – heated primarily by solar radiation
    • Ozone (O3) layer absorbs UV energy, causing temperatures to rise
    • Above 55km (stratopause) temps fall again
  • Mesosphere – thin air (can’t absorb energy), very cold up to 80km
  • Thermosphere – above 80km, temps rise rapidly (to just below freezing!)
latent heat
Latent Heat
  • Sometimes heat transfer causes a change of state – change from solid to liquid, or liquid to gas. This occurs without a change in temperature. Examples:
    • Water stores energy when it changes from a liquid to a gas, since it absorbs the energy, but does not change temperature.
    • Water releases energy when it changes from a gas to a liquid. This is the source of wind energy found in hurricanes.
latent heat7
Latent Heat
  • Latent heat – energy stored or released during a phase change without temperature change
humidity
Humidity

H2O in air exists in 2 forms: vapor (invisible) and liquid e.g. rain, fog, clouds.

Saturation: Maximum quantity H2O vapor that air can hold. Additional H2O condenses into liquid water.

Saturation increases with temperature (hot air can hold more water vapor than cold air.

Conditions left of curve cause water vapor to condense.

relative humidity
Relative Humidity

Relative humidity (RH)- ratio of actual amount H2O vapor in air to the amount at saturation.

Often, as the days warms up, the air, more water will evaporate into the air (actual amount), but since the temperature has increased, so has the amount of water needed for saturation

Therefore, the RH stays about the same.

relative humidity10
Relative Humidity

What happens if the air now cools down?

Actual amount of water vapor in the air stays the same but amount needed for saturation decreases.

Therefore the RH increases.

relative humidity11
Relative Humidity

When the relative humidity reaches 100%, the air is saturated, regardless of actual amount of water vapor present.

At low temperatures, 100% RH means less water vapor than at higher temperatures.

dew point temperature
Dew Point Temperature

Dew point temperature – temperature at which RH = 100 %.

If saturated air cools below the dew point temperature, water vapor will condense into liquid.

At the dew point temperature, clouds, fog rain or dew appear.

solar energy insolation
Solar Energy (Insolation)
  • Also called solar radiation, although NOT radioactive!
  • Composed of electromagnetic waves with different properties depending on wavelength, frequency
    • Longwave (low frequency): includes heat (infrared), radio waves
    • Shortwave (high frequency): includes visible light as well as ultraviolet, x rays, gamma rays
    • Electromagnetic spectrum – shows EM wavelengths by frequency and wavelength
shortwave solar energy
Shortwave solar energy
  • The highest frequencies (xrays, gamma rays) are absorbed by oxygen atoms in the thermosphere and O2 gas in the mesosphere.
  • Ultraviolet (uv) absorbed by the ozone in the stratosphere.
  • Visible light waves (still considered shortwave) pass through and are absorbed by earth.
ozone high and low
Ozone high and low

The ozone layer in the stratosphere is a good thing because it protects life on Earth from harmful UV rays

The Ozone in the troposphere is a bad thing because it damages hearts and lungs.

depletion of the ozone layer
Depletion of the ozone layer

Ozone – O3 forms in the stratosphere and absorbs UV energy, which can be harmful

Halons and Chlorofluorocarbons (CFCs), – are organic compounds that destroy ozone in the ozone layer

depletion of the ozone layer19
Depletion of the ozone layer

Ozone hole – reported in 1985 and linked to CFCs in Antarctic ice clouds

Many nations of the world agreed to reduce or stop use of these CFCs and halons

Most industrial countries no longer produce CFCs.

Since banning CFCs, the hole may be decreasing

absorption and emission
Absorption and Emission
  • Absorption of radiation – electrons of absorbing material are “excited” by increase in energy
    • Increase in temperature; physical/chemical change
    • Examples: sunburn, cancer
  • Emission of radiation – excited electrons return to original state; radiation emitted as light or heat
    • Example: earth emits radiation in the form of heat after absorption of solar energy (light)
reflection and albedo
Reflection and Albedo
  • Reflection–electromagnetic radiation bouncing of from a surface without absorption or emission, no change in
    • material
    • energy wavelength
  • Albedo – proportional reflectance of a surface
    • a perfect mirror would have an albedo of 100%
    • Glaciers & snowfields approach 80-90%
    • Clouds – 50-55%
    • Pavement and some buildings – only 10-15%
    • Ocean only 5%! Water absorbs energy.
the radiation balance
the Radiation Balance
  • Sun emits EM radiation of all wavelengths, but primarily shortwave (i.e. light).
    • Earth’s surface absorbs this energy
    • Most is re-emitted upward, as heat (longwave)
  • Greenhouse Effect and Counterradiation
    • “greenhouse gases” (water vapor, carbon dioxide, methane) let shortwave energy pass, but absorb and longwave energy radiated upward by the Earth.
    • this longwave energy is re-radiated in all directions, some of it returning to the Earth’s surface.
cloud formation
Cloud Formation

Clouds – made of water droplets and/or ice particles (not water vapor, which is invisible)

Cloud particles grow around a tiny solid surface; these are called condensation nuclei (singular nucleus).

Examples include dust, smoke, pollen, sea salt pollutant particulates.

cloud formation27
Cloud Formation

clouds form when the air is saturated (100% relative humidity) and H20 vapor condenses.

air must cooled to dew point for saturation to occur.

Large scale cooling occurs when an air mass is lifted to a higher level in the atmosphere, due to the Adiabatic Principle.

slide28
When a gas expands, it’s temperature decreases.

When a gas is compressed, it’s temperature increases.

The adiabatic process refers to a temperature change caused by a change in pressure.

The Adiabatic Process

slide29
Adiabatic (expansional) cooling – occurs when rising air expands due to decrease in air pressure.

Adiabatic (compressional) warming - sinking air compresses, due to increase in air pressure.

slide31
For clouds to form by adiabatic cooling, the air mass must rise to where the air pressure is less; then it can expand

The Adiabatic Process

what makes air rise
What makes air rise?

Warm air is less dense (lighter) than cool air.

Water vapor is less dense (lighter) than dry air.

Air near earth’s surface warms, picks up water vapor from near the surface of the Earth, then rises.

Adiabatic cooling lowers temperature to dew point, which causes cloud formation.

Air may be “helped” to rise by various means.

slide33

Adiabatic Lapse Rates

Dry: 10°C/1000m Wet: approx 5°C/ 1000m

<--- lifting condensation level

clouds
Clouds

Cloud families – based on height

  • Low: to 10,000 ft above the surface
  • Middle: 10,000-20,000 ft above the surface (prefix alto)
  • High – above 20,000 ft high (prefix cirro)
  • Clouds with vertical development

Cloud classes - based on shape

  • stratiform – layered clouds
  • cumuliform - globular
cirrus high altitude clouds
Cirrus – high altitude clouds

Formed from ice crystals, not liquid water drops.

Strong winds at altitude blow them into wisps (“mare’s tails”).

No rain (or snow) comes directly from them, but they are often an indication of unsettled weather in the near future.

low stratus clouds
Low Stratus Clouds

Horizontally layered, sheet-like clouds.

Form in relatively stable conditions when air stops rising as soon as condensation occurs.

Causes a gray overcast sky that may persist for days.

Nimbostratus clouds bring steady rain or snowfall (nimbo = rain).

cumulus clouds display vertical development
Cumulus clouds display vertical development

Fluffy, white clouds with flat bottoms and billowy tops that may rise as much as 4 miles up in the air.

Form from relatively unstable air which continues to rise after condensation takes place. Flat base of cloud is where condensation started.

Rain or snow comes in the form of brief, intense showers.

other cumulus clouds
Other Cumulus Clouds

Fair weather cumulus

Cumulonimbus

slide41

Lenticular clouds form as moist air flows up and over a mountain peak. They are classified as altocumulus. Lenticular clouds indicate high winds aloft.

slide42
Fog

Fog is a cloud that forms at or very close to the ground. The picture shows an example of radiation fog, from air near the earth’s surface which cooled by radiation during the night. Fog usually disappears during the day, when the sun warms the earth and it begins to emit heat.

san diego marine layer
San Diego Marine Layer

The marine layer is an example of an advection fog: warm air over the ocean takes in water layer, but as prevailing west winds blow it over the land, the water vapor condenses

precipitation
Precipitation
  • Clouds sometimes release moisture as precipitation
    • Occurs as rain, hail, snow or sleet
    • 3 mechanisms that cause air to rise, leading to cloud formation and precipitation
      • Orographic precipitation
      • Cyclonic precipitation
      • Convection-Convergence precipitation
orographic precipitation
Orographic Precipitation

Prevailing winds push air up against, and then over, a mountain range

This process is responsible for our deserts in eastern San Diego County

rainfall map
Rainfall Map

Orographic precipitation occurs on west side as air is lifted over mountains.

Great Central Valley has less rain than coastal regions.

Death Valley and Mojave Deserts are rainshadow deserts.

cyclonic precipitation frontal wedging
Cyclonic Precipitation (Frontal Wedging)

When moving warm and cold air masses meet (a “front”), more dense cold air forces the less dense warm air to rise.

This happens when a storm (cyclone) passes through

convection convergence precipitation
Convection-Convergence Precipitation
  • Forms when warm, moist air
    • Heats up near a hot surface
    • Rises and cools adiabatically
    • Condenses and forms clouds
    • May form fair weather cumulus
    • If conditions are unstable, can lead to precipitation in the form of thunderstorms.
thunderstorms and unstable air
Thunderstorms and Unstable Air

Unstable air conditions caused by:

  • surface air that is very warm and moist
  • the environmental temperature lapse rate exceeds both dry and wet adiabatic rate (relatively cold, dry air aloft)
  • Rising air remains warmer than its surrounding air, causing strong, persistent convection (updrafts)
  • Clouds with intense vertical development – “towering cumulus”
  • Cumulonimbus clouds and thunderstorms
exploring thunderstorms
Exploring Thunderstorms
    • Vertically developing clouds
    • Reach very high altitude
    • Are affected by high velocity winds
    • Become anvil-headed
  • Strong convective flows
    • Are created by precipitation dragging cool air down
    • And warm rising air taking its place
  • Hail and lightning are destructive by-products of thunderstorms
the force exerted by the atmosphere
The force exerted by the atmosphere
  • Gas molecules in the atmosphere bounce randomly, creating force in all directions.
  • In addition, the force of gravity causes atmospheric gas molecules to concentrate at lower elevations. More force (in all directions) at lower elevations.
barometric pressure force exerted by the gas molecules in the atmosphere over a given area
Barometric Pressure - force exerted by the gas molecules in the atmosphere over a given area
  • English unit is pound per square inch (psi). At sea level, the atmosphere exerts about 14 pounds of force on a one by one inch area (slightly bigger than a postage stamp).
  • How many postage stamps fit on the top of your head?
  • How many pounds of force does the atmosphere exert on the top of your head?
  • Why don’t you have a big headache right now?
barometric pressure
Barometric pressure
  • At 5 km (about 3 miles) of elevation, there are only half the gas molecules above you that there are at sea level.
  • Now your headache is due to altitude sickness!
measuring barometric pressure
Measuring barometric pressure
  • If you evacuate a tube (i.e. remove all the air) and put it in a dish of liquid, the liquid will fill the tube as the air pressure pushes on the liquid in the dish.
  • If you tried this with a dish of water, the water would rise up to about 33 feet in the tube!
measuring barometric pressure58
Measuring barometric pressure
  • Using mercury, a very heavy liquid, we find that at normal sea-level barometric pressure, the liquid in the tube rises to a height of 760 mm (or 29.92 inches).
  • This apparatus is the original form of the barometer, a device used for measuring barometric pressure.
measuring barometric pressure59
Measuring barometric pressure
  • What is a normal barometric pressure in the units reported by the TV news weatherman?
  • Hint: the units are not psi, and not millimeters
answer
Answer
  • In the U.S., Mr. TV Weatherman reports barometric pressure in inches, with normal ranging from 29-31 inches (listen for it tonight).
  • Overseas, Mr. TV weatherman probably announces the barometric pressure in Millibars (1013 millibars = normal sea level pressure)
  • Meteorologists routinely use millibars for scientific applications.
measuring barometric pressure the modern way
Measuring barometric pressure – the modern way
  • Mercury barometers are dangerous and difficult to use.
  • Modern aneroid barometers use changes within a partially evacuated chamber to move the pointer to the correct value.
slide62
This graph shows how the barometric pressure (x axis – in millibars) decreases as the elevation increases and the number of gas molecules above gets less and less.
acid rain
Acid Rain
  • Burning of coal and petroleum release sulfur and nitrogen oxide gases
  • In moist air, these gases form acids
  • Atmospheric acids dissolve in water droplets and fall as acid rain
  • The damage often occurs over 100 miles away
  • Acid rain damage in Ontario, Canada can be traced to coal-burning power plants along the Ohio River Valley
photochemical smog
Photochemical Smog
  • Incompletely burned gasoline reacts with nitrogen oxides and oxygen in the presence of sunlight to become ozone (O3).
  • Ozone reacts again with gasoline exhaust to become smog
ozone and smog
Ozone and smog
  • Irritates the lungs and aggravates asthma
  • Increases the liklihood of heart disease
  • A suspected carcinogen