Weather Chp. 2

42
Weather Chp. 2

description

Weather Chp. 2. Energy of the Atmosphere Sun – 98% of the energy in Earth’s atmosphere comes from the sun in the form of electromagnetic waves. Radiation – is the direct transfer of energy by electromagnetic waves. -visible light most - infrared -ultraviolet. - PowerPoint PPT Presentation

Transcript of Weather Chp. 2

Page 1: Weather Chp. 2

Weather Chp. 2

Page 2: Weather Chp. 2

Energy of the Atmosphere

Sun – 98% of the energy in Earth’s atmosphere comes from the sun in the form of electromagnetic waves.

Radiation – is the direct transfer of energy by electromagnetic waves.

-visible light most- infrared-ultraviolet

Page 3: Weather Chp. 2

Blue sky – is the product of the reflection and scattering of light in all directions causing the short wavelengths of blue and violet to appear.

Dusk and Dawn – the scattering of longer wavelengths (red and orange) due to light traveling through more atmosphere.

Dusk/dawn

Mid-day

Page 4: Weather Chp. 2

Energy at the surface

1. Absorbed by earth2. Reflected back to atmosphere3. Absorbed by the clouds and gasses in atmo.

Green house effect – is when energy is absorbed by water vapor, CO2, methane, and other gasses in the air, causing a warm “blanket” to form in the atmosphere.

Page 5: Weather Chp. 2

TemperatureThermal energy – the total energy of motion in

the molecules of a substance.

Temperature – is the average amount of energy of motion of each molecule of a substance, thus the measure of how hot or cold a substance is.

Thermometer – a thin glass tube with a bulb on one end that contains a liquid (colored alcohol)

http://www.colorado.edu/physics/2000/waves_particles/wavpart2.html

Page 6: Weather Chp. 2

---- temp-----

when a liquid is heated up it will expand! This expansion is restricted to going only two directions in a thermometer, UP or Down! When it rises it indicates more energy in the liquid molecules and causing the liquid to expand up. When heat (energy) is lost the molecules will come closer together taking up less space and indicating a lower temp.

Page 7: Weather Chp. 2

Heat Transfer3 types

1. radiation – the direct transfer of energy by electromagnetic waves.

2. Conduction – the direct transfer of heat from one substance to another substance that it is touching.

3. Convection – The transfer of heat by the movement of a fluid.

Pg. 51

Page 8: Weather Chp. 2

radiation

Page 9: Weather Chp. 2
Page 10: Weather Chp. 2
Page 11: Weather Chp. 2

eyr

Page 12: Weather Chp. 2

Winds

Wind – is the horizontal movement of air from an area of high pressure to an area of lower pressure.

- pressure differences are caused byan unequal heating of the atmosph. - cold dense air sinks and warm air rises causing a movement of air

(wind)high pressure vs. low pressure.

Page 13: Weather Chp. 2

Anemometer – measures wind speed.Wind chill is the cooling of

warm blooded mammals do to heat loss from wind.

Wind direction – Named (west wind) by the direction is coming from. So, a west wind would be coming from the west and blowing toward the east.

Local wind – winds that blow over short distances. Ste. Gen to Cape or smaller, do to unequal heating of surface of Earth.

Page 14: Weather Chp. 2

Sea breeze – wind blowing inland from the sea.Earth heats up quicker less pressure than air over water

more pressure. Day time.Land breeze – wind blowing out to sea from the

land, due to opposite of sea breeze. Night time

Monsoons – sea and land breezes over a large region that change direction with the seasons.

Page 15: Weather Chp. 2
Page 16: Weather Chp. 2

Global winds – (created by unequal heating) winds that blow steadily from specific directions over long distances. The movement of air from the equator to the poles as a result of convection is a global wind. See pg 59.

Coriolis Effect – The way Earth’s rotation makes winds curve. http://ww2010.atmos.uiuc.edu/(Gh)/guides/mtr/fw/gifs/coriolis.mpg

Page 17: Weather Chp. 2
Page 18: Weather Chp. 2
Page 19: Weather Chp. 2

Jet stream – A high level stream of fast moving air. At altitudes of 6 miles high and at

speeds of 180km to 350km.

Page 20: Weather Chp. 2

El Nino

• El Nino - (El Nee-nyo) is the warming of water in the Pacific Ocean.

• Rain and flooding along the Pacific Coast• Warm water disrupts the food chain of fish,

birds, and sea mammals.• Tornadoes and thunderstorms in the

southern US• Fewer than normal hurricanes in the

Atlantic

Page 21: Weather Chp. 2

La Nina• La Nina - (Lah Nee-Nyah) is the cooling of

water in the Pacific Ocean. • Snow and rain on the west coast • Unusually cold weather in Alaska • Unusually warm weather in the rest of the USA • Drought in the southwest • Higher than normal number of hurricanes in the

Atlantic • http://esminfo.prenhall.com/science/

geoanimations/animations/26_NinoNina.html

Page 22: Weather Chp. 2

Water Cycle• Amount of water remains the same

as it moves through the cycle• Fresh water is limited• All living organisms need liquid water• Earth’s water is continually being

recycled

Page 23: Weather Chp. 2

Evaporation – process by which water molecules escape into the air by radiant energy from the sun changing water into a gas (water vapor).

Relative humidity – the percentage of moisture the air holds relative to the amount it could hold at a particular temperature.

Psychrometer – instrument used to measure the amount of R. humidity in the air. It consist of two thermometers, one wet and one dry.

Page 24: Weather Chp. 2

Cloud formation

Clouds form when water vapor in the air becomes liquid water or ice crystals. Water vapor changing into a liquid----CONDENSATION

The temperature at which condensation begins is called dew point.

Page 25: Weather Chp. 2

Cumulonimbus – Thunderstorm clouds that produce severe weather, tornadoes, hail, strong winds. Have anvil shape to top of cloud.

Page 26: Weather Chp. 2

CloudsCumulus – usually indicate fair weather. 2 to 7 miles in the sky (cotton balls).

Page 27: Weather Chp. 2

Cirrus – Feathery or fibrous in appearance. Very high altitudes usually between 6 and 12 kilometers. Indicate the onset of rain or snow in a few hours.

Page 28: Weather Chp. 2

Stratus clouds – smooth gray clouds that cover the whole sky and block out the sun are

called stratus clouds. These clouds produce steady, light precipitation.

Page 29: Weather Chp. 2

Precipitation – Water vapor that condenses and forms clouds that can fall to the Earth as rain, sleet, snow, freezing rain or hail.

sleet – water droplet that freezes when it falls through cold air. (winter)

snow – forms when water vapor changes directly to a solid.

Hail – ice balls that fall after water is frozen in the air then pushed further up and collects more water and freezes again, over and

over until it becomes to heavy to stay suspended in the air. The stronger the uplift the larger the hail stone. (summer)

Page 30: Weather Chp. 2

Freezing rain – rain that freezes upon contact with the ground.

Page 31: Weather Chp. 2

• IsobarA line on a weather map connecting places

that have the same air pressure.

Page 32: Weather Chp. 2

high-pressure system

A generally calm and clear weather system that occurs when air sinks down in a high-pressure center and spreads out toward areas of lower pressure as it nears the ground.

(More dense cold air)

Page 33: Weather Chp. 2

low-pressure system

A large and often stormy weather system that occurs when air moves around and into to a low-pressure center, then moves up to higher altitudes.

(Less Dense Warm Air)

Page 34: Weather Chp. 2

Storms• Caused by:• Changes in temperature & drop in

barometric pressure• Ex: Hurricanes are a low pressure mass

over tropical (warm) water

Page 35: Weather Chp. 2

Weather Fronts• Air mass-a huge body of air that has

similar temperature, humidity, and air pressure

• Front-the area where two air masses meet and do not mix

• Dense,cold air moves underneath the less dense warm air, pushing it up

Page 36: Weather Chp. 2

Front Types• Cold front-rapidly moving cold air mass

that runs into a slowly moving warm air mass

• Move quickly, causing violent storms• Warm front- warm air that collides with

cold air • Moves slowly, causing fog or rain for days,

and in the winter, snow

Page 37: Weather Chp. 2

Cold Front(More Dense cold Air)

Cold Front

Page 38: Weather Chp. 2

Warm Front(Less Dense Warm Air)

Warm Front

Page 39: Weather Chp. 2

Stationary Front

Stationary Front

Page 40: Weather Chp. 2

Weather Forecasting• Meteorologists-scientists who study

weather and try to predict it• Forecasting has greatly improved due to

computer technology• Collecting weather data has improved

because of satellites and balloons

Page 41: Weather Chp. 2

Seasons and Climate• Earth has seasons because Earth’s axis

tilted as it moves around the sun• Winter-axis tilted away from sun resulting

in shorter days and indirect rays• Summer-axis tilted toward sun resulting in

longer days and direct rays

Page 42: Weather Chp. 2

Climate• Caused by:• Altitude• Latitude• Mountain barriers• Proximity (closeness) to oceans

• Climate is classified by precipitation and temperature based on these factors