Meteorology: The Atmosphere, Weather, & Climate

What is the atmosphere?

  • Thin envelope of mixed gases surrounding earth

  • Composition: ESRT

  • Composition doesn’t vary

    • Only water vapor and carbon dioxide

Layers and boundaries between the layers of the atmosphere

  • ESRT page 14

  • Layers: troposphere, stratosphere, mesosphere, thermosphere

    • Basis for division is based on temperature shifts/changed (cooling/heating)

  • Boundaries: Tropopause, stratopause, mesopause

    • Named for layer below boundary

The Troposphere

  • Temp cools as altitude increases

    • b/c moving away from surface which reradiates heat (infrared) and warms air

  • Highest moisture content

    • Causes weather

  • Highest pressure

    • Bc weight of more air molecules above

The Stratosphere

  • Temp increases as altitude increases

    • Bc ozone (O3) absorbs UV and reradiates some of the energy as heat (infrared)

The Mesosphere

  • Temp decreases as altitude increases

    • Bc of lack of ozone

    • Far from ground (& the heat it reradiates)

The Thermosphere

  • Temp increases as altitude increases

    • Bc N2 and O2 atmos absorb solar energy

  • Thins into space


Energy

  • A major source of energy for most of Earh’s processes is the Sun

How is energy measured?

  • Temp = measurement of avg. kinetic energy (KE) of particles

    • Faster moving →more KE → higher temp

  • Measured with a thermometer

  • Heat = total KE of particles

    • Measured in Joules (J)

    • Always flows with high temp (source) to low temp (sink)

What is electromagnetic (EM) energy?

  • A type of energy that is radiated, or given off in the form of waves from all matter

    • Only given off above absolute zero (0 Kelvin or -273C, the lowest theoretical temp)

  • Types are classified by their different wavelengths

    • Wavelength: Distance from one crest to the next crest

What are the characteristics and types of EM energy?

  • Visible light Is the only EM energy that can be seen by human eyes

  • Infrared = heat (energy can be felt from warm obects)

  • Instruments must be used to observe other forms of EM energy, such as UV rays

How does EM energy interact with the environment?

  • Reradiated

    • Absorbed and released as heat

  • Refraction

    • Bent when passes through materials w/diff densities

  • Reflected

    • Bounced of materials

  • Scattered

    • Deflected into many diff directions

  • Transmitted

    • Passed through material without being changed

  • Absorbed

    • Taken into material

    • Material heats up

      • Releases heat in form of infrared

        • Reradiation

What are three ways energy is transferred?

  • Conduction

    • Molecules colliding w/each other

    • Solids

  • Convection

    • Due to density differences

      • Warm rises

    • Liquids and gases

  • Radiation

    • By EM waves

    • Anything transparent

How is the Earth’s atmosphere heated?

  • Insolation

    • Incoming solar radiation

  • Most directly heated by Earth’s surface

    • Radiation: Insolation is absorbed by Earth’s surface

    • Conduction: Earth’s surface heats air molecules that come in contact with it

    • Convection: Heat travels through atmosphere in currents due to density differences

What is the Greenhouse Effect?

  • Contributes to heat of the atmosphere

    • Short waves absorbed by Earth’s surface

      • Long wave infrared radiation/heat is reradiated

        • Most IR escapes, some IR is trapped by greenhouse gases in the atmosphere

        • (CO2, H2O, methane, etc.)

          • Causing heating

  • The more greenhouse gases in the atmosphere, the more heat absorbed

Causes and effects of the enhance greenhouse effect

  • Burning fossil fuels

  • Deforestation

  • Cattle ranching

    • Enhanced greenhouse effect

      • Temp rise and climate change

      • More severe hurricanes

      • Desertification

      • Impact on health (ex. insect-borne disease)

      • Habitat alteration (and migration patterns)

      • Sea level rise

  • How to minimize the amount of carbon dioxide released into the atmosphere and decrease reliance on fossil fuels:

    • Use alternative energy, minimize use of cars

What type of insolation reaches Earth’s surface?

  • Visible light = dominant form of energy from Sun that reaches surface

    • Most energy does not reach surface bc absorbed by atmosphere

      • Ex. ozone in stratosphere absorbs harmful UV radiation

        • Humans are depleting the ozone layer by using chemicals like chlorofluorocarbons (CFCs). This allows more UV rays to reach Earth, which can cause skin cancer and eye damage.

The Heat Balance of Earth and the Atmosphere

  • Overall flow of energy into/out of the atmosphere balances

    • Important bc:

      • Keeps temp at a level that makes life possible

      • Balance can be upset…

        • Energy in > out = heating

        • Energy out > in = cooling

If energy flow into and out of the atmosphere is in balance, what causes Earth’s temperature to vary from place to place and time to time?

  • Main reason = uneven heating of the surface due to:

    • Differences in intensity of insolation

    • Aount of insolation reaching the surface

    • Amount of insolation absorbed by the surface

What factors affect the intention of insolation?

  • Which angle would have the:

    • Most intense insolation?

      • 90 degrees bc most direct (most concentrated)

    • Least intense insolation?

      • 0 degrees bc least direct (most spread out/least concentrated)

  • Which latitudes would have the:

    • Most intense insolation?

      • 0 degrees (Equator) bc highest angle of insolation

    • Least intense insolation?

      • 90 N/S (poles) bc lowest angle of insolation

  • Which time(s) of day would have the:

    • Most intense insolation?

      • Noon bc highest angle of insolation

    • Least intense insolat?

      • Sunrise/sunset bc lowest angle of insolation

  • In NY (N. Hemi.) which season(s) would have the:

    • Most intense insolation?

      • Summer bc tilted towards the Sun

    • Least intense insolation?

      • Winter bc tiled away from the Sun

How much insolation reaches Earth’s surface?

  • Atmospheric transparency (how much insolation reaches Eath’s surface) depends on reflection, refraction, scattering, and absorption of insolation by clouds, dust, etc.

  • Which would be warmer:

    • Clear day or cloudy day?

      • Clear day bc more insolation reaches surface

    • Clear night or cloudy night?

      • Cloudy night bc clouds act like a blanket trapping heat re0radiated by surface

  • Dust from volcanic ash, pollution, meteor impacts, forest fires blocks sunlight from reaching Earth, and can result in cooling

What factors affect how much insolation is absorbed by Earth’s surface?

  • Albedo (ability to reflect light)

  • what types of surfaces would have:

    • Low ‘albedo’

      • Dark, dull, rough (absorbs more insulation)

    • High ‘albedo’

      • Light, shiny, smooth (relects more insolation)

  • Specific heat (amt. of heat needed to raise 1g of a substance by 1C/resistance to heating/cooling)

    • Which material heats & cools faster/slower?

      • Faster = land, low specific heat

      • Slower = water, high specific heat

    • ESRT pg 1

  • Good absorbers of energy are also good radiators (& vice versa)

What else causes Earth’s temperature to vary from place to place and time to time?

  • Geographic location

    • Which location has a greater temp range (continental/maritime)?

      • Greater temp range = Continental (inland & leeward coast)

      • Smaller temp range = Maritime (windward coast) wind blowing from water towards the coast) water helps to moderate temp bc of high specific heat

  • How do currents affect a location’s temp?

    • Warm currents help to moderate climate

  • Altitude

    • Which altitude is warmer?

      • Near sea-level = warmer

      • Higher altitude (above sea-level) = cooler

        • Adiabatic temp changes

          • Rate of change ~1C/160m (= normal lapse rate)

        • Adiabatic temp changes caused by expansion/compression of air as altitude changes

          • Rising → expansion = cooling

          • Sinking → compression = heating

Why Did the Isotherms Shift with the Seasons?

  • Land (w/ low specific heat) heats and cools more readily than water (w/ high specific heat)

    • Shift is more dramatic over land than water


Weather

What is weather?

  • Short-term state of atmosphere at given time and place

  • Use senses and different tools to observe

  • Weather factors are interrelated; when one changes, one or more of the others change

  • To try to predict the weather you need to:

    • Observe weather factors over a period of time

      • And look for patterns in how these factors change relative to each other

What factors affect weather? - Temperature

  • Recall.. Temp = measurement of avg. kineti energy of particles

    • Faster moving particles → greater avg. kinetic energy → higher temp.

  • Measured with thermometer

    • Celcius, Fahrenheit, Kelvin scales

      • ESRT pg 13

  • Isotherms connect equal temperatures on maps

  • Temp goes up, density goes down

    • Warm air rises/cold air sinks

  • Altitude in troposphere goes up, temp goes down

    • Farther from surface reradiating hear

    • ESRT pg 14

What factors affect weather? - Humidity

  • amount of water vapor in air

    • Most important gas when it comes to understanding atmospheric process

  • Mositure capacity = amount of H2O vapor air can hold

    • Warm air can hold more moisture (more space between particles)

  • Relative humidity (RH)

    • Amount of H2O vapor in air compared to moisture capacity (expressed as %)

      • 100% RH means air is saturated (full of water) and at its dew point (DP) temperature (condensation occurs)

        • Clouds can form and precipitation is likely

  • Measure RH and DP w/sling psychrometer

Determining RH

  • Sling psychrometer

    • Dry bulb thermometer: measures normal air temperature

    • Wet bulb thermometer: has a wet cloth on the bulb which causes the thermometer’s temp to lower due to the cooling effect of evaporation

  • → How to use

    • Wet wick on wet bulb

    • Spin psychrometer for a specified amount of time

    • Read temps on both wet and dry bulbs

      • Wet bulb temp should always be equal or cooler than dry bulb temp. due to expiration of water

    • Record data

  • Use RH chart

    • Calculate difference

    • Locate difference on the RH chart

    • Locate dry bulb temp

    • Find where they intersect

  • IT’S THE SAME PROCESS FOR DEW POINT, JUST THE OTHER CHART

What is the relationship between air temp, DP, and RH?

  • Closer air temp and DP, the higher the RH

    • Precipitation more likely

  • Farther apart air temp and DP, lower the RH

    • Precipitation less likely

How do Clouds form?

  • Parcel of warm air rises, expands, and cools to DP temp where RH = 100% (at condensatino level), confesses onto condensation nuclei (ex. dust, salt, etc.)

  • Cloud shape depends on air movement

Types of precipitation

  • Drizzle

    • Very fine water droplets that fall slowly and close together

  • Rain

    • Larger droplets that fall faster than drizzle

  • Snow

    • Ice crystals collide and clump

  • Sleet

    • Supercooled raindops that freeze in the air

  • Freezing rain

    • Supercooled raindrops freeze instantly when hit surface

    • Causes sheet ice or glaze

  • Hail

    • Layers of ice, snow, and water formed by many movements in thunderstorm clouds

Characteristics of Water

  • Recall..

    • Solid water = ice

    • Liquid water = water

    • Gases water = water vapor

  • Phase changes require energy transfer in the form of heat

    • Latent heat = energy absorbed or released during phase change

Phase changes

  • Melting

    • Solid → liquid

    • Requires addition of 334J/g of energy

  • Freezing

    • Liquid → solid

    • Requires release of 334J/g of energy

  • Vaporization

    • Liquid →gas

    • Requires addition of 2260J/g of energy

  • Condensation

    • Gas → liquid

    • Requires release of 2260J/g of energy

Why is Evaporation of Cooling Process?

  • Molecules enter atmosphere as vapor → taking energy with them → slower molecules left behind and have less average energy → causing cooling

  • What factors affect exaporation rates?

    • Temperature

      • Warm = higher rate

    • Humidity

      • Low = higher rate

    • Winds

      • High/fast = higher rate

    • Surface area

      • Larger = higher rate

    • Covering

      • Uncovered = higher rate

What factors affect weather? - Air Pressure

  • Aka atmospheric or barometric pressure

  • Weight of gases pushing on Earth’s surface

    • High pressure → more gases pushing down

    • Low pressure → less gases pushing down

  • Measured with a barometer

    • Aneroid (units = millidars_

    • Mercury (units = inches)

      • ESRT pg 13

  • Isobars

    • Connect points of equal pressure

  • Air pressure is affected by:

    • Humidity

      • Dry air, more dense, sink → high pressure

      • Humid air, less dense, rises → low pressure

    • Altitude

      • Low altitude, more air above → high pressure

      • High altitude, less air above → low pressure

    • Temp

      • Cold air, more dense, sinks →high pressure

      • Warm air, less dense, rises → low pressure

  • All are inverse relationships

  • Barometric trends can tell us what weather to expect…

    • When air pressure is:

      • Increasing over time → clear/fair weather is coming

      • Decreasing over time → stormy weather is coming

  • Pressure center: highest or lowest pressures on a weather map

    • Isboars form circles, or “bulls-eye,” around the pressure centers

What is a High-Pressure Center/System?

  • As move towards center of closed isobars, pressure increases

    • Aka “high” or “anticyclone”

      • “Heavy”/dense, cool, dry air

      • Circulates clockwise

        • “Right-hand rule”

        • Thumb goes down

      • Sinks/hits and diverges

      • Fair, “happy” weather

What is a Low-Pressure Center/System?

  • As move toward center of closed isobars, pressure decreases

    • Aka “low” or “cyclone”

      • “Light”/less dense, warm, wet air

      • Circulates counterclockwise

        • “Right-hand rule”

        • Thumb goes up

      • Converges and lights

      • Stormy, “lowsy”

What factors affect weather? - Wind

  • Horizontal movement of air

    • Caused by density differences due to uneven heating

  • Always blow from hight pressure (cool) to low pressure (warm)

  • Named for direction from which they blow (ex. noth wind blows FROM north)

    • Direction indicated by wind vane

      • Arrowhead points into wind (where blowing from)

  • Speed

    • Depends on pressure gradients (change in pressure over change in distance)

    • Greater (steep) gradient → faster wind

      • Isobars close together

    • Lower (gentle) gradient → slower wind

      • Isobars father apart

    • Measured with anemometer

How does specific heat of land vs. water affect wings?

  • Sea (ocean) breeze: during the day, the surface wind blows from the water (cooler w/high pressure) towards the land (warmer w/low pressure)

  • Land breeze: at night, the surface wind blows from the land (cooler w/ high pressure) towards the water (warmer w/ low pressure)

  • Mon soons: Seasonal reversing of winds and precipitation patterns caused by large temp diff of land and ocean water in certain seasons

    • Summer: heavy rain occur when moist wind flows from ocean onto land

    • Winter: dry conditions occur when dry wind flows from the land to ocean

How can all of these weather factors be shown on a map at the same time?

  • Station model: simple diagram that summarizes 10 pieces of weather information

    • A station model shows no units!

    • A/N : A SEPARATE NOTE WILL BE MADE REGARDING STATION MODELS

What is an air mass? How do air masses originate?

  • Air mass = immense body of air with uniform properties (temperature and moisture content)

  • Originate when: Air maintains some position for days/weeks over a large, uniform surface where winds are light

    • Source region/where forms affects main properties

      • Temp depends on if air is from tropics or poles

      • Humidity depends on if air is from land or see

Maritime Tropical (mT)

  • Warm and humid

  • Source region = over water near equator

Maritime Polar (mP)

  • Cool/cold and humid

  • Source region = over water near high lat./poles

Continental Tropical (cT)

  • Warm and dry

  • Source region = over land near equator

Continental Polar (cP)

  • Cold and dry

  • Source region = over land near mid to high lat./poles

Continental Arctic (cA)

  • Very cold and dry

  • Source region = over land near high lat./poles

    • **Don’t really need to know much about it

How do air masses affect weather?

  • May take days to pass

    • Weather of the place air mass move to becomes like the weather of the source region

    • Fast-moving air masses bring more extreme weather than slow-moving ones

Which air masses are most important to us in NY?

  • The weather in NY is most influenced by two air masses:

    • cP from Central Canada

    • mT from Gulf of Mexico

Global Winds, Air Masses, and Weather Systems

  • Large global winds (the westerlies) generally move air masses and weather systems from west to east in the US

Fronts

  • Beginning edge of an air mas

    • Where two air masses with different temperature & humidity (& density) meet

      • Brings weather changes

        • Precipitation usually occurs along (or in front of) the front

  • Generally named by the air mass behind it

  • Extend outward from low-pressure center

  • Causes changes in:

    • Precipitation

    • Temperature

    • Humidity

    • Air pressure

    • Wind direction

Stationary Front

  • Warm, air & cold air push against each other, neither get displaced/move

    • Very little mixing of air

  • Weather ‘sits’ in an area for a long time

  • Often light rain over several days

  • Symbols point in direction of movement, one on each side of the line

Cold Front

  • Cold (dense) air advances and pushes warmer (less dense) air upward

  • Air behind front brings colder/drier air

    • Pressure increases

  • Severe storms can occur along/on front

  • Symbols point in direction of movement

Warm Front

  • Warm air tries to push cold air (& warm, less dense air slides on top of cold air)

  • Air behind front brings warmer/more humid air

    • Pressure decreases

  • Long, steady rain can occur ahead of front

  • Symbols point in direction of movement

Occluded Front

  • Warm air mass is squeezed between two cold air masses (as advancing cold air catches up to it) and warm air mass is pushed upwards

  • Thunderstorms form along front

    • After front passes sky is usually clear and dry

  • Mid-latitude cyclones (lows) can form

  • Symbols point in direction of movement

How are maps used to determine current weather conditions and to presdict future weather conditions?

  • Weather maps may show:

    • Station models

    • Temperature (isotherms)

    • Air pressure (isobars)

    • High ad low-pressure centers

    • Fronts

    • Wind speed (spacing of isobars)

    • Air masses

    • Precipitation locations (around the low[pressure center, at the cold fronts, and ahead of the warm front)

    • Satellite maps can show areas of precipitation and clouds

How are maps usedd to predict future weather conditions?

  • Weather forecasting: forecast over next few hours..days based upon direction pressure centers and fronts are moving

    • Storm track: in US, storms move from w→e dues to prevailing global winds (westerilies)

      • Typically look at weather conditions in the midwest to predict our future weather conditions in NY

How does radar help scientists determine changes in weather?

  • Doppler radar: a radio tracking system that uses Doppler effect to determine the location and velocity of a storm, clouds, and precipitation


Storms and Severe Weather

What are the Characteristics of Thunderstorms?

  • Cumulonismbus (thunderhead) clouds

  • Lightning and thunder

  • Strong up-and-down air motion

  • Winds do not flow in inward spiral

  • Gusty winds, heavy rain, hail

How do Thunderstorms form?

  • Formed by strong upward movement of warm, unstable air

What causes unstable air associated with thunderstorms?

  • Localized heating of land

    • Causes: Convective lift

  • Fronts

    • Usually cold

    • Can also occur along a warm front bc warm air rising and cooling to dew point

When do thunderstorms usually occur?

  • Spring and summer

    • Greater humidity

    • Warmer temps

      • Causes air rising, cooling to DP, forming clouds and precipitation

What are the Characteristics of Tornadoes?

  • Rapidly rotating column of extermely low pressure air extneding down from thunderstorm

  • Usually accompanied by rain, lightning, and hail

  • Most violent of all storms

  • Often vortex/funnel - shaped (w/ flying debris)

  • Usually narrow (~100 ft diameter)

  • Most only last a few minutes

How do tornados form?

  • Two large air masses with marying “opposing” temp and humidit collide over land with warm air in lower layer and cold air in uppoer layer

    • Causes rotating updraft (mesocyclone) w/ extremely low pressure at center forms

  • Air gets sucked in, expands, and cools

    • Causes air to reach DP, water vapor condenses, and wall cloud mat become visible at base of storm

When do tornados form?

  • Usually late afternoon in spring/summer

    • Atmosphere is warmest and unstable

Where do tornados form?

  • MOSTLY in “Tornado Alley” (Texas, N to S.Dakota)

    • cP and mT air masses collide

What is a tornado that forms over water?

  • Called a waterspout

Can tornados be predicted?

  • Its difficult; improvements have been made

    • Tools:

      • Conventional radar → map precipitation

      • Doppler radar → identify which way winds are moving within sotmr

        • Can identify rotating mesocyclone and give people ~20 min advance-warning

What is the difference between a tornado watch and warning?

  • Watch → tornado MAY form

  • Warning → tornado spotted

How are tornados classified?

  • Fujita scale based on intensity

  • F0 (weakest) to F5 (most violent)

What are some of the effects of tornadoes?

  • Uprooted trees

  • Damage to homes

    • Broken windows

    • Roof damage

    • Desruction of walls

    • Torn off foundation

  • Damage to vehicles

  • Downed power lines

  • Flying debris

  • Loss of life

What are the characteristics of hurricanes?

  • Large, cyclonic (counterclockwise) low-pressure storm

  • Sustained winds of 119+ km/hr (74+ mph)

  • Heavy rains

What is the difference between a hurricane, typhoon, and cyclone?

  • Location

    • Atlantic? Hurricane

    • Pacific? Typhoon

    • Indian? Cyclone

How do hurricanes form?

  • Mild atmospheric disturbance over warm tropical water causes humid air to rise

    • Causes more water to condense and release heat

  • Must begin to rotate counterclockwise (in N. Hemi) bc of Coriolis effect

  • Evaporation of warm water powers the hurricane

    • Loses power when moves over colder waters or land

What are the 3 main parts of a hurricane?

  • Rain bands

    • Clouds that spin out and make storm bigger

  • Eye wall

    • Outer edge of eye

      • Strongest wing and rain bc strongest convergence of air

  • Eye

    • Lowest pressure

    • Calmest part of storm bc converging winds never fully reach center

When is hurricane season in the US?

  • June 1 - November 30

  • August - October is peak

In which direction do most atlantic hurricanes move?

  • Generally, omve west or NW

    • Then, often north and may eventually head east due to global wind patterns

Predicting the path of a hurricane

  • Actual paths can vary considerably: shown by “cone of uncertainty”

What is the difference between a hurricane watch and warning?

  • Watch → expected to arrive w/in 24-36 hours

  • Warning → expected to arrive w/in <24 hours

How do scientists classify tropical storms/hurricanes?

  • Wind speed

    • Tropical depression → up to 61 km/hr

    • Tropical storm → 61-119 km/hr

    • Hurricane →119+ km/hr

  • Saffir - Simpson scale to rate strength

What are some of the effects of hurricanes?

  • Wind damage

  • Inland flooding

  • Storm surge

    • Large wave of water from strong winds of eye wall

      • Blow water into a dome

  • Waves

    • Coastal erosion

  • Loss of life

What are the characteristics of winter storms?

  • Strong mid-latitude cyclone (lows) that form and grow along polar front

  • 2 conditions must be met:

    • Enough mositure

    • Temps cold enough for snow

What is a blizzard?

  • Snowstorm w/high winds and low temps

What causes lake-effect snow?

  • Cold, dry air picks up poisture and heat by passing over a relatively warmer lake

  • When is lake effect snow likely to occur

    • Late fall into early winter bc lake temperatures are at warmest, relative to colder air moving over the,

      • Once lakes freeze over moisture/heat source lost, lake-effect snow hard time forming

How should we prepare for storms?

  • General storm prep

    • Have a family and city emergency storm plan

    • Listen to weather reports for the latest information and instructions in your area

    • Have storm supply kit for your home and car

      • First aid kit and meds

      • Non-perishable food

      • Water

      • Battery operated flashlight and radio

      • Protective clothing and blankets

      • Backup generator

      • Cash


Climate

What is climate?

  • Conditions of the atmosphere over a large region over a long period of time (30+ years)

  • Affected by:

    • Temp and precipitation

  • Affects:

    • Vegetation in an area

    • Animals in an area

    • Landscape features

What factors affect temperature and precipitation, and therefore climate?

  • Latitude

  • Elecation

  • Planetary Winds

  • Nearness to Large Bodies of Water

  • Ocean Currents

  • Mountain Ranges

How do planetary (prevailing) winds affect climate?

  • Planetary windsL general movement of winds in the troposphere that bend due to earth’s rotation (and Coriolis effect)

  • Winds are named for where they are coming from

  • ESRT page 14: NY (40-45N) is in the SW wind belt

How do planetary winds affect climate?

  • Winds from:

    • High latitudes (polar) cause a colder climate

    • Lower latitude (equatorial) cause a warmer climate

    • Off of ocean cause a wetter climate

    • Off the land cause a drier climate

Global Wind and Pressure Belts

  • “Lower Pressure Belts = moist latitudes: 0, 60N, 60S

    • Air rises, cools, and causes water vapor to condense (causes rain)

  • "High Pressure Belts” = Dry latitudes: 30N, 30S, 90N, 90S

    • Air sinks causing it to warm. When air warms, no condensation is possible

What is El Niño?

  • A natural event that changes worldwide weather patterns

    • Caused when surface ocean temp along the weast coast of S. America increases, caysing ocean currents to reverse (or slow) and winds to weaken causing a disruption of normal weather patterns

  • Effects:

    • Winters are warmer and drier in NY

    • Increase temp and precipitation on west coast of S. America

    • Decrease in fishing industry in S. America

    • Droughts in Australia and SE Asia

    • Heavy rains in southern US

How do mountain ranges affect climate?

  • Orographic effect: Changes in climate caused by mountain barriers

  • Windaward: faces toward direction wind is coming from (wind hits windward side)

  • On windward side, air is pushed upward to higher altitude. As air rises, it:

    • Expands bc air is thinner

    • Cools

    • Condenses into a liquid, causing clouds and precipitation to occur

  • Leeward: side of mountain range that faces away from wind (wind is leaving)

  • As air sinks down the leeward side, it:

    • Is compressed

    • Wamrs

    • No condensation can occur in warming air, so its very dry and forms “rain shadow desert”