Weather and Climate

What is the weather like today?

Is it like this EVERY day? Why?

What is the difference between WEATHER and CLIMATE?

Weather and Climate

 Weather – The

temporary

environmental conditions in a localized area over a short period of time.

In other words…what it’s like OUTSIDE, right HERE, right NOW  Climate –

The long-term

environmental conditions across a large area and long time.

In other words…the AVERAGE of all the WEATHERS

What affects weather and climate?

 There are two major factors that affect the overall environment and climate … -The

tilt

of the Earth in relation to it’s orbit around the Sun - The direction of that

tilt

that changes as the Earth travels around the Sun

First, some basic vocabulary…

 Revolution – one ORBIT, or trip around the Sun. This takes the Earth 365 ¼ days Rotation – one SPIN of the Earth on it’s axis. This takes about 24 hours…one DAY.

Earth’s

TILT

 The Earth is not vertical (straight up-and down) in relation to it’s orbital path, it’s

tilted 23 ½ degrees from vertical

.



DRAW THIS ! ! !

This tilt means that the Sun’s energy doesn’t hit the Earth equally.

Earth’s

TILT

 This tilt results in uneven heating of the Earth’s surface.

“Direct” sunlight “Indirect” sunlight

From

TILT

to SEASONS

 As the Earth travels around the Sun, the

tilt

changes in relation to the Sun. Sometimes “toward” the Sun, sometimes “away”, and sometimes neither.  DRAW THIS !!

This creates a predictable cycle of warmer and cooler periods, or seasons.



Seasons

Because the direction of the tilt (“towards” or “away”) is opposite for the Northern and Southern hemispheres, so are the seasons.

Here is the rule to remember… Tilted “toward” the Sun means Summer, tilted “away” from the Sun means winter



Sol

stice

Solstice and Equinox

– the point at which the Earth is pointed farthest toward / away from the Sun, creating long summer days and short winter days . (Latin root word “sol”) – Summer – around June 21 – Winter – around December 21  Equinox – the point at which the Earth is not pointed toward OR away from the Sun, creating

equal

day and

night

. (“equi-nox”) Spring (“Vernal”) around March 21 Fall (“autumnal”) around Sept. 21

Earth’s

tilt

affects length of days

 Places experiencing summer have “longer” days (more sunlight per 24 hrs.) Shorter Winter days Longer Summer days  Places experiencing winter have “shorter” days (less sunlight per 24 hrs.)  Areas above 66 ½ degrees N or S will experience 24 hr. extremes (light and dark) depending on the season 24 hrs.

of light from Nov.

to Feb.

24 hrs.

of dark from May to August

Greenhouse Effect



RULE #1 OF NATURE – Energy can be either absorbed or transferred

 Normally, when the Sun’s energy penetrates the atmosphere, some of it is absorbed, and some of it is reflected back to space.

 Human and natural events increase pollutants that trap the reflected energy and send it back to the Earth again, increasing the Earth’s heat.

Distributing the Sun’s Heat -

WIND



RULE #2 OF NATURE – Nature seeks balance (equilibrium)



Wind is the movement of air from High pressure to Low pressure

 Air Pressure changes with temp.

 “Hot” (more active) molecules need room to move, so they spread apart, meaning LESS molecules  in a given space (LOW pressure) “Cold” (less active) molecules don’t move as much, so they pack closer together, meaning MORE HOT air RISES molecules in a given space (HIGH pressure) COLD air SINKS

  

WIND

– Sea Breeze

When the sun shines, land (solid) heats up faster than water (liquid) – remember RULE #1 ?

 Only the top 2-3 inches of earth get warm, then the heat is reflected back to the air. (Why do dogs dig in the dirt?) The warm air rises, creating LOW PRESSURE over the land during the early/mid-morning This imbalance ( RULE #2 ) creates a

H

in from the water,

L

called a SEA BREEZE

WIND

– Land Breeze

 When the sun sets, the process reverses and land cools off faster than water ( RULE #1 )  This creates COOL

er

air (HIGH pressure) over the land and WARM

er

air (LOW pressure) over the water at night  The WARM wind blowing out from the land is called a LAND BREEZE

L H

 

WIND

- Monsoons

On a larger scale, the same factors create monsoons -

seasonal

winds Due to the Earth’s tilt, differences in the heating of land and ocean create long term wind patterns that bring seasonal rainy and dry periods.



Global Wind Patterns

RULE # 3 OF NATURE – Nature obeys the stronger force

 The Earth gets the most direct sunlight in the tropics, so HOT air RISES at the Equator.

 The least sunlight hits the polar region, so the COLD  air sinks at the poles These two extremes force the middle latitude winds to flow “backwards”, rising at 60 deg. and sinking at 30 deg., even though that is warmer air.

Coriolis Effect

    Because the Earth spins (rotates) under the winds as they travel N and S, they appear to curve because of the Coriolis effect. (see it) The result is curved wind patterns across the Earth surface.

All winds are named for where they come FROM.

Areas of no major wind pattern are called “doldrums” or “horse latitudes” (Spanish explorers)

Water Currents

 Most ocean currents are affected by global wind patterns blowing across the oceans.

Most

WARM

currents flow WEST Most

COOL

currents flow EAST



Precipitation – Nature’s Thermostat

There are 3 basic causes for rain. They are: – Convection – due to evaporation and cooling  Sun’s energy causes surface water to evaporate and become humidity  As the day cools off, the air cools and condenses, causing storms and rain  Usually in tropical environments – Frontal – due to changes in temperature   Starts with warm, moist air at the surface and above As a cold front approaches, it stays low, forcing the moist air aloft  This cools and condenses the air, creating rain on the “leading edge” of the front  Usually in mid-latitudes where warm and cold air systems collide



Precipitation, Part II

Orographic – due to changes in elevation – Moist air travels over land and approaches a steep rise in elevation – As the air is forced up the side of the rise, the air cools, causing precip . on the “windward” side of the mountain – As the (now dry) air continues over and down the “leeward” side of the mountain, it warms up and absorbs any available moisture, creating a “rain shadow desert” – Found in areas of mountains or other rapid elevation change

CLIMATES

 The world is divides into three large climate zones, based on latitude.



DRAW THIS !!!

Low Latitude (“Tropical”) climates – always hot Mid Latitude (“Temperate”) climates – hot/cold seasons High Latitude (“Polar”) climates – seasons either mild or extreme cold

Climate Zones

 Climate zones are divided into regions with differences in

two

key characteristics: – Amount of moisture (rain), and – Typical temperature range through the year  These two characteristics are affected by balancing the effects of four factors:   Latitude Altitude  WRITE THESE DOWN !

 Nearness to water  Direction of atmosphere and ocean currents

Latitude

 Due to the Earth’s tilt, the amount of sun energy changes over the earth’s surface… Polar (High Latitude) zone – either mild temps. or extreme cold Temperate (Mid-Latitude) zone – seasonal, most varied climates Tropical (Low Latitude) zone – year round direct sunlight, always hot

RULE: The HIGHER the latitude, the COLDER the temps.

Altitude (Elevation)

 Higher elevation = thinner air, therefore less air to hold heat makes it colder.

RULE – The HIGHER the elevation, the COLDER the temperatures.

    

Nearness to Water

Land heats up and cools down QUICKLY.

Water heats up and cools down SLOWLY.

Therefore, water acts like a blanket… holding heat and releasing it slowly.

This results in smaller daily and seasonal temperature changes near large bodies of water.

“Coastal” areas are humid, “continental” areas are dry

30 degree change in Houston 45 degree change in Denver



Direction of Currents

Global wind and ocean currents transfer heat and moisture around the world,

and

moisture from the oceans to the land help carry – Warm water moving

toward

the land brings moisture (H 2 O) – Warm water moving

parallel

to the coast brings heat, no H 2 O – Cool water brings cool, dry air -> mild or desert climates



How it Works...

Tropical Wet Climate

L

atitude – in the tropics  HOT 

A

ltitude – low land doesn’t stop air flow until mtns. in the west 

N

earness – flat land “acts coastal”, allows moisture inland 

D

irection – air flow brings in warm, moist air from the ocean which then hits the mountain and rains