LACEMOPS Power Point
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Transcript LACEMOPS Power Point
Climate Factors
&
World Climate Regions
LACEMOPS
TEKS 3A,B,C and 4A,B,C
Latitude
Latitude
a) Low Latitudes –> 30° south to 30°
north
(1) Warm to Hot all year long
b) Middle Latitudes –> 30 ° to 60 °
in both N. & S. hemisphere
(1) Hot and Cold with seasons
c) High Latitudes –> 60 ° to 90 ° in
both N. & S. hemisphere
(1) Chilly to Cold all year
Air Currents
Global Wind Patterns
Same kind of circulation just on a larger
scale
– Hot air flows toward the poles, cold air
moves toward the equator
– Because the earth rotates, winds turn
at an angle
In the North – turn to the right
In the South – turn to the left
–Coriolis Effect – bending of the
wind
Global Wind Currents
Convection Currents
Continentality – a region’s distance
from the moderating influence of
the sea
a) Air crossing over continents
loses its warmth the farther
inland it goes
(1) Larger land masses =greater
changes in temperature
(2) Land gets hot or cold depending
on air temp., while water
remains the same
Elevation
Elevation -the distance above sea level
– also affects climate
– Air temps drop about 3.5 degrees per 1,000
ft.
– (pics of mt. everest, death valley, etc.) maybe
Mountain Barriers
The lay of the land affects climate
as winds blow up the side of a mountain
they cool and drop rain, snow, etc.
(windward side)
as they come down the other side they
are drier and warm as they come down
(leeward side)
Deccan Plateau
What climate inferences can be made regarding this picture ?
Ocean Currents
Like rivers flowing in the ocean
– Warm waters flow away from the equator
– Cold waters flow back toward the equator
Currents affect temperature of a region
–Warmth of Gulf Stream and North
Atlantic Drift help keep Europe’s
temperature moderate
–Atacama Desert in South America
and Namib Desert in Africa formed
partially by cold ocean currents
Pressure and Prevailing
Winds?
High Pressure –
heavy, cold air
Low Pressure –
warm, light air
– Heat rises
– Prevailing winds
Storms
Storms are created by Prevailing winds
Where polar winds meet Westerlies there
are storms
– When hot air masses and cold air masses
collide – there are storms
Cyclonic storms (hurricanes, typhoons)
– Spin counter-clockwise in the Northern Hem.
– Spin clockwise in the Southern Hem.
El Nino/La Nina
La Niña is characterized by unusually cold ocean
temperatures in the Equatorial Pacific,
– when winds blow warmer water onto the western Pacific rim
– Causes more rain in India and dryness along the coast of Americas
El Niño, which is characterized by unusually warm ocean
temperatures in the Equatorial Pacific
– Occurs every 2-7 yrs
– Prevailing winds that blow over central Pacific Ocean slow or
reverse direction – changes ocean temps, affecting weather
worldwide
El Nino
La Nina
Global Warming
Global temperature is rising
Natural? Or Man-made?
Greenhouse effect – burning of fossil fuels
traps solar energy, increasing temperatures
World Climate Regions
Factors in Climate
Key factors in climate differences –
Rain amount
Location
Topography
Elevation
Temperature
Tropical Wet
Always hot
Avg. temp of 80 degrees
Days begin sunny but becomes rainy in
the afternoon
Rains almost daily
Avg. more than 80 inches of rain
Location
– Central & South America, Africa &
Southwest Asia
Tropical Wet & Dry
Rainy season in summer – temp warmer
Dry season in winter – temp cooler
Rainfall is less than Tropical Wet
Location
– Africa, South & Central America, parts of Asia
Semiarid
Does get rain but not much: about 16 in. per
year
Summers are hot
Winters are mild to cold
Some areas can produce snow
Location –
– In the interior of continents or around desert
zones
– Contains some of the most productive
agricultural lands in the world
Desert
Can be hot/cool/cold depending on the
amount of rainfall
Less than 10 in. of rain per year
Hot Deserts
– Sahara & Arabian Desert – have low humidity,
high temps during day, temps drop at night
– Cool/Cold deserts – found in mid-latitudes near
mountain ranges – temps range from pretty hot
to below freezing
Mediterranean
Named for its location around the
Mediterranean Sea
Summers – dry & hot
Winters – cold & rainy
Supports dense population & rich
agricultural activity
Also is located along the west coast of
U.S. and parts of Australia
Marine West Coast
Mostly cloudy, foggy, & damp
Winds over the ocean moderate temps &
keep temps constant
Rain is evenly distributed throughout the
year
Industrial regions experience smog (smoke
& fog)
Location –
– Close to the ocean along parts of west coast
of U.S. & Canada
– Western Europe also
Humid Subtropical
Long summer heat & humidity
Areas are on the east coasts of continents
Subject to hurricanes in late summer &
autumn
Winters – mild & cool
Very suitable for raising crops, esp. rice
Location –
– Southeastern U.S. and large parts of
China
Humid Continental
Large variety of temps & rainfall
Found in mid-latitude interior of
continents
Arctic air collides with tropical air to
create a vast change in temps.
Length of seasons depends on
latitude
Subarctic
Covered by evergreen forests (taiga) esp.
– Canada & Russia
Huge temp range between summer &
winter
Summers – short, cool
Winters – very cold
Temps at freezing or below for the last 5
to 8 months of the year
Tundra
Flat, treeless lands that form a ring
around the Arctic Circle
Almost completely in the Northern
Hemisphere
Very little rain, less than 15in.
Permafrost – subsoil is frozen
constantly
Summer – temps may reach 40
degrees – but only lasts for a few
weeks
Highlands
Climate varies with latitude, elevation,
topography, and continent location
Other factors are whether a slope is
facing north or south & the kinds of
winds that are carrying moisture
Many are amongst mountain ranges
Ice Cap
Snow, ice, permanently freezing temps
So cold it rarely snows!
“polar deserts” – less than 10 in. of rain
a yr.
Coldest temp recorded –
–128.6 below zero, Vostok, Antarctica
Soil Regions
Soil – a thin layer of weathered rock,
humus, air, & water
Humus – organic material
World’s food supply depends greatly on
the topsoil (top 6 in. of soil)
Depth, texture, & humus content
determine what type of vegetation can be
grown in a region
Vegetation Regions
Soil, temp., & moisture influence the kind
of vegetation that will grow in a region
Ecosystem – community of plants &
animals
Biome – the ecosystem of a region
– Forest
– Grassland
– Desert
– Tundra
Forestlands
2 Types
Deciduous Trees – broadleaf
Ex: rainforest, some may stay green all year
Most shed their leaves at least once a year
Located – almost completely in Northern
Hem.
Coniferous Trees – needleleaf, cone bearing
Located – northern parts of N.A., Asia, &
Europe
Mostly flat regions dotted with a few trees
- Different names from different regions
a. Savanna – tropical grassland region
b. Steppe or Prairie – northern hemisphere
c. Pampas – southern hemisphere
A. Can only support plants that can:
(cacti, sagebrush, shrubs )
- Conserve water
- Withstand heat
B. Only supports plants that hug the
ground
- Mosses
- Lichen