1. Climate and Ecosystems
Chapter 11

2. What effects can a changing climate have on living organisms?
We’ve talked about Global Climate Change (sometimes called Global Warming).
What is climate?
What effects can a changing climate have on living organisms?
Suppose your region has an especially hot summer, followed by a very cold winter that includes a snowstorm. Does this support, disprove, or have little to do with Global Climate Change? D A I L Y W O R K

3. Climate Climate is not the same thing as weather!
Climate consists of the prevailing weather patterns in a region over longs periods of time.
Climate is caused by many factors, including location on the globe, nearness to an ocean, wind direction, geography.

4. True or False: Summer is warmer than winter because the earth is closer to the sun in the summer.

5. True or false: When it is winter in the northern hemisphere, it is summer in the southern hemisphere.
True
False

6. Think about this…
If it were true that seasons were caused by the earth being closer to or further away from the sun…
…how would it be possible that the southern hemisphere is experiencing summer while the northern hemisphere is experiencing winter?
Remember, we are 93 million miles from the sun. Small changes in distance aren’t going to have a big effect.

7. The sun drives climate as well as the seasons.
Summer in the
Northern
Hemisphere
North
Pole
90° N
23.5°
tilt 0°
equator
FIGURE 29-1 Earth's curvature and tilt produce seasons and climate
Temperatures are highest and most uniform at the equator and lowest and most variable at the poles. Equatorial sunlight is more perpendicular and hits this band year-round, while polar sunlight is seasonal, and its angle spreads it over a much larger land surface. The tilt of Earth on its axis causes seasonal variations in the range and directness of sunlight. 0°
23.5°
tilt
Summer in the
Southern
Hemisphere
South
Pole
90° S
June 21st :
northern summer
solstice; southern
winter solstice
December 21st :
northern winter
solstice; southern
summer solstice

8. Average temperature at any part of the globe is affected not by how close we are to the sun (a common misconception) but by the angle of incidence of the sun’s rays.
Less direct rays = less solar energy = cooler region
More direct rays = more solar energy = warmer region

9. Global air circulation influences local climates.
Rising air cools and drops moisture.
Descending air tends to be dry.
cold, dry
air falls
cool, moist
air rises
(rain/snow)
Polar
Easterlies
90 N
polar cap
60 N
Westerlies
warm, dry
air falls
30 N
desert
N.E.
Tradewinds
hot,
moist
air rises
(rain)
rain
forest
rotation
S.E.
Tradewinds
rain
forest
desert
30 S
warm, dry
air falls
Westerlies
60 S
Polar
Easterlies
polar cap
90 S
cool, moist
air rises
(rain/snow)
cold, dry
air falls

10. According to this diagram, where on the planet should we find:
Deserts?
Tropical rain forests?
Permanent snowfields?
A. Cool, moist, rising air D A I L Y W O R K
B. Warm, dry, falling air
C. Warm, moist, rising air

11. Ocean current also affects climate.
Water tends to absorb and retain heat, and lose it slowly.
Ocean water near the equator tends to be warm, so currents from the equator are warm.
Water near the poles is much cooler.

12. The Gulf Stream carries warm water from the equator northward, warming the coast of Europe.
There is evidence that the Greenland ice is melting, due to Global Climate Change, and pouring cold water into the North Atlantic. If enough cold water is dumped into the Atlantic, it could divert the Gulf Stream.

13. If the Greenland ice melts and disrupts the Gulf Stream, what will happen to the climate of Northern Europe?
It will get much colder.
It will get much warmer.
There will be very little change.

14. Observe this diagram of the Jet Stream, prevailing winds across the North American Continent.
Remembering that oceans tend to absorb more heat than land, and that currents and wind pattern affect climate, explain the pattern of climate across North America as shown by the map of USDA planting zones in the next slide. D A I L Y W O R K

16. Climate Fluctuations
Some natural processes can cause local climate to fluctuate from year to year.
One example: El Niño/ La Niña weather cycles along the American Pacific coasts.

17. More info at: http://www.sbg.ac.at/ipk/avstudio/pierofun/atmo/elnino.htm

18. In an El Niño cycle, prevailing Trade Winds weaken
In an El Niño cycle, prevailing Trade Winds weaken. Warm water spreads back across the Pacific, disrupting upwellings along the South American coast.

19. As a result of El Niño, what happens to the fishing industry off of the coast of Peru?
Warmer water increases the nutrients and the number of fish.
Loss of cold upwellings decreases nutrients and the number of fish.
There is no change to the fishing industry; this is just part of the weather cycle.

20. Local Climate Localized climate zones can be caused by:
Proximity to oceans or large lakes.
Position of mountain ranges.
Wind direction.

21. Oregon Coast
Peruvian Coast
Oregon is on the west side of the North American continent. Peru is on the west side of the South American continent. Why do these two areas look so different?

22. Water is released
as air rises and
cools.
Dry air sinks,
warms and
absorbs water
from the land.
Water is carried
from ocean by
prevailing winds.
dry climate in
rain shadow
moist climate
The rain shadow effect can cause moist conditions on one side of a mountain range and dryer conditions on the opposite side of the mountains.
On the Peruvian coast, prevailing winds blow from the mountains toward the ocean. What effect might that have on climate on the coast of Peru?

23. Lakes, too, can influence local climate if they are large enough.
Lake Effect
Lakes, too, can influence local climate if they are large enough.

24. high
rock, snow, ice
tundra
coniferous
forest
deciduous
forest
altitude
tropical
forest
low
equator
(0°)
poles
(90°)
latitude
Altitude and latitude also interact to create local climates that support different types of communities.

25. Observe the map of Oregon on the next slide
Observe the map of Oregon on the next slide. Use what you have learned to explain the average rainfall in the different areas of the state indicated on the map. D A I L Y W O R K

26. D A I L Y W O R K Oregon Coast: Willamette Valley: 70-100 inches
Coastal Mountains
Cascade Mountains D A I L Y W O R K
Pacific Ocean
Oregon Coast:
inches
Willamette Valley:
25-30 inches
Eastern Oregon:
6 – 8 inches

27. If the prevailing winds in Oregon blew from east to west, what would our coastline be like?
Rainy, as it is now.
Dry, like Peru.
A mixture of dry and wet areas, depending on the local terrain.

28. The prevailing winds blow from west to east on the North American continent. Why is the east coast of the U.S. NOT a dry desert like Peru? D A I L Y W O R K

29. Recap Climate begins with the sun’s heat.
Climate is influenced by ocean and atmospheric currents, which are driven by the sun’s heat.
Geography influences local climate.
Climate directly affects what organisms can live in an area.