Earth
Science, 10th edition
Chapter
19: Climate
I. The climate system
A. Climate is an aggregate of weather
B. Involves the exchanges of energy and
moisture that occur among the
1. Atmosphere
2. Hydrosphere
3. Solid Earth
4. Biosphere, and
5. Cryosphere
(ice and snow)
II. World climates
A. Every location has a distinctive
climate
B. The most important elements in a
climatic description are
1. Temperature, and
2. Precipitation
III. Climate classification
A. Brings order to large quantities of
information
B. Many climatic-classification systems
have been devised
C. Köppen
classification of climates
1. Best known and most used system
2. Uses mean monthly and annual
values of temperature and precipitation
3. Divides the world into climatic
regions in a realistic way
4. Boundaries Köppen
chose were largely based on the limits of certain plant associations
5. Five principal climate groups
a. Humid tropical (A)
b. Dry (B)
c. Humid middle-latitude with
mild winters (C)
d. Humid middle-latitude with
severe winters (D)
e. Polar (E)
6. A, C, D, and E climates are
defined on the basis of temperature characteristics
7. Precipitation is the primary
criterion for the B group
IV. Human impact on global climate
A. Humans have been modifying the
environment over extensive areas for thousands of years
1. By
using fire
2. By overgrazing of marginal lands
B. Most hypotheses of climatic change are
to some degree controversial
C. Global warming
1. Water vapor and carbon dioxide
absorb heat and are largely responsible for the
greenhouse effect of the atmosphere
2. Burning fossil fuels has added
great quantities of carbon dioxide to the atmosphere
D. The atmosphere response
1. Global temperatures have
increased
a. Balance of evidence
suggests a human influence on global climate
b. Globally averaged surface
temperature is projected to increase by 1.4 to 5.8°C by the
year 2100
2. The role of trace gases
a. Atmospheric race gasses
1. Methane
2. Nitrous oxide
3. Certain
chlorofluorocarbons
b. Absorb wavelengths of
outgoing Earth radiation
c. Taken together, their
warming effects may be nearly as great as carbon dioxide
VI. Climate feed-back mechanisms
A. Possible outcomes of altering the
climate-system
B. Two types
1. Positive -feedback mechanisms
reinforce the initial change
2. Negative-feedback mechanisms
produce results that are just the opposite of the initial
change and tend to offset it
VII.
Some possible consequences of global warming
A. Altered distribution of the world’s
water resources and the affect on the productivity
of agricultural regions
B. Rise in global mean sea level
C. Changing weather patterns
1. Higher frequency and intensity
of hurricanes
2. Shifts in the paths of
large-scale cyclonic storms
3. Changes in frequency