CK12 Earth Science

(Marvins-Underground-K-12) #1

North Atlantic Oscillation mostly alters climate in Europe. The Mediterranean also goes
through cycles, varying between being dry at some times, and warm and wet at others.


Causes of Climate Change


Many natural processes cause climate to change. There can be changes in the amount of
energy the Sun produces. As Earth orbits the Sun, there are also changes over thousands
of years in the tilt of Earth’s axis and orbit. Over millions of years, the positions of our
continents change, driven by plate tectonic motions. Random catastrophic events, like a
large asteroid impact can cause sudden, dramatic changes in climate. Human activities have
greatly increased the amount of greenhouse gases in the atmosphere, which impacts global
climate by warming the Earth.


Solar Variation


The amount of energy the Sun radiates is variable. Sunspotsare magnetic storms on the
Sun’s surface that increase and decrease over an 11-year cycle (Figure17.32). When the
number of sunspots is high, solar radiation is also relatively high. But the entire variation in
solar radiation is tiny relative to the total amount of solar radiation that there is and there
is no known 11-year cycle in climate variability. The Little Ice Age corresponded to a time
when there were no sunspots on the Sun.


Figure 17.32: Sunspots on the face of the Sun. ( 33 )

Plate Tectonics


Plate tectonic movements can alter climate. Over millions of years as seas open and close,
ocean currents may distribute heat differently. For example, when all the continents are
joined into one supercontinent (like Pangea), nearly all locations experience a continental
climate. When the continents separate, heat is more evenly distributed. Plate tectonic
movements may help start an ice age. When continents are located near the poles, ice
can accumulate, which may increase albedo and lower global temperature. Low enough
temperatures may start a global ice age.


Plate tectonics also triggers volcanic eruptions, which release dust and CO 2 into the atmo-
sphere. Ordinary eruptions, even large ones, have only a short-term effect on weather. Ash

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