Exam review, Paleoclimates Flashcards

1
Q

what are the climatic conditions (in terms of general trends) of the Pleistocene

A

VERY COLD (large fluctuations still within the cold temperatures)

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2
Q

when did the Pleistocene happen

A

1.8 mya - 12 kya

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3
Q

what are the subsections of the Pleistocene

A

lower
middle
upper

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4
Q

when was the lower Pleistocene

A

1.8 mya to 780 kya):

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5
Q

what is the lower Pleistocene characterized by

A

characterized by steadily decreasing global temperatures

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6
Q

when was the middle Pleistocene

A

780 kya to 126 kya

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7
Q

what is the middle Pleistocene characterized by

A

characterized by generally low, yet wildly fluctuating temperatures

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8
Q

when was the upper Pleistocene

A

126 kya to 12 kya

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9
Q

what did upper Pleistocene correspond to

A

corresponding to the end of the last major Ice Age (Last Glacial Maximum)

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10
Q

what is the Paleoclimates: Milankovitch Cycles responsible for

A

Earth’s glacial and interglacial periods within the Late Pleistocene have been caused primarily by cyclical changes in the Earth’s circumnavigation of the Sun

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11
Q

what do the Milankovitch Cycles affect

A

These changes affect the seasonality and location of solar energy around the Earth, thus impacting contrasts between the seasons

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12
Q

what are the three changes in Milankovitch Cycles

A

eccentricity, obliquity (axil tilt), precission

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13
Q

what does eccentricity do

A

changes to the shape of the Earth’s orbit around the Sun. Orbital shape ranges between more and less elliptical on a cycle of about 100,000 years. Greater variation in Sun’s energy reaching Earth when orbital shape is more elliptical

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14
Q

what is obliquity (axil tilt)

A

is the inclination of the Earth’s axis in relation to its plane of orbit around the Sun. Oscillations in the degree of Earth’s axial tilt occur on a periodicity of 41,000 years from 21.5 to 24.5 degrees. Affects the severity of the Earth’s seasons

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15
Q

what is Precession

A

is the Earth’s slow wobble as it spins on axis. This wobble has a periodicity of 23,000 years. Contributes to differences in seasons felt by the Northern and Southern hemispheres

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16
Q

where are we currently in the Milankovitch Cycles

A

in between basically all of them (actually doesn’t say for Precession)