PALEOCLIMATOLOGY Flashcards

1
Q

Study of ancient climates, prior to the widespread availability of instrumental records.

A

PALEOCLIMATOLOGY

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2
Q

derived from natural sources such as tree rings, ice cores, corals, and ocean and lake sediments.

A

PALEOCLIMATOLOGY DATA

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3
Q

These proxy climate data extend the archive of weather and climate information hundreds to millions of years.

A

PALEOCLIMATOLOGY

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4
Q

represent wood that grew in the spring and early summer

A

light-colored

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5
Q

One light ring plus one dark ring equals?

A

one year of the tree’s life.

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6
Q

Tree rings usually______ in warm, wet years and they are thinner in years when it is cold and dry.

A

grow wider

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7
Q

represent wood that grew in the late summer and fall.

A

dark rings

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8
Q

are very sensitive to changes in climate.

A

corals

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9
Q

Scientists analyze the chemical composition of each layer in the calcium carbonate to reconstruct monthly, annual, and longer records past temperature and salinity.

A

coral

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10
Q

Allow us to generate continuous reconstructions of past climate, going back at least 800,000 years.

A

ice cores

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11
Q

The _________ of each annual layer tells how much snow accumulated at that location during the year.

A

thickness

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12
Q

It provides the only direct record of atmospheric composition (direct gases, total gas content, and isotopic ratios) available in the field of paleoclimatology.

A

ice cores

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13
Q

are washed or blown into lakes can accumulate in sediments and provide a record of past vegetation.

A

Pollen grains

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14
Q

reflect the vegetation that was present around the lake and, therefore, the climate conditions favorable for that vegetation.

A

Different types of pollen in lake sediments

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15
Q

are mineral deposits formed from groundwater within underground caverns.

A

speleothem

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16
Q

may be annually banded or contain compounds that can be radiometrically dated.

A

Stalagmites, stalactites, and other forms

17
Q

used to determine past climate conditions.

A

Thickness of depositional layers or isotopic records

18
Q

used as a foundation for climate scientists by providing crucial information such as rates of past climate change and how vegetation and animal populations responded to the change.

A

paleoclimate data