Ch 7b: Atmosphere Flashcards

1
Q

Climate:

A

time-average weather conditions at a place on the Earth’s surface.

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2
Q

climate records typically include

A

temperature, precipitation, humidity, wind, cloud cover

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3
Q

Climate change over geological time

A

cenozoic record of cooling, cretacenous warm interval.

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4
Q

Koppen scheme of climate classification:

A

tropical, dry, temperate humid (mesothermal), temperate cold (microthermal), polar

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5
Q

Deserts:

A
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6
Q

Semi-deserts:

A

250-500 mm

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7
Q

Distribution of deserts:

A

belts of low rainfall correspond to regions of divergence.

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8
Q

Types of deserts:

A

subtropical, continental, rainshadow, coastal, polar

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9
Q

Subtropical desert eg

A

Sahara, Kalahari, Great Australian

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10
Q

Continental desert eg

A

Gobi, Takla Makan

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11
Q

Rainshadow desert eg

A

Sonoran

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12
Q

Coastal desert eg

A

Atacama, Namib

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13
Q

Polar desert eg

A

Antarctica

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14
Q

Instrumental records

A

Short term, weather records

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15
Q

Proxy records

A

short to long term: historical, biological, geological, chemical

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16
Q

Average weather records

A

Global correlation, overall warming trend over last 150 yrs.

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17
Q

Geological: Glacier ice records

A

records of glacier extents, geological or historical.

18
Q

Longer-term change: hundreds to thousands of years

A

climate is inferred indirectly, requires validation by other sources. Similar proxy data types as earlier changes.

19
Q

Historical proxy records include

A

agriculture or shipping records, pictures, sketches, paintings, writings, personal letters.

20
Q

Biological Climate proxies:

A

dendrochronology: ring widths show correlation with climate

21
Q

Palynology

A

pollen: record of land vegetation

22
Q

Last 2 Ma: Quaternary Period

A

marked by cold climates worldwide, glacial erosion and deposition in areas no longer glaciated

23
Q

Extent of ice cover:

A

records indicate at least 4 advances and retreats, separated by interglacial periods.

24
Q

Ocean sedimentary records:

A

6 layers of ice-rafted debris deposited during last glaciation (between 70-10ka)

25
Q

Heinrich events:

A

catastrophic calving of ice sheet

26
Q

Ocean sediment records: marine micro-organisms

A

many species of plankton have restricted temperature range. Species alternate in cores, indicating changing temperature changes.

27
Q

Isotopes:

A

O18:O16.

28
Q

When water evaportes:

A

vapor contains slightly less O18.

29
Q

As ice sheets grow, O18:

A

increases in ocean water, decreases in continental ice sheets.

30
Q

O18 is heavier

A

land rain is O16 enriched.

31
Q

Cycles of climate change:

A

isotopes record many glacial and interglacial intervals in last 2Ma. Dominant period in last 800000 years is 100000 years.

32
Q

Earlier glaciations:

A

late paleozoic, late proterozioc time

33
Q

Late paleozoic

A

gondwanaland, glacial and interglacial intervals

34
Q

Late proterozoic time

A

difficult to reconstruct, snowball Earth hypothesis

35
Q

Milankovitch cycles

A

affect the distribution of solar energy over Earth’s surface. Affect climate: global totals, seasons

36
Q

Causes of Climate change:

A

milankovich cycles, changes in solar energy output, plate tectonics, volcanic events, degassing of sediments, asteroid/comet impact.

37
Q

Plate tectonics:

A

position of continents, redistribution of heat

38
Q

Volcanic Events:

A

short term: dust particles in atmosphere reduce solar energy reaching the ground.
Long term: major volcanic episodes, ash to the atmosphere: cooling effect, carbon dioxide: greenhouse warming effect.

39
Q

Degassing of sediments

A

hydrocarbons, esp methane, trapped in sediments may be released. Gas hydrates on continental margins. Methane burps.

40
Q

Asteroid

A

triggering of the younger dryas cooling by ET impact.