Climate change Flashcards

1
Q

Medieval Warming Period case stidy

A

Period in history when temperatures were warmer and thus European cultures flourished

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2
Q

Earth systems science

A

To recognize and perhaps modify the changes we have initiated, we need to understand how the entire Earth works as a system. The discipline, called Earth systems science, seeks to further this understanding by learning how the various components of the system—the atmosphere, oceans, land, and biosphere—are linked on a global scale and interact to affect life on Earth.

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3
Q

Monitoring

A

the regular collection of data for a specific purpose; real-time monitoring refers to collecting these data while a process is actually occurring.

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4
Q

Earth’s climate system,

A

defined as the system consisting of the atmosphere, hydrosphere, land surface, biosphere, and cryosphere (i.e., ice, snow, and frozen ground), which are linked and often interact with each other in complex ways

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5
Q

Climate

A

The characteristic atmospheric condition (weather) at a particular place or region over time periods of seasons, years, or decades.

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6
Q

Hadley cells

A

There are three cells of circulation (called Hadley cells, named after George Hadley, who first described them) in each hemisphere. Simplified, warm air rises at the equator and moves toward the poles, where it sinks after going through cell 2 (see Figure 18.6), and return flow is along the surface toward the equator.

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7
Q

troposphere

A

The lower, active part of the atmosphere, where weather occurs

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8
Q

The instrumental record

A

Starting about 1860, measurements of temperatures have been made at various locations on land and in the oceans

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9
Q

The historical record.

A

A variety of historical records go back several hundred years. Included are people’s written recollections (e.g., books, newspapers, journal articles, personal journals) of the Medieval Warm Period and the Little Ice Age, as well as ships’ logs, travelers’ diaries, and farmers’ crop records.

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10
Q

proxy data

A

refers to data that are not strictly climatic but that can be correlated with climate, such as temperature of the land or sea. Some of the information gathered as proxy data includes natural records of climate variability, as indicated by tree rings, ocean sediments, ice cores, fossil pollen, corals, and carbon-14

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11
Q

dendrochronology

A

Tree ring chronology

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12
Q

Coral reefs

A

consists of corals (and other organisms) that have hard skeletons composed of calcium carbonate (CaCO3) extracted by the corals from the seawater. The calcium carbonate contains isotopes of oxygen, as well as a variety of trace metals, that can be used to estimate the temperature of the water that the coral grew in. Thus, corals are a source of paleo-proxy data that can help us to interpret climate change. Corals may be dated by using several dating techniques, and a chronology of change over time may be constructed.

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13
Q

cosmic rays

A

come from outer space and are a product of the energy from the sun

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14
Q

Global warming

A

Refers to the hypothesis that the mean annual temperature of the lower atmosphere is increasing as a result of burning fossil fuels and emitting greenhouse gases into the atmosphere.

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15
Q

Milankovitch cycles

A

The question that begs to be answered is: Why does climate change? Examination of Figure 18.18 suggests that there are cycles of change lasting 100,000 years, separated by shorter cycles of 20,000 to 40,000 years

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16
Q

Climate forcing

A

an imposed change of Earth’s energy balance

17
Q

Climate sensitivity

A

response of climate to a specific climate forcing after a new equilibrium has been established

18
Q

climate response time

A

the time required for the response to a forcing to occur

19
Q

Global dimming

A

Slight cooling caused by human release of air pollution particles that reflect incoming solar radiation back to space.

20
Q

Glacier

A

a land-bound mass of moving ice

21
Q

firn

A

Glacial ice forms as snow accumulates over a period of years, is compressed from the weight of overlying snow, and recrystallizes as a granular ice known as firn

22
Q

continental glaciers, or ice sheets

A

Glaciers that cover large tracts of land

23
Q

glacial surge

A

rapidly advancing glaciers

24
Q

ground moraine, or till plains

A

composed of till, material carried and deposited by the continental glaciers that completely buried preglacial river valleys

25
Q

outwash

A

material carried away from glaciers by meltwater in streams

26
Q

permafrost

A

Permanently frozen ground

27
Q

continuous permafrost

A

the only ice-free ground is beneath deep lakes or rivers

28
Q

discontinuous permafrost

A

characterized by scattered islands of thawed ground in a predominantly frozen area.

29
Q

loess

A

windblown silt

30
Q

primary loess

A

has been essentially unaltered since being deposited by the wind

31
Q

secondary loess

A

as been reworked and transported a short distance by water or intensely weathered in place

32
Q

hydroconsolidation

A

occurs when the clay films or calcium carbonate cement around the silt grains wash away.

33
Q

positive feedback cycle

A

This explains, in part, why warming at higher latitudes and elevations may exceed other areas

34
Q

El Niño

A

An event during which trade winds weaken or even reverse and the eastern equatorial Pacific Ocean becomes anomalously warm; the westward moving equatorial current weakens or reverses.

35
Q

slip face

A

downward slope of a sanddune

36
Q

dune migration

A

When the wind blows, sand moves up the gentle slope and down the slip face, causing the dune to move in the direction of the wind. The process is known as dune migration.

37
Q

Desertification

A

Conversion of land from a more productive state to one more nearly resembling a desert.

38
Q

saline aquifers

A

Two geologic environments have received considerable attention in this regard. The first is sedimentary rocks that contain salty water. These rocks, known as saline aquifers, are fairly widespread at numerous locations on Earth and have large reservoir capacity with the potential to sequester large amounts of carbon.

39
Q

Abrupt climate change

A

large-scale change in the global climate system that takes place over a few decades or less. Such change is anticipated to persist for at least a few decades and will cause substantial disruptions to both human and natural systems.