Week 5 Flashcards

1
Q

Layers of the atmosphere (order)

A

Thermosphere
Mesosphere
Stratosphere
Troposphere

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2
Q

Troposphere

A

80% of gasses here; Typically, the temperature drops about6.5° Cwith each increase in altitude of 1 kilometer (about3.6° F per 1,000 feet); the lowest region of the atmosphere, extending from the earth’s surface to a height of about 3.7–6.2 miles (6–10 km), which is the lower boundary of the stratosphere.

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3
Q

lapse rate

A

The rate at which the temperature changes with altitude

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4
Q

stratosphere

A

the layer of the earth’s atmosphere above the troposphere, extending to about 32 miles (50 km) above the earth’s surface (the lower boundary of the mesosphere).

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5
Q

Stratopause

A

transition space between stratosphere and mesosphere

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6
Q

Mesosphere

A

Air = light; water vapour and ice crystals;
the region of the earth’s atmosphere above the stratosphere and below the thermosphere, between about 30 and 50 miles in altitude

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7
Q

thermosphere

A

Idominization and gamma rays; the region of the atmosphere above the mesosphere and below the height at which the atmosphere ceases to have the properties of a continuous medium. The thermosphere is characterized throughout by an increase in temperature with height

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8
Q

TheMontreal Protocol

A

protocol on Substances that Deplete the Ozone Layer (aprotocolto the Vienna Convention for the Protection of the Ozone Layer) is an international treaty designed to protect the ozone layer by phasing out the production of numerous substances that are responsible for ozone depletion.

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9
Q

Greenhouse Effect

A

is used to describe the role of CO2 and H20 vapour and secondary gases in holding heat within the atmosphere.

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10
Q

Albedo

A

is the measure of diffusive reflection of solar radiation out of the total solar radiation received by a body, for example a planetary body such as Earth; biggest reflect is ice cap because it is white material, asphalt absorbs heat

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11
Q

Anthropogenic

A

(chiefly of environmental pollution and pollutants) originating in human activity.

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12
Q

El Nino

A

is a strong weather event, characterized by unusually warm ocean temperatures in the Equatorial Pacific; dead fish (therma shock) litters the water and beaches of the coasts of Peru and Ecudaor

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13
Q

La Nina

A

is weather events in the Pacific characterized by unusually cold ocean temperatures in the Equatorial Pacific

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14
Q

Drought

A

is a period in which the balance between precipitation and evapotranspiration in an area results in less water.

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15
Q

Evapotranspiration

A

the process by which water is transferred from the land to the atmosphere by evaporation from the soil and other surfaces and by transpiration from plants.

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16
Q

Types of Drought (4)

A

meteorological
hydrological
agricultural
socio-economic

17
Q

Meteorological Drought

A

Drought can be defined simply as a deviation below normal precipitation for a considerable period of time; triggered by climate variation in any particular area

18
Q

Hydrological Drought

A

Rivers, lake will dwindle over time as a result of prolonged drought; effects fish populations; high concentration in the shallow water and heat is not being evaporated lack of oxygen fish dying

19
Q

Ogallala aquifer

A

is a shallow water table aquifer surrounded by sand, silt, clay and gravel located beneath the Great Plains in the United States.

20
Q

Safe Aquifer Yield

A

Managing water withdrawals fromaquifersso as to not exceed “safe yields” is an emerging water supply issue.Safe yieldis the amount of water that can be withdrawn from anaquiferwithout significant ecological impacts.

21
Q

Agricultural drought

A

Depends on the moisture condition of soil, time of the year and the type of farm crops that are cultivated

22
Q

Palmer Drought Index

A

used to measure agricultural drought measure the relationship/ratio bw current moisture in soil and avg moisture of soil over time

23
Q

Aridification

A

long term drying up of an area as a result of climate change;is the process of a region becoming increasingly dry. It refers to long term change rather than seasonal variation. It is often measured as the reduction of average soil moisture content.

24
Q

Desertification

A

gradual increase by barring; the process by which fertile land becomes desert, typically as a result of drought, deforestation, or inappropriate agriculture; potential to drive up indigenous people from the land (eco-migrant)

25
Q

Peachland, BC

A

fire; displacement of 1500 people

26
Q

Crown fires

A

Where fire can easily move up from the ground to the tops of trees it can crown; enable embers to blow downwind causing more fires.

27
Q

How is fireline intensity calculated?

A

The fireline intensity is calculated by the number of kilowatts of energy per square metre along the fireline and estimated by the height of flames.

28
Q

Fire Frequency

A

depends on climate and the type of vegetation

29
Q

Trees adapted to fires

A

Jack Pine, Cork Oak

30
Q

Fire Suppression Methods

A

air tankers, back burns, burnouts

31
Q

Assessing global fire hazards

A

use of remote sensing in fire mapping and assessment, wildfire fuel assessment, wildfire education and assessments; production of priority maps of hazards