1er Parcial Flashcards

Earth system, weather and climate, elements of climate, greenhouse, footprints (50 cards)

1
Q

The five components of Earth system.

A
Atmosphere
Hydrosphere
Cryosphere
Geosphere
Biosphere
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2
Q

The gaseous layer surrounding Earth, composed of 78% nitrogen, 21% oxygen, 1% other gases (0.35% CO2)

A

ATMOSPHERE

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3
Q

The atmosphere layers

A
TROPOSPHERE
STRATOSPHERE
MESOSPHERE
THERMOSPHERE
EXOSPHERE
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4
Q

Atmosphere layer where wind, climate and life exist, its temperature is about 20ºC

A

TROPOSPHERE

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5
Q

Atmosphere layer where it is located the Ozone layer. Its temperature is about -30ºC

A

STRATOSPHERE

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6
Q

Atmosphere layer where meteors burn and it iss seen the Aurora Borealis.

A

MESOSPHERE

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7
Q

Atmosphere functions

A

1) Contains oxygen for humans and used for photosynthesis.
2) Filters solar rays
3) Regulates nature cycles: carbon, nitrogen, water
4) Retain heat through greenhouse

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8
Q

Earth system component that involves the water on Earth.

A

HYDROSPHERE

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9
Q

Percentage of water on Earth

A

97% sea salty

3% fresh

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10
Q

Hydrosphere functions

A

1) Regulate heat (high heat storage capacity)
2) Regulate micro weather at coastal areas
3) Regulate soil erosion

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11
Q

Earth system component that involves frozen water covering 10% surface of the planet.

A

CRYOSPHERE

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12
Q

Sources of frozen water

A

SNOW, POLAR CAPS, ICEBERGS, GLACIERS, PERMAFROST

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13
Q

Cryosphere functions

A

1) Heat storage

2) Avoid Earth from overheating, white color reflects part of the sunlight.

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14
Q

Earth system component made up by thin layers of solid ruck crust and a molten interior.

A

GEOSPHERE

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15
Q

Layer of the Earth where life exists. Heights up to 10km above sea level, marine depth over 8km deep.

A

BIOSPHERE

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16
Q

The continuous flow of carbon going in and out of the atmosphere.

A

CARBON CYCLE

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17
Q

Mechanisms that remove carbon from the atmosphere.

A

CARBON SINKS

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18
Q

Main carbon sinks:

A

Oil deposits of decay organic matter (past)

Oceans, growing forests.

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19
Q

Explain Carbon cycle

A

Plants get CO2 used for respiration and photosynthesis, a part goes into soil and some of it is used for microbial respiration, emitting carbon.
Human factories emit.
There is an exchange in sea, where the amount of carbon used for photosynthesis and respiration is proportional to the one emitted toward the surface of the ocean and to the ocean sediment.

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20
Q

The instantaneous values of atmospheric conditions.

A

WEATHER

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21
Q

List momentaneous values that compose weather.

A

Temperature, humidity, pressure, precipitation, winds, cloudiness.

22
Q

The average weather is called.

23
Q

Three causes of climate change

A

SUNSPOTS CYCLES
VOLCANIC BURSTS
MOLANKOVICH CYCLES

24
Q

Cause of climate change that have reduced concentrations of temperature in the surface of the Sun, caused by magnetic field flux.

A

SUNSPOT CYCLES (10-12 YEARS)

25
The volcanic eruptions have opposite effects on climate change due to...
1. Dust and ash, within sulfure particle COOL DOWN. | 2. Greenhouse gases emitted HEAT UP
26
Milankovich cycle that shows that the Earth orbit around the sun is changing.
ECCENTRICITY (100,000 YEARS)
27
Milankovich cycle that shows a variation in the Earth's axis' inclination.
TILT (41,000 YEARS)
28
Milankovich cycle that shows axis oscillation.
PRECESSION
29
Climate measuring elements
GEODYNAMIC: Temperature, atm pressure, winds ACQUEOUS: Humidity, cloudiness, rainfall
30
Humidity percentages
0-1%: Arctic Circles 1-3%: Mid-latitudes 2-4%: Tropics
31
Why is it warmer at the equator?
Because of the Earth axis tilt.
32
FACT
The less humid the place, the nearer and thinner the clouds
33
Wind types
PERIODICAL: breezes REGULAR: Hayley, Ferrel, polar cells IRREGULAR: hurricanes, tornados, local winds
34
Explain sea and earth breezes (regional)
On the day, Earth warms land, thus the air as well, "lifting" it and then it cools down, so we get that sea breeze. At night, soil cools as does the air, so it "lowes" and periodically gets warmer at sea, rising.
35
Explain montain and valley breezes.
On the day, the air is warmed up, so it is lifted to the mountains to create valleybreezes. At night, the air cools down, so it rushes down through the mountains.
36
Periodic winds work
On SUMMer, the air is warm, and cools down somepoint in the ocean, so it is a cycle, water condenses and precipitates on the coast (RAINY SUMMERS) On WINTER, the air is cool down and warmed up somepoint in the ocean, condensing and leaving the coast without precipitation (DRY WINTERS)
37
Regular winds work
Air is warmer at the equator so it rises and splits to north or south, after it the wind cools down and some of it returns to the equator and the other goes into the opposite side, where it encounters polar winds, rising both again, and determining a cycle. The warmer the air, the more precipitation (less capacity of holding moisture)
38
Forests and Deserts
When air rises, it condenses and happens precipitation; when it cools down, it is dry.
39
Climate factors
``` Sunlight Altitude Latitude Land-water distribution Vegetation Marine currents Wind direction ```
40
Phenomenon whereby certain gases retain part of the energy that emits earth heated by the sun
GREENHOUSE EFFECT (4BILLION YEARS)
41
What is ALBEDO?
The whiter the surface, the more reflective. (1) The darker the surface, the more absorbent. (0) Average albedo: 0.31
42
Greenhouse gases
CO2 (82%), CH4 (9%) -Permafrost N2O (6%) -Fertilizers Fluorinated (3%) -Refrigerants
43
Main sources of CO2 (82%)
- Electricity (38%) - Transportation (32%) - Industry (14%)
44
Main sources of CH4 (9%)
- Natural gas and petroleum system (29%) - Enteric Fermentation (25%) - Landfills (18%)-microbes decoposing
45
Main sources of N20 (6%)
- Agriculture (75%) - Industry or chemical production (6%) - Stationary combustion (5%)
46
Main sources of Fluorinated gases (3%)
-Substitutes for ozone.depleting chemicals (89%)
47
How long do greenhouse gases last?
CO2: 200 years N2O: 110-120 years CH4: 12 years Fluorinated: thousands
48
measure of how much energy the emissions of 1 ton of a gas will absorb over a given period of time, relative to the emissions of 1 ton of carbon dioxide (CO2).
GLOBAL WARMING POTENTIAL (GWP)
49
measure of the impact our activities have on the environment
CARBON FOOTPRINT. | AV: 4,000 KG OF CO2 PER PERSON
50
Is the impact of a person or community on the environment, expressed as the amount of fertile land required to sustain their consumption.
ECOLOGICAL FOOTPRINT