Unit 3 Flashcards

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1
Q

What are the 5 elements of the earth’s climate system?

A
  1. Sun
  2. Atmosphere
  3. Oceans
  4. Water
  5. Land surface
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2
Q

What role does the sun play in defining the earth’s climate system?

A

Solar radiation is the external source of energy that drives the climate system.

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3
Q

What role does the atmosphere play in defining earth’s climate system?

A

The atmosphere has several layers that absorb harmful shortwave radiation, it also regulates earth’s temperature.

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4
Q

What role do the oceans play in defining the earth’s climate system?

A

Covering 70% of the planet’s surface, oceans absorb tremendous amounts of energy and tend to retain and slowly release this heat.

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5
Q

What role does water play in defining the earth’s climate system?

A

Phases of water that include liquid, frozen, and vapor all having distinctive influences on the heat generated or retained at the planet’s surface.

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6
Q

What role does land surface play in defining the earth’s climate?

A

What the surface is covered by (dark vs light colored surfaces) dictates the amount of energy reflected or absorbed.

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7
Q

How does the atmosphere modify incoming radiation from the sun.

A

The atmosphere operates like a window that’s transparent to many of the wavelengths of energy from the electromagnetic spectrum modifying the energy from the Sun. For example, X-rays and gamma rays are not able to penetrate while a small portion of UV and IR can. Visible light and radio waves have properties that allow them to penetrate through the atmosphere.

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8
Q

How do the oceans and land surface influence incoming energy by either reflecting or absorbing energy (based on features of albedo)?

A

Dark surfaces with a low albedo will absorb energy and light surfaces with a high albedo will reflect energy. When energy is absorbed it generates infrared radiation/heat.

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9
Q

How do the 3 phases of water influence how much reflection and absorption takes place?

A

Dark surfaces absorb energy while light surfaces reflect. This means that ice is very reflective and open water will absorb energy. Gases in the atmosphere will absorb and trap heat, that is what water vapor does.

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10
Q

What is the role of the atmosphere in distributing heat around the planet?

A

In atmospheric convection, heating of the ground surface heats the air, producing an updraft of less dense, warm air. There are areas within the atmosphere where warm material is rising in the center and cold material sinking.
The convection process ultimately causes air currents.

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11
Q

What is the role of the oceans in distributing heat around the planet?

A

The ocean conveyor belt operates on the basis of a thermohaline gradient. Cold salty water developed at the Arctic and Antarctic assist to move water and generate a consistent current that transports it into the Atlantic Ocean. It leads to a significant sea to air transfer of heat from the ocean to the atmosphere that is moved toward Europe by prevailing winds.

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12
Q

What is the role of GHG’s (natural and enhanced/human generated) in contributing to the temperature of the planet?

A

GHG’s act as a blanket within the troposphere to absorb, re emit and trap infrared radiation which then heats the planet.

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13
Q

What are examples of positive feedback occurring in the Arctic?

A

With the continual warming that has resulted in loss of sea ice, more energy is being absorbed and retained by the oceans which warms the oceans more which results in a further loss of sea this creates a continuous positive feedback loop.

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14
Q

How has the accelerated loss of sea ice resulted in Arctic amplification today?

A

As sea ice declines, it becomes younger and thinner, and therefore more vulnerable to further melting.

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15
Q

How has sea ice loss in the Arctic contributed to climate change through positive feedback?

A

As the atmosphere warms and sea ice melts, the darker ocean absorbs more heat, causes more ice to melt, and makes the Earth warmer overall.

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16
Q

How has Greenland-based glacial melt in the Arctic contributed to climate change through positive feedback?

A

With massive amounts of glacial melt happening, cold water is entering warmer ocean water and slowing ocean currents. The addition of glacial melt water also contributes to sea levels rising.

17
Q

How has permafrost soil thawing in the Arctic contributed to climate change through positive feedback?

A

Organic matter currently frozen will begin to thaw and decompose releasing trapped methane and carbon dioxide into the atmosphere.

18
Q

What are the 4 levels of the atmosphere and what are their main functions?

A
  1. Thermosphere - Gases in extremely thin air absorb x-rays & shortwave radiation (extends 480km)
  2. Mesosphere - Meteors burn up from friction with air molecules (extends 80km)
  3. Stratosphere - Contains ozone layer that absorbs most of the sun’s UV (extends 50 km)
  4. Troposphere - Weather happens here (storms, turbulent winds, storms & clouds). Air circulation moves heat and energy, redistributing contaminants and concentrating them at higher latitudes. (extends 12km)
19
Q

What is a “heat island”?

A

Cities are generally paved with cement and asphalt that absorb incoming energy from the Sun. It leads to the situation where the temperature is usually warmer than the surrounding rural areas.

20
Q

What is the composition of the atmosphere?

A

78% is nitrogen gas, 21% oxygen and 1% of trace gases.

21
Q

What is the zig zag profile?

A

This refers to the rising and falling of temperatures and how that affects the CO2 levels in the atmosphere. With temperatures falling, CO2 levels rises. As temperatures increase, CO2 levels fall.

22
Q

What is the electromagnetic spectrum?

A

Various wavelengths emitted by the Sun described as shortwave (limited amount of UV reaches earth’s surface and most is blocked by the stratosphere), visible light (drives photosynthesis), and long wave radiation (infrared radiation is generated when energy is absorbed at the surface and represents the outgoing energy).

23
Q

Describe the absorption of energy.

A

70% of radiation is absorbed by the atmosphere and land, this contributes to photosynthesis and generates heat.

24
Q

Describe the reflection of energy.

A

30% of radiation is reflected by the atmosphere and land. Like a mirror, the energy bounces off the surface and is redirected back out to space (this energy does NOT contribute to heating and photosynthesis).

25
Q

What does “albedo” mean?

A

A surface that is light in color reflects more than it absorbs making surfaces like snow, ice, glaciers and icebergs (the cryosphere) very reflective. Highly reflective surfaces are described as having high albedo.

26
Q

What is the relationship of solar intensity and latitude?

A

Due to the features of the tilt and curvature of the planet, more intense energy is received at the equator than at higher latitudes. Seasonal differences are driven by the axis inclination of the planet.

27
Q

Define Albedo.

A

Albedo is the measure of reflectivity of a surface expressed as a percentage.

28
Q

What is thermohaline gradient?

A

Deep-ocean currents are driven by differences in the water’s density, which is controlled by temperature (thermo) and salinity (haline). This process is known as thermohaline circulation.

29
Q

Compare the relative strengths of CFC’s, methane and nitrous oxide in contrast to CO2.

A

GHG’s warming potentials and set CO2 assigned with a value of one.
CH4 is 25x more powerful.
N2O is 300x more powerful.
CFC’s are 5000x more powerful.

30
Q

What is a CFC?

A

Chlorofluorocarbon.

31
Q

Explain how scientists are able to evaluate the geological record of atmospheric conditions with modern measurements. What are the conclusions forthcoming from this evaluation?

A

They use Lake Vostok Antarctic ice core data. Vostok ice cores contain records of atmospheric gas composition. It holds measurements of “fossil” air trapped in bubbles in ice cores. This data concludes that variations in CO2 and CH4 are caused by global temperature change and freeze thaw cycles at high altitudes.