Unit 6: Atmospheric Systems Flashcards
What is the Atmosphere?
The atmosphere is a dynamic system (with inputs, outputs, flows and storages) that has undergone changes throughout geological time.
How has the Atmosphere changed through Time?
The biotic components of the Earth (living organisms) have transformed the composition of the atmosphere and vice versa throughout geological time.
• E.g. some energy from the sun is absorbed or reflected
What are the Inputs of the Atmospheric System?
- Water from evaporation + transpiration
- CO2, SO4 and NO2 from combustion
- Ammonium from livestock + bacteria
- Volcanic ash
- Solar radiation
- Oxygen from photosynthesis
- CO2 from respiration
- Aerosols
What are the Output of the Atmospheric System?
- Precipitation
- Solar radiation
- Oxygen from respiration
- CO2 from photosynthesis
Give two examples of a transformation inside the Atmospheric System
1) Radiation
2) Evaporation
Give two examples of a transfer inside the Atmospheric System
1) Reflection/scattering
2) Convection
What are the Chemical Components of the Atmosphere?
- Nitrogen (78%)
- Oxygen (21%)
- Argon (0.9%)
- Carbon dioxide (0.03%)
- Water vapor (0.0-4%)
- Other gasses: helium, neon, hydrogen, ozone, hydrogen, krypton, xenon and methane.
What are the Layers of the Atmosphere?
1) Troposphere
2) Stratosphere
3) Mesosphere
4) Thermosphere
5) Exosphere
What is Thermal Stratification?
The division of the atmosphere into a number of layers in terms of temperature variations.
Distinguish between Temperature Lapse and Temperature Inversion
Temperature lapse occurs when there is a decline in temperature with altitude. Temperature inversion occurs when there is an increase in temperature with altitude.
How do Humans impact the Atmospheric System?
Human activities impact atmospheric composition through altering inputs and outputs of the system. Changes in the concentrations of atmospheric gases have significant effects on ecosystems.
What are the two Layers of the Atmosphere mostly affected by Pollutants?
Troposphere and stratosphere
How do Clouds play an important role in Earth’s Albedo Effect?
More water vapour in the atmosphere means more cloud formation = more clouds lead to increased albedo of the earth.
• Clouds block radiation from reaching the ground
• Albedo level: 0.6-0.9 (thick)
What is the Greenhouse Effect?
The greenhouse effect of the atmosphere is a natural and necessary phenomenon maintaining suitable temperatures for living systems. It functions through greenhouse gasses which trap heat energy to maintain earth’s temperature.
What is the Role of Greenhouse Gasses?
Maintaining mean global temperature by allowing radiation (e.g. UV) to pass through to the Earth’s surface, and trapping the longer wavelengths (e.g. infrared).
What are examples of Human Activities that alter Atmospheric Composition?
- Vehicle emissions – fuel combustion
- Dust
- Industrial processes (fossil fuels energy)
- Solvent use
- Fires
- Agriculture
- Waste disposal (+ radioactive waste)
What are some examples of Greenhouse Gasses?
- Carbon dioxide
- Methane
- Water vapor
- Nitrous oxide
What is the Albedo Effect?
Albedo is the ratio of reflected light relative to the amount of incident light hitting the surface. The albedo effect is the scenario in which lighter surfaces reflect more light than darker surfaces.
What are the Values of Albedo? (+ Examples)
Albedo values range from 0 (no reflection) to 1 (100% reflection). Fresh snow has the highest rate of reflectivity whereas fresh water has the least rate.
What is Stratospheric Ozone?
Stratospheric ozone is a gas with the capacity to absorb UV radiation and convert it into heat energy – hence it is essential to protect organisms from harmful radiation.