Analysis of the Earth and Environment Lecture 14: The Atmosphere Flashcards

1
Q

Define the atmosphere

A

The envelope of gases surrounding the earth or another planet.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

What is the atmospheric pressure of Earth

A

Atm. Pressure at the surface of
the Earth is ~1013 hPa.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

Describe the composition of Earths atmosphere

A

78% Nitrogen
21% Oxygen
1% other gasses:
-0.93 %argon
-0.04% trace gases (including the greenhouse gases carbon dioxide, methane, nitrous oxide and ozone.)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

What are the four sections of the atmosphere

A

Split into 4 main layers based of Temperature

Troposphere
Stratosphere
Mesosphere
Thermosphere

Troposphere and stratosphere account for 99.9% of mass of atmosphere (almost half concentrated within 6 km of the Earth’s surface).

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

Describe the Troposphere

A

The troposphere is the lowest section. Extends upward 6 - 10 km

We live in this part of atmosphere. Almost all weather takes place here - most clouds found here as 99% of atmospheric water is found here.

As you get higher in the troposphere the temperatures decreases

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

Describe the Stratosphere

A

Extends from top of Troposphere about 50km

The Stratosphere contains the Ozone layer which absorbs high energy UV light converting it into heat. As a result, the higher you go in the Stratosphere the higher the temperature.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Describe the Mesosphere

A

Extends from top of Stratosphere around 80km

Most meteors burn up in this layer

Mesosphere is the coldest layer of the atmosphere (-100 degrees centigrade)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Describe the Thermosphere

A

Highest part of Earth’s atmosphere. Extends to between 500 to 1000km

Temperatures vary from 500 to 2000 degrees centigrade (or higher). However air is so thin up here that is not the same kind of temp experienced at surface.

Aurora occurs in thermosphere, as well as where international space station orbits

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

Define the Barometric law

A

Pressure decreases exponentially with height above the Earth’s surface

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

Describe the atmospheric composition and conditions of Mercury

A

Mercury’s gravity is around a third of that on earth so it cannot retain much of an atmosphere. Solar winds are also a big influence.

42% Oxygen
29% Sodium
22% Hydronium
7% Other gases

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Describe the atmospheric composition and conditions of Mars

A

Temperatures on Mars can reach 35 degrees C. The atmosphere is mainly CO2 so greenhouse effects are there,but with less gravity the volatiles escaped over time ? Now the pressure and concentration of the gas is very low (millibar).

95% Carbon Dioxide
3% Nitrogen
1.5% Argon
0.5% Other gasses

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Describe the atmospheric composition and conditions of Venus

A

Atmospheric pressure on Venus is around 92x that on Earth,mainly CO2,and a temperature of around 480 degrees C. Both are partly due to greenhouse effects.

96% Carbon dioxide
3% Nitrogen
1% Other gasses
Clouds of sulfuric acid

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Describe the origins of Earths atmospheric composition

A
  1. Origins
    In the early years of our planet the atmosphere was composed of H and He: as the primordial disk from planetary formation.
  2. Chemical/Pre-biological
    Atmosphere formed from volcanic outgassing dominated by water vapour,CO2,SO2 and other gases.
  3. Microbial era
    Initial O2 formed through photodissociation, this allowed an ozone layer to be formed, early microbes emitted O2 as waste product.
  4. Biological era
    Simultaneous decrease in atmospheric CO2 and the increase in O2 due to respiration/transpiration processes as life developed.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Define the ionosphere

A

The ionosphere is the very upper part of the atmosphere that is ionized by solar
radiation. This is where the atomic oxidation number comes from.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Describe how radiation interacts with the ionosphere

A

Solar radiation at ultraviolet (UV)and shorter x-ray wavelength are considered ionizing since photons of energy at these frequencies are capable of dislodging an electron from a neutral gas atom or molecule during collision.

At the same time, an opposing process called
recombination begins to take place
in which a free electron is “captured” by a positive ion if it moves close enough to it.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

Describe how radiation reacts with gasses

A

As the gas density increases at lower altitudes,the recombination process accelerates since the gas molecules and ions are closer together.

  • The point of balance between these two processes determines the degree of ionization present at any given time.
  • This is also what is constantly happening with ozone in the atmosphere,it is continually being formed and destroyed,it is the
    balance in that process that is important.
  • CFC are now banned as refrigerant as these chemicals disturb this balance, removing Ozone at altitude. But at ground level,Ozone is a pollutant
17
Q

How is an ozone layer formed

A

The ozone layer is formed when ordinary molecules of oxygen gas (O2 ) in the stratosphere absorb UV radiation from the sun with wavelength <240 nm, which causes them to dissociate into single oxygen atoms.

18
Q

Define the Chapman mechanism

A

A theory for the origin of this ozone layer was proposed in 1930 by a British scientist, Sydney Chapman, and is known as the Chapman
mechanism.

19
Q

Describe the Decomposition of stratospheric Ozone

A

Ozone is a very reactive molecule and is termed a meta-stable molecule

  • isolated molecules will decompose slowly
  • when in contact with a molecule of another gas, it will react quickly.