Final Exam Flashcards
1
Q
- Marked climatic changes within recorded history have been caused by a very small change of only a couple of degrees Celsius in average temperature during a period known as “The Little Ice Age”, which ranged from about
A
1,400 A.D. to 1,800 A.D.
2
Q
- The amount of incoming solar radiation absorbed by clouds is
A
4-5%
3
Q
- The amount of incoming solar radiation that is reflected by clouds is
A
4-6%
4
Q
- The amount of incoming solar radiation reflected by Earth’s surface is
A
5%
5
Q
- Much of the outgoing terrestrial infrared radiation is absorbed by
A
water vapor
6
Q
- The reradiated amount back to the surface following the absorption of the outgoing terrestrial infrared radiation is nearly
A
50 per cent
7
Q
- Without the absorption of the outgoing terrestrial infrared radiation by the atmospheric “green house” gases, the average surface temperature would be approximately
A
-18 degrees C
8
Q
- The albedo of Earth, which is the fraction of the incoming solar radiation that goes back into space, including the amounts backscattered by air, reflected by clouds, and reflected by surface, is approximately
A
0.30
9
Q
The principal pollutant of “London”-type fog is
A
sulfur dioxide
10
Q
- Aerosols generally include particles that range in size from a cluster of molecules to
A
about 20 micrometers in radiu
11
Q
- Aerosols with the following composition serve as very effective cloud condensation nuclei
A
halite
12
Q
- A radical atom or a radical molecule is a chemical species that
A
has unpaired electrons
13
Q
- The maximum concentration of ozone in the atmosphere is at an altitude of
A
about 24 to 28 km
14
Q
- Other than destruction by photolysis, ozone in the stratosphere is also destroyed at a significant rate by the reaction with
A
nitric oxide
15
Q
- Which one of the following is considered to be probably the most important atmospheric “scavenger” for removal of a large number of atmospheric pollutants, such as carbon monoxide (CO), methane (CH4)
A
OH• (or hydroxyl radical),
16
Q
- The primary production of hydroxyl radical (OH•) in the troposphere is by
A
the ultraviolet dissociation of hydrogen peroxide (H2O2)