classify wind based on its spatial extent
Answers
Answer:
i)Homosphere: This layer is extended up to a height of 80 km from
the earth’s surface. In this layer the chemical composition of all the gases is
same. About 99% mass of all the atmospheric elements is confined to this
layer.
ii)Heterosphere: The layer just above the homosphere is known as the
heterosphere. This layer of the atmosphere has created four layers by
nitrogen, helium and hydrogen with respect to their atomic weight. The air
density is too negligible in this layer of the atmosphere.
3. Write with diagram about the layers of the atmosphere based on the
variations in altitude and temperature and write the characteristics of each
layer in brief.
Answer: Based on the variations in altitude, the atmosphere can be divided
into the
following
layers:
i)Troposphere:
It is the lowest
layer of the
atmosphere. It
extends up to a
height of 12 km
from the
earth’s surface.
In this layer,
with the
increase in
altitude,
temperature
decreases.
Here, cloud formation, precipitation etc occurs.
ii)Stratosphere: This zone extends up to a height of 50 km from the
earth’s surface. The main characteristic of this zone is temperature increase
with the increase in height. Moreover, the thin layer of ozone gas which
absorbs the harmful ultraviolet rays of the sun is found in this layer.
iii)Mesosphere: This layer extends up to a height of 30 km from the
stratopause. The main characteristic of this layer is the decrease of air
temperature with the increase in altitude.
iv)Thermosphere: This layer extends up to a height of 400 km from
mesopause. This layer contains electrically charged ion particles. Hence, this
layer is also known as Ionosphere. The radio waves sent from the earth’s
surface are also reflected from this layer.
v)Exosphere: This is the topmost layer of the atmosphere which is
immediately above the thermosphere. This layer extends from a height of
400 km to 10000 km from the earth’s surface. Due to the dominance of only
hydrogen and helium gases, the air of this layer is very thin. The air
temperature at this level of atmosphere rises to about 55500C.
Explanation:
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