Lecture 11 - A World of Changing Environments Flashcards

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1
Q

What is the Definition of Weather?

A

-The atmospheric conditions of any place for a short period of time (temporary changes in the climate)

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2
Q

What is the Definition of Climate?

A

-Average of the day-to-day weather conditions over a long period of time (usually at least 30 years)

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3
Q

What Factors define a System?

A

-Have a structure/ organisation
-Are generalisation of the world
-Facilitate the flow of energy/ material
-Show functional and structural relationships between their components

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4
Q

What are the Different types of Systems?

A

-Open system = allows flow of mass/ energy through a boundary
-Closed system = allows energy but NOT mass to flow through a boundary
-Isolated system = allows no mass or energy to flow through a boundary

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5
Q

What are Couplings?

A

-Positive = and increase causes an increase
-Negative = an increase causes a decrease and vice versa

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6
Q

What are Feedback Loops?

A

-Positive = disturbances are amplified (they are usually unstable)
-Negative = tend to diminish the effect of disturbances (normally stable)

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7
Q

What is meant by Equilibrium?

A

-A state of balance in a system due to an external action of opposing forces (represented by a negative feedback loop or a stable relationship)

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8
Q

Explain the Atmosphere’s Role in the Climate

A

-46% of solar radiation is absorbed by the Earth’s surface
-23% absorbed on the atmosphere by water vapour and clouds (lower altitude) and by ozone at higher altitudes
-It acts as a radiative blanket hindering the loss of heat to space

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9
Q

Describe the Troposphere

A

-Vertical and horizontal mixing is common and there is a highly variable water vapour content
-This is the lowest boundary/ the planetary boundary

-The highest point is the tropopause:
-main jet streams here
-height varies controlled by
surface energy exchange
-Highest at equator (17km) and
lowest at poles (9km)

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10
Q

Describe the Stratosphere

A

-8-17-50km
-Temperature remains fairly constant with low mixing
-Temperature can increase due to stratospheric thermal inversion
-Ozone is 320ppb here compared to only 34 in the troposphere
-This ozone heats this layer as it absorbs energy from incoming UV radiation

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11
Q

Describe the Mesosphere

A

-50-80km
-Temperature here decreases with altitude
-75C to -90C (coldest layer in the atmosphere)
-Mesopause separates the mesosphere from the thermosphere
-Also separates the homosphere (where gasses are well mixed) from the heterosphere (where gasses start separating by mass)

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12
Q

Describe the Thermosphere and Exosphere

A

-At around 100km
-Extreme low pressure (<0.0002 hPa)
-Temperature can rise to 100s of C depending on solar radiation
-The exosphere is the uppermost layer and is the transition between interplanetary/ space

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