Physical Geography - Atmosphere and Weather

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35 Terms

1

What is the troposphere?

The troposphere is 12 miles thick and contains our weather

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2

What is the tropopause?

The tropopause is the top layer of the troposphere

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3

What are the 6 factors to the daytime energy budget model?

1) Solar radiation (Insolation)

2) Reflected solar radiation (Albedo)

3) Heat transfer into soil (Absorption)

4) Evaporation (Latent Heat Transfer)

5) Sensible heat transfer (Convection)

6) Long wave radiation

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4

What is the simple daytime energy budget equation?

Energy available = solar radiation - (Albedo+ surface absorption + latent heat transfer + sensible heat transfer + long wave radiation)

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5

What Impacts can clouds have on the daytime energy budget?

1) Some clouds allow insolation, some trap long wave radiation

2) Overcast clouds may reflect up to 80% of insolation

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6

Define Latent Heat Transfer

When evaporation occurs allowing heat energy to rise into the atmosphere

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7

Define Sensible Heat Transfer

Heat energy transferred by convection

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8

What are the 6 factors affecting the atmospheric heat budget?

  • Sun spots - can result in less or more energy being received if they are present

  • Distance from the sun

  • Altitude of the sun in the sky - depending upon altitude, there may be a greater surface area to pull over/through

  • The earths obliquity

  • Albedo

  • Greenhouse Effect

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9

What is vertical heat transfer?

Energy is transferred from the warmer surface of the earth vertically by conduction, radiation and convection. Latent heat also helps to transfer the energy

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10

What is horizontal heat transfer?

Around 80% of the heat transferred away from the tropics is carried by winds including jet streams, hurricanes and depressions.

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11

What is the pressure gradient force (PFG)

Air will always move from areas of high pressure to low pressure

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12

What is the Coriolis force

The Earth is spinning in an Easterly motion

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13

What is Ferrels law

Air is deflected to the right in the NH and left in the SH

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14

What are the characteristics in the Equatorial Low Pressure Belt and the Intertropical Convergence Zone

  • Trade winds meet at the ITCZ

  • Winds that are warm will rise

  • Warm air rises, generating latent heat (condensation), convectional rainfall)

  • Weather patterns will include lots of sun and heavy rainfall

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15

What are the characteristics in the Sub-tropical High Pressure Belt and Easterly Trade Winds

  • Cooler dense but dry air return to the ground at 30o N/S and is warmed by the ground, causing hot dry air and deserts form

  • As this is high pressure it will want to return to low pressure forming wind. Due to the Coriolis effect these mostly easterlies, that is they flow towards the west, are known as trade winds

  • Weather is warm with dry mornings and showery afternoons caused by continuous evaporation from tropical seas

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16

What are the characteristics in the temperate Low Pressure Belt and Westerly Winds

  • At 60o air is rising

  • Air moves from subtropical high to temperate low

  • PFG

  • Boundary at 60 is our polar front

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17

What are the characteristics in the Polar High Pressure Belt and Easterly Polar Winds

  • High pressure at poles, cold dense air wants to move from high -> low

  • Polar highs -> temperate lows

  • Winds are coming from the east

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18

What are geostrophic winds?

Geostrophic winds are the upper winds that align themselves with equal pressure (isobars). They are better known as jet streams

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19

What are Rosby waves?

Meanders in the jet streams

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20

What is Gyre?

Rotating current system, driven by CF and winds

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21

What is radiation cooling?

When air loses heat due to long wave radiation from clouds and gasses into the atmosphere

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22

What is conduction cooling?

Leads to condensation when moist air comes into contact with a cold object whose temperature is below the dew point of the air

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23

What is adiabatic cooling?

Occurs when air is forced to rise, it expands due to less pressure and therefore it cools. As air is cooled by the reduction in pressure rather than by a loss of heat to the surrounding air it is said to be adiabatically cooled

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24

How does radiation fog occur?

Radiation fog occurs when the air is so cold that condensation occurs around the condensation Nuclei, often taking place at night or early morning

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25

How does Advection fog occur?

Advection fog occurs when warm air moves over a cold surface it will rapidly cool, meaning the ability to hold water vapour decreases leading to condensation

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26

What is the ELR normal lapse rate?

6.5°C/km

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27

What is the DALR?

10°C/km

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28

What is the SALR?

5°/km

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29

What is the dew point?

10°C

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30

What are the 3 main cloud types?

Stratus → Very low level, mist or fog

Cumulus → Fine weather, if they get bigger they can produce showers

Cirrus → Thin/wispy, high altitudes

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31

What is the eruption theory for global warming?

Volcanic winters (Ash plumes block insolation), Higher volumes of GHGs trap heat

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32

What is the sunspot theory for global warming?

There are darker areas on the suns surface which increase insolation

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33

What is the orbital theory for global warming?

Eccentricity - how circular the earths orbit is

Cycles -> oval like or circular

Oval - closer to the sun at certain types of the year

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34

What is the urban heat island?

The zone above and around and urban area which has higher temps than surrounding rural areas

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35

How can wind change in urban areas?

Wind speeds can be increased in city spaces by the venturi effect, or they can be slowed down by buildings as they increase friction

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