Atmosphere Flashcards

(31 cards)

1
Q

Composition of Atmosphere

A

Nitrogen 78%
Oxygen 20%
Other gasses 2%

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2
Q

Troposphere

A
  • between surface & 8 - 18 km
  • Varies in depth -> twice as high over equator (60,000 ft) compared to poles (30,000 ft)
  • First layer of Earth atmosphere - Temp drops w increasing height
  • Contains atmospheres convection, water vapour, weather & clouds
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3
Q

Tropopause

A
  • Temp lapse rate changes
    -> air no longer cools w hight
  • Marks point where convection from
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4
Q

Stratosphere

A
  • Temp starts to increase w hight (gets heated by radiation it absorbs)
  • Very little vertical mixing of air
  • Only clouds found here are TCU or CB
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5
Q

How much water vapour in atmosphere

A

minute traces to 3% of total mass

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6
Q

Stratopause

A
  • Above stratosphere
  • abrupt temp change
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7
Q

Temp lapse rate

A

-2’C / 1000 ft

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8
Q

Pressure lapse rate

A

-1 hPa / 30 ft

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9
Q

Standard atmospheric temp

A

15’C

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10
Q

Standard atmospheric pressure

A

1013 hPa

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11
Q

Whats lighter

Warm air
or
Cold air ?

A

Warm air
-> in atmosphere warm air rises & meets cooler air
-> air keeps rising until same temp as environment around is same temp

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12
Q

Why is the equator hotter ?

A

Given amount of Solar Radiation is spread over smaller area near equator compared to larger amount at poles

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13
Q

How is heat transferred to the lower layers of the atmosphere ?

A

Conduction
-> heated air rises
-> pushes cold air down

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14
Q

What altitude is the Ozone layer ?
What does the Ozone layer do ?

A

50 km above surface

Ozone absorbs large amounts of solar Radiation

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15
Q

What happens with incoming Solar Radiation ?

A
  • Ozone Layer absorbs large amounts
  • Some reflected back into space (Cloud tops)
  • Some scattered by particles in air (giving sky blue colour)
  • Absorbed by land surface
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16
Q

What are the layers of the atmosphere ?

A

Exosphere
- Thermosphere
Mesopause
- Mesosphere
Stratopause
- Stratosphere
Tropopause
- Troposphere

17
Q

What layer of the atmosphere has increasing temp with increasing hight ?

18
Q

Pressure Height Formula

A

ELV + (1013 - QNH) x 30 = PH

19
Q

ISA Temp Formula

A

15 - ( 2 x thousands of ft ) = ISA Temp

20
Q

Density Height formula

A

ISA dev x 120 + PH = Density Hight

21
Q

ISA Deviation Formula

A

Outside temp - ISA Temp = ISA dev

22
Q

Stable atmosphere =

A

Air STOPS rising or sinking on its own

23
Q

Unstable atmosphere =

A

Air CONTINUES to rise & sink on its own

= Greater Environment Lapse Rate
-> Warming of lower levels of environment
-> Cooling of upper levels

24
Q

What effects the stability of the atmosphere ?

A

the way Temp behaves both inside & outside the parcel

The Environmental Lapse Rate determines stability

25
What is an Adiabatic Process ?
one which temp changes without any heat transfer It changes temp through compressing air - Heat is squeezed into smaller volume = hotter Heat expanded into larger volume = colder
26
What is the Dry Adiabatic Lapse Rate (DALR) ?
1) Air rises & cools by expansion -> no cloud forms 2) This expansion causes adiabatic cooling of the parcel Usually -3'C / 1000 ft
27
What is the Saturated Adiabatic Lapse Rate (SALR) ?
1) Air rises & cools -> Cloud forms 2) Latent Heat released 3) Slows down Adiabatic cooling rate - Rate of condensation (release of latent heat) is greatest near cloud base - SALR increases from base -> top of CLD Usually -1.5'C / 1000 ft
28
Conditional Instability
When the ELR is between DALR (3'C/1000ft) & SALR (1.5'C/1000ft) The Atmosphere will be : -> Stable when there is no cloud -> Unstable when there is cloud Unstable for cloud because -> Latent heat released -> reduced cooling of air in cloud -> increasing temp difference between cloud & environmental air
29
What weather does Conditional Instability produce With Cloud = & No Cloud =
With Cloud = TCU & TS No Cloud = mod turbulence
30
If the ELR is below 1.5'C / 1000 ft Is the atmosphere stable or unstable ?
Totally stable
31
What is a high ELR ? What is a low ELR ?
HIGHT = Environment cooling rapidly w hight = unstable LOW = Stable