Lecture 3: Water in the atmosphere Flashcards

1
Q

Water on earth- my notes

A

Water vapour is different to what makes up a cloud- cloud is liquid water droplets

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2
Q

Phase diagram- my notes

A
  • solid to a gas is sublimation
  • boiling point is not fixed at 100 degrees only at sea level- can change with different atmospheric pressure

Evaporation exceeds condensation- stage 1

  • is a function of temperature
  • rate of evaporation exceeds condensation

Dynamic equilibrium- Stage 2
- evaporation cat go anywhere- therefore water molecules tuns into condensation

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3
Q

Temperature increase- my notes

A
  • more evaporation than condensation
  • evaporation is so dependent on temp
  • Britain in winter- less water vapor- in comparison to the tropics
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4
Q

what is a dew point?- my notes

A

where due will occur

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5
Q

Relative humidity in the home- my notes

A
  • cold air- contains little water vapour
  • were not adding water to the air- were heating – transforming the atmosphere in our home to extreme conditions- plants dry
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6
Q

Clouds - my notes

A
  • smoke particle- is a flat surface
  • increase of temp and pressure
    no such thing as pure water on planet earth
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7
Q

Formation of fog- my notes

A
  • Rapid cooling of the air

- -By adding water vapour from elsewhere

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8
Q

High clouds - my notes

A

Cirrus, cirrostratus and cirrocumulus- so high up – ice crystal – even in the tropics- below 0

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9
Q

Middle clouds - my notes

A

altostratus and altoculmus

-Foggier appearance

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10
Q

Low clouds - my notes

A

Most common in london

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11
Q

Phases of water

A

Water (H2O) is a dipole molecule consisting of one oxygen and two hydrogen atmos. It is an efficient absorber of infrared radiation.
• Water exists on Earth in three phases (or states):
• gasphase(watervapour) • liquidphase(liquidwater) • solidphase(ice)

  • In the gas phase the molecules are moving freely, mixing with other gases. Compressible
  • In the liquid phase molecules still move freely but are constantly bumping and jostling. Liquid water is virtually not compressible.

• When temperatures are lowered the molecules move slower and at temp’s below freezing point the molecules are arranged in grid-like structure, able to vibrate but not to move freely (solid phase)

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12
Q

Phase diagram

A

The Phase Diagram describes the boundaries/limits for the three phases of water as a function of ambient pressure and temperature

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13
Q

LATENT HEAT TRANSFER

A

As ice melts or water evaporates it absorbs heat and the surrounding environment cools in the process
• As water vapour condenses or liquid water freezes to ice it releases heat to the surrounding environment
• The transition between the gaseous and liquid phase involves about seven times as much heat energy as the transition between the liquid and the solid phase
• The energy that is transferred through these phase changes is called “latent heat”

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14
Q

HYDROLOGICAL CYCLE

A

Evaporation: Solar energy transforms liquid water into water vapour
• Transpiration: Moisture given up by plants (in form of water vapour)
• Condensation: Water vapour reverts back to liquid phase (formation of droplets)
• Precipitation: Liquid or solid forms of water falling from clouds (e.g. rain, snow, hail)
• Surface water returns as runoff to the oceans, or it percolates through openings in the
soil into groundwater

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15
Q

EVAPORATION AT ROOM TEMPERATURES

A

Water evaporates not only at boiling point but also at room temperatures.
• The temperature describes the average kinetic energy of a sample of molecules.
• In fact a range of kinetic energies (varying speeds of molecules) are found and they can be represented by a statistical distribution.

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