8.16.6 Relative Humidity vs Dewpoint

  • Relative Humidity is a relative measurement of how full of water the air is.
  • Dew point is an absolute measurement of how much water the air contains

8.16.12 PHYSICAL STATES OF MOISTURE

  • Gas Condensates to Liquid. Liquid Freezes to solid.
  • Solid Melts to Liquid. Liquid Evaporates to Gas.
  • Solid directly to Gas is Sublimation.
  • Gas directly to Solid is Deposition.

8.16.12 Physical States of Moisture

  • Cooled – Gas Condensates to Liquid. Liquid Freezes to solid.
  • Heated – Solid Melts to Liquid. Liquid Evaporates to Gas.
  • Rapid Heating – Solid directly to Gas is Sublimation.
  • Rapid Cooling – Gas directly to Solid is Deposition.
8.16.12 Describe each of the following processes with regard to the changes of state of water:
(a) condensation;
(b) evaporation;
(c) deposition;
(d) sublimation;
(e) melting;
(f) freezing.

8.24 Atmospheric Moisture to Clouds

Requirements for cloud to form:

  • Saturated Air – Temperature equals Dew Point or below.
  • Condensation Nuclei – Dust, smoke etc.

Lifting Processes:

  • Orthographic – mountains.
  • Frontal Wedging – rising over cool air at fronts.
  • Convergence – two air masses meet
  • Localized lifting – lifting from thermals and rises.

Types of Clouds:

  • Cirrus – High thin wispy clouds.
  • Cumulus – Puffy smaller clouds.
  • Stratus – Layered clouds, sheets.
  • Cirro(prefix) – Added to cloud name, indicates high altitude.
  • Alto(prefix) – Added to cloud name, indicates mid altitude.
  • Nimbo(prefix) – Added to cloud name, indicates dark colour and rain.
8.22.2 Describe the cloud formation process.
8.22.10 Describe the following lifting mechanisms found in the atmosphere:
(a) orographic;
(b) convection (including ‘thermals’);
(c) turbulence;
(d) widespread ascent (including fronts)
8.22.8 Describe the meaning of the following cloud terms:
(a) cumulus or cumulo (prefix);
(b) stratus or strato (prefix);
(c) alto (prefix);
(d) nimbo (prefix) or nimbus (suffix);
(e) cirrus or cirro (prefix).
8.24.4 Describe the following types of precipitation:
(a) rain;
(b) drizzle;
(c) snow;
(d) sleet;
(e) hail

8.6 Why does altitude affect temperature

  • Air pressure decreases with altitude.
  • Each parcel of air increases in size, giving particles more room which is a decrease in temperature.

 

  • Air is warmed by the earths surface. Air will generally cool as it gets further away.
8.10.8 Define ‘pressure lapse rate’

8.8 Energy Transfer In The Earth’s Atmosphere

  • Radiation – The Sun heats Earth’s surface.
  • Conduction – The hot surface warms the air touching it.

Convection

  • Heated air rises. Rising causes the air to cool.
  • Cooled air now sinks.
  • Air is reheated and rises, this cycle repeats.
8.8.12 Describe the transfer of heat in the atmosphere with reference to the processes of:
(a) conduction;
(b) convection;
(c) advection

The history of the barometer

  • Liquid height in the Barometer will decrease until inside and the atmosphere outside both have the same pressure.
  • As atmospheric pressure increases, the height of the liquid increases.
  • The height of the Liquid is measured against a scale, giving us our reading.

8.10.6 AIR PRESSURE vs ALTITUDE

  • Particles in the air are pulled towards the earth due to gravity. This is atmospheric pressure.
  • The higher we are in altitude, the fewer air particles are left above us. Creating less atmospheric pressure.
8.10.2 Define ‘atmospheric pressure’

8.6.2 Where does the atmosphere end?

  • Troposphere – Taller at the equator. 9 – 17 km or 30,000 ft to 60,000 ft tall
  • Stratosphere – 50 km or 150,000 ft tall
8.6.2 Describe the structure of the troposphere and lower stratosphere