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Chapter 3
The Changing Weather
Chapter 3 Terms
Condensation
Orographic Condensation
Precipitation
Weather
Convectional Condensation Air Masses
Frontal Condensation
Continental Artic
High Pressure System
Maritime Tropical
Low Pressure System
Climate
Maritime Polar
Front
Ocean Currents
Gulf Stream
Labrador Current
Weather Radar
Stations
Meteorologists
Radiosonde
Conditions leading to
Condensation
Snow
Snow forms when
water vapour
condenses at a
temperature below
the freezing point
Read pp. 33 - 36
Snow Storm
For a snowstorm to
happen – it needs
two things…
Snow
Wind
Low & High Pressure Systems
Low Pressure System – Air rising over a warm surface
High Pressure System – Cool air sinks towards the surface, pushing the
air underneath away
Why we get wind…
Air over the North and South Poles sink, because it is cold, producing an area of
high pressure
Air over the equator rises because it is hot, producing an area of low pressure
The earth rotates on its axis once every day, so that a point on the equator travels
approximately 40000 km in 24 hours – a velocity of nearly 1700km/hr
Winds in the northern hemisphere blow counterclockwise into a low pressure area
and clockwise out of a high pressure area
An area between high and low pressure feels the effects of both circulations
High winds can develop when areas of very high and very low pressure come close
together
Questions… Page 37 #’s 1 - 4
Factors which affect Climate
Climate – average conditions of temperature
Precipitation – rain, snow, humidity, pressure and wind
Weather – conditions of the atmosphere over a short
period of time
They can all be demonstrated on a climate
graph…
Climate Graph
Consists of…
Temperature – on left of
graph – shown by a line
graph
Precipitation – on right
of graph – shown by a bar
graph
Months of the year – on
bottom of graph
Climate Graph Assignment
Factors which influence the
climate in Atlantic Canada
Latitude – because of the shape of the earth’s surface, there are parts of Atlantic
Canada which receive more intense sunshine than others
Air Masses – affect the climate because they take on the temperature and
humidity characteristics of the areas in which they originate
Ocean Currents – the waters of the world’s oceans are constantly in motion. Tides
move the water up and down while currents move water from place to place. The
major ocean currents have considerable influence on climate.
Proximity to Water – Areas very close to large bodies of water stay cooler in
summer and warmer in winter than areas inland
Elevation – As height increases, temperatures decrease, largely because air is so
much thinner at high altitudes
Read pp. 37 – 41
Questions…Page 42
Examining
Weather
Land & Sea – weather
observers note and
transmit information
about the state of the
atmosphere
From the Air – use radar
to detect, locate and
measure the amount of
precipitation in clouds
From Space – weather
satellites are used to
make long-term weather
forecasts
Weather Radar Station
Read pp. 43 – 45, Questions…Page 46
Read pp. 46 – 47, Questions…Page 48