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Created by
Kathleen moore
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Cards (214)
Disturbance
Fire
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Climatic Variation Within
British Columbia
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Orographic
Precipitation
Precipitation caused by the lifting of
moist air
over
mountains
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National Oceanic and
Atmospheric
Administration (
NOAA
)
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Lodgepole
pine
Regenerates in the
understory
on some dry sites with
low
densities
Produces viable seed by age 5 - 10 years
Serotinous
cones - therefore requires
heat
for
cone
opening
Can form
pyral
climax communities
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Damaging Agents & Potential Hazards
Mountain
pine beetle (
Dendroctonus
ponderosae)
Dwarf
mistletoe
Various
fungi
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Observed presence of mountain pine beetle from
1999
to
2012
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Lodgepole
pine trees killed by mountain pine beetle near
Bonaparte
Lake, BC
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Eighty years of fire exclusion – giant sequoia-mixed conifer forests of
Yosemite National Park
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Impacts of Climate Change in our Region
Wildfires
Insect Outbreaks
Drought
Flooding
Economics
Social
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Ecosystems are constantly
changing
– they are not
static.
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It's the
rate
of
change
that is concerning to us.
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Climate
Long-term
statistics of
climate elements
(such as temperature, pressure, or winds) sustained over several decades or longer
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Precipitation Kamloops
Airport
1951-2012
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Climate
data
Used for
long-term
planning and understanding
trends
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Weather data
Used for
short-term
forecasting and understanding
current
conditions
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Climate change is any systematic change in the
long-term
statistics of climate elements (such as
temperature
, pressure, or winds) sustained over several decades or longer
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Earth coordinate
system
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Climates of the
Earth
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What to believe
Firsthand
experience
Values
Opinion leader
Experts
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Has the
climate
changed in your
lifetime
?
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Does
it
fit in with
your world view
?
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If you believe in unfettered freedom, you might
reject
smoking as dangerous to you and others because it represents
government
control
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Opinion leaders
Joe
Oliver
- Canada's former
finance
minister
Al
Gore
- former
Vice President
of the USA
Buzz
Aldrin
- astronaut
Rush Limbaugh
- talk show host
David Suzuki - environmentalist
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Climate
scientists
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Shortwave radiation
Solar radiation
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Longwave
radiation
Infrared
radiation emitted by the
Earth's
surface and atmosphere
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Net radiation equation
Incoming shortwave radiation -
Outgoing longwave
radiation
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Greenhouse effect
Trapping of
longwave
radiation by
greenhouse
gases in the atmosphere, causing the Earth's surface to warm
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Where does
nearly all the energy driving our climate come from
?
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Joules
Unit of
energy
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Watts
Unit of
power
(energy per time)
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Radiation depends on
temperature
Energy emitted =
T^4
, where T is temperature in
Kelvins
and is emissivity
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Each surface has an
energy budget
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Shortwave radiation (K)
Solar radiation
irradiating on a
surface
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Longwave
radiation (L)
Infrared
radiation emitted by the
Earth's
surface and atmosphere
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Albedo
Measure of how much
shortwave
radiation is reflected by a surface, between 0 and
1
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Albedo
can
vary
considerably
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Shortwave radiation
budget calculation
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Absorptivity
Ability of a surface to absorb
longwave
radiation
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