Sem#2 Chap 8 Flashcards
Signs of a stealth disaster:
- Melting glaciers
- Rising sea level
- Hot temperatures
- Frequent, large wildfires
- Devastating floods
- Worsening algal blooms
Future natural disasters will
be more frequent and severe.
Climate change controversy
is partly due to its stealth.
Slow changes are hard to
detect and easily dismissed
All objects emit _________.
electromagnetic radiation
Hotter objects emit ________ wavelengths than cooler objects.
shorter
Earth absorbs sunlight, which is mostly ________.
shortwave radiation
Earth radiates longwave radiation into ______
space
Absorbed energy is balanced with _________
radiated energy
Greenhouse gases absorb Earth’s ________ , radiated energy.
longwave
CO2 is _____ times more efficient at trapping heat than water vapor.
CO2 is 20 times more efficient at trapping heat than water vapor.
- Contributes 9%–30% of the greenhouse effect
CH4 is _____ times more efficient at trapping heat than water vapor.
CH4 is 70 times more efficient at trapping heat than water vapor.
* Contributes 4%–9% of the greenhouse effect
Weather:
atmospheric conditions at a given location and time
Climate:
average weather conditions over years or decades
A region’s climate depends upon:
- Average temperature and temperature range
- Amount and distribution of precipitation
- Seasonal variations in temperature and precipitation
- Characteristic weather extremes and storms
Temperatures at most latitudes vary over _______
a year
Insolation:
the amount of solar energy at a location
Insolation varies due to Earth’s 23.5° tilted axis.
* N. Pole has no insolation in January.
* N. Pole has 24 hours of daylight in June.
Earth has seasons because of its tilted axis
Sunlight intensity varies due
to ______________
Earth’s spherical shape
At low latitudes:
- Steep sunlight angle
- More energy is absorbed
than at high latitudes
At high latitudes:
- Shallow sunlight angle
- Less energy is absorbed than
at low latitudes
Water has a greater ______
capacity than land.
heat
- Temperature change in
oceans is less than on land. - Coasts have less temperature
range than inland locations.
Climate change occurs over ________
decades, centuries, or millennia.
Global warming:
An average increase in global temperature
Global cooling:
An average decrease in global temperature
Paleoclimates:
- Climates that existed before instruments and record keeping
- Scientists use paleoclimate indicators to discern ancient climates.
Class Question #1
How is climate different from weather?
a) Climate is about atmospheric gases such as H2O, CO2, and CH4 and their relative concentrations, while weather is only about H2O concentrations.
b) Climate is about how the atmosphere absorbs electromagnetic radiation, while weather is about how the atmosphere reflects electromagnetic radiation.
c) Climate is about how the atmosphere is in a state of accelerated warming, while weather is about how the atmosphere warms and cools over long periods of time.
d) Climate is about atmospheric conditions over decades or millennia,
while weather is about atmospheric conditions at given location and
time.
(NOT GIVEN) (Probably D)
Fossils:
- Indicate climate as far back as 539 Ma
- Fossilized grass pollen indicates warmer climates.
- Fossilized spruce pollen indicates cooler climates.
Microfossils
are plankton remains in marine sediment.
- Indicate climate as far
back as 66 Ma
Isotopes:
elements with varying numbers of neutrons
* 18O: a heavier oxygen variety
* 16O: a lighter oxygen variety
Climatologists examine ______ and _________.
ice cores and isotope ratios.
Ice with a low 18O/16O ratio
indicates _________.
cooler climates
Ice with a high 18O/16O ratio
indicates _______.
warmer climates
Ice O2 ratios indicate_____
~1 Ma old climates.
Limestone O2 ratios indicate _______
~500 Ma old climates.
Ice cores contain ________
trapped air bubbles.
Air bubbles contain _________.
gases from ancient atmospheres
Gases are identified, and their
_______ ratios measured.
O2
Lab photos of ice cores reveal
annual ________.
snowfall layers
These exhibit annual growth rings:
Trees, clams, and coral reefs
Growth ring width varies
according to:
- Annual temperature
- Annual precipitation
Wide tree rings indicate ________
favorable growing conditions.
* Warm, wet years
Narrow tree rings indicate _________
poor growing conditions.
* Cool, dry years
Composite tree ring records are
made from ________
many trees.
Living, dead, and buried trees
are used for a composite record.
Earth alternates between
_____ and ______ intervals.
warmer and colder intervals.
Hothouse intervals are
__________.
warmer periods
Icehouse intervals are _________.
cooler periods
Temperature anomalies are
comparisons between:
- Temperature at a specific time
- Average temperature over a long time period
Paleocene-Eocene climatic optimum:
- Occurred ~55 Ma
- Average global temperature
was 5°–8°C higher than today
Cenozoic Era extends from
the _______.
present to 66 Ma
Advances of Glaciers:(Where do they move)
glaciers move towards equator
Retreats of Glaciers: (Where do they move)
glaciers move towards poles
An interglacial period is the
time between:
- The end of the last retreat
- The start of the next advance
Pleistocene was (years ago)
2.6 Ma–11,000
years ago.
Pleistocene marine sediment
contains _______
oxygen-isotope ratios.
Pleistocene Ice Age Oxygen-Isotope Ratios
:Record …..
points to numerous glacial advances and retreats.
Causes of Long-Term Climate Change
Greenhouse gases may increase or decrease.
* If CO2 is removed from atmosphere, Earth cools.
* If CO2 is released into atmosphere, Earth warms.
Limestone formation removes CO2.
Volcanic eruptions release CO2.
Tectonic uplift may remove CO2.
Plants and shell-producing organisms remove CO2.
Solar radiation intensity has changed over Earth’s history.
Continents drifting to high latitudes may facilitate cooling.
Variations in ocean currents change heat distribution.
Greenhouse gases may increase or decrease.
- If CO2 is removed from atmosphere, Earth cools.
- If CO2 is released into atmosphere, Earth warms.
Earth’s orbit and tilt change
________.
cyclically
Eccentricity (orbital shape):
- Over 100,000 years, Earth’s
orbital shape changes. - From more circular to more
elliptical
Tilt of the Earth’s axis:
- Over 41,000 years, Earth’s axis tilt changes.
- From 22.5° to 24.5°