Front Back
weather
the day-to-day state of the atmosphere with respect to temperature, precipitation, wind, cloudiness, pressure, etc. variations occur on annual cycle (season) generally controlled by regional changes in atmosphere temperature and moisture conditions Can locally controlled by geogr…
climate
the average prevailing weather conditions of a region throughout the year, averaged over a series of years Variations occur on much longer cycles (decades to tens of thousands of years) Controlled by long-term changes in the atmosphere, hydrosphere, cryosphere, geosphere, and biosph…
Geosphere
all the solid rock material, sediment, and molten rock from the surface down to the core
Atmosphere
envelope of gases held to Earth by gravity, extending 100s of km upward
Hydrosphere
all liquid water at the surface (rivers, lakes, oceans, etc.) as well as groundwater
Cryosphere
all solid ice in the form of glaciers, snowcaps, sea ice, permafrost, etc
Biosphere
all living organism on planet Earth
Anthroposphere
the parts of the environment that are influenced or modified by human activity
proxy data
geologic record shows how global climate has changed throughout time Widespread glacial deposits tell us about ice ages Coal beds tell us about warm, tropical conditions Limestones formed by coral reef environments tell us about warm, shallow seas Evaporites tells us about ari…
Seafloor Sediments
contain fossils that give us give us indication of warm vs. cold water conditions Foraminifera- very sensitive to changing temperatures
oxygen isotopes
18 O (8 p and 8 n) versus 16 O (8 p and 10 n) rations in marine fossils The lighter 16O will evaporate more readily than 18O and become incorporated into atmospheric moisture Both will form in CaCO3 shells and skeletons of marine organisms High 18O = cold Low 18O = Hot
corals
exhibit growth rings similar to trees, contain oxygen isotopes good estimate of water temperature They build their skeletons out of CaCo³ from sea water
ice core records
air bubbles, pollen, dust, volcanic ash in addition to snowfall amounts Air bubbles trap paleo-atmosphere composition of paleo-atmosphere (due to gases and such) dust from meteorites Photosynthetic ice algae: cryophiles
pollen
show vegetation changes in an area dependent on temperature, moisture, altitude, latitude incorporated into sediment or ice by wind or water can determine which species of plants were present
historical documents
written records of events year without a summer (1816 Mt. Tambora erruption in 1815) First frost of the year When crops are ready to harvest Spring thaw Annual flood levels Major droughts Major blizzards
Atmosphere compostion
Nitrogen - 78% Oxygen - 21% Argon - 1% Carbon Dioxide - 398 ppm all others include: neon, helium, methane, krypton, hydrogen
factors that can change absorption or reflection of solar radiation
cloud cover ice cover vegetation volcanic output greenhouse gases sea level aerosols
albedo
The percentage of energy reflected back into space dark materials absorb more heat lighter materials reflect heat energy
positive feedback loop
components amplify each other resulting in runaway effect example: snowball earth
negative feedback loop
components mute each other resulting in equilibrium example: clouds and air temperature
greenhouse gases
gases in the atmosphere that absorb and radiate heat energy from the sun These include water vapor and clouds, CO², methane, N²O, and Ozone Without GHGs, the Earth would be too cold to support life as we know it GHGs in the atmosphere absorb that radiation keeping that heat energ…
tectonic plate positions
equator vs. poles Changes oceanic circulation & heat transfer Changes albedo & potential for glaciation
orbital cycles
Eccentricity, obliquity, precession affect the distribution of solar energy on the earth’s surface Milankovitch cycles - The cycles correspond to major stages as seen from ice core and foraminifera oxygen isotope data over the past million years
volcanic activity
ash, dust, volcanic gases This can reflect solar radiation back into space causing short-term global cooling until the ash and dust settle Periods of abnormally high volcanic activity may result in global warming as more CO2 is emitted Deccan Traps, India Siberian Traps, Russi…
solar activity and sunspots
widely debated hypotheses that sunspot cycles are linked to temperature and precipitation variations Possible, but no concrete evidence to support either.
anthropogenic
relating to, or resulting from the influence of human beings on nature altering climate back to 12,000 years ago, with the Neolithic agricultural revolution clearing forests, domestication of animals, burning wood/fuels
Industrial Revolution
Began in the mid-1700s Switch from burning wood to coal, petroleum, and natural gas burning coal generates unwanted byproducts.. carbon dioxide, methane, nitrogen oxide, sulfur dioxide..

Access the best Study Guides, Lecture Notes and Practice Exams

Login

Join to view and access 3M+ class-specific study document.

or
We will never post anything without your permission.
Don't have an account?
Sign Up

Join to view 2 2 and access 3M+ class-specific study document.

or

By creating an account you agree to our Privacy Policy and Terms Of Use

Already a member?