Chapter 14 Flashcards
Climate Change
an array of changes in aspects of Earth’s climate, such as temperature, precipitation, and the frequency and intensity of storms
Global Warming
an increase in Earth’s average surface temperature; only one aspect of climate change
Solar Radiation
influences climate; sun supplies most of our planet’s energy; Earth;s atmosphere, clouds, land, ice and water together absorb about 70% of incoming solar radiation and reflect the remaining 30% back into space.
Oceans
influences climate by storing and transporting heat and moisture
Earth’s tilt and orbit (MIlankovitch cycles)
variations that alter the way solar radiation is distributed over Earth’s surface; the planet wobbles on its axis, varies in the tilt of its axis and experiences change in the shape of its orbit
Atmospheric Gases and Greenhouse effect
Carbon dioxide, methane, nitrous oxide, hydrochlorofluorocarbon HFC-23; after absorbing radiation emitted from the surface greenhouse gases re-emit infrared radiation; some of this re-emitted energy is lost to space but most travels back downward, warming the lower atmosphere
Anthropogenic Factors affecting climate
greenhouse gases: since the start of the industrial revolution global concentrations of carbon dioxide, methane and nitrous oxide in the atmosphere have increased markedly
Carbon dioxide
human activities send more CO2 from Earth’s surface to its atmosphere than is moving from the atmosphere to the surface (fig 14.4); fossil fuel burning
Methane
concentrations are rising 2.6 fold since 1750; we release methane by tapping into fossil fuel deposits, raising livestock, disposing of organic matter in landfills and growing certain crops such as rice
Nitrous oxide
by-product of feedlots, chemical manufacturing plants, auto emissions and synthetic nitrogen fertilizers; risen by 20% since 1750
Tropospheric ozone
associated with photochemical smog; risen 36% since 1750
Halocarbon gases (CFCs)
begun to slow since the Montreal Protocol and controls on production and use
Land use
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Aerosols
microscopic droplets and particles that can have either a warming or cooling effect; soot particles or “black carbon aerosols” generally cause warming by absorbing solar energy, but most other tropospheric aerosols cool the atmosphere by reflecting the sun’s rays
Surface Albedo
the fraction of solar energy (shortwave radiation) reflected from the Earth back into space. It is a measure of the reflectivity of the earth’s surface
Radiative Forcing
to measure the degree of impact that a given factor exerts on Earth’s temperature; the amount of change in thermal energy that the factor causes
Feedbacks and Uncertainty
.
Proxy Indicators
types of indirect evidence that serve as proxies, or substitutes for direct measurement
Ice cores
ancient atmosphere preserved in ice cores in air bubbles; layers in ice cores provide a time scale; can determine atmospheric composition, greenhouse gas concentrations, temperature, snowfall, solar activity, and frequency of forest fires and volcanic eruptions
Sediment cores
sometimes sediment beneath bodies of water; often preserve pollen grains and other remnants from plants that grew in the past; because climate influences the types of plants that grow in an area knowing what plants were present can tell us a great deal about the climate at the place and time
Tree rings
reveal year-by-year histories of precipitation and fire
Packrat middens
rodent dens in which plant parts may be preserved for centuries in arid regions
Coral reef cores
reveal aspects of ocean chemistry
Direct measurements
tells us about the present