CCP 101 Flashcards
Intergovernmental Panel on Climate Change (IPCC)
- Established (1988) by the World Meteorological Organization (WMO) and the
United Nations Environment Programme (UNEP) - Rigorous and comprehensive scientific and technical assessments and
summaries of existing climatic studies (no original research) - Focuses on human-caused portion of climate change (anthropogenic) -
separate from natural climate change
system
a regularly interacting or interdependent group of items forming a unified whole.
Climate System
highly complex system consisting of five
major components:
* the atmosphere (gases and particles),
* the hydrosphere (liquid water),
* the cryosphere (frozen water),
* the lithosphere (solid earth),
* the biosphere (all forms of life), and
* the interactions among them.
Weather
the state of the atmosphere at
a particular place during a short period of
time
Climate
the average of weather for a given location and season, averaged over a period of time ranging from months to thousands of years, or even longer. A typical timeframe for defining climate
from weather statistics is 30 years.
Climate is influenced by
Latitude (determines annual exposure to sunlight)
Altitude (higher elevations tend to be cooler, & vice versa)
Location, including what’s upwind (ocean vs. lakes vs. plains vs. mountains)
Cloudiness, humidity, & wind (influence temperature & precipitation)
characterizations of climate include
Average conditions for a specific time of the year
Spatial scale being described (local, regional, or global)
Temporal scale (period of interest compared to some baseline period)
state of the climate system
influences the odds that certain types
of weather are more or less likely to
happen.
Climate variability
change in weather patterns due to natural
causes on relatively short to medium time spans (weeks to years). For example, El Niño / La Niña, Artic Oscillation
Climate change
a change in the state of the climate that can be
identified (e.g., by using statistical tests) by changes in the mean and/or the variability of its properties and that persists for an extended period, typically decades or longer. It may result from natural causes, human (anthropogenic) causes, or both.
Global Warming
a long-term increase of the
average annual temperature for the whole earth.
Climate change can
- be an increase or decrease
- refer to many parameters
- be local, regional, or global
Climate change is not
uniform and proportional to the level of
warming.
Energy Balance
the balance between the total energy that enters, leaves, and accumulates within a system (such as Earth’s climate system). Global warming, or global cooling, results from a long-term change in the balance of energy inputs into and outputs from the climate system.
Radiative Forcing
the difference between incoming and outgoing
energy.
Earth’s energy budget
Things that reflect & emit energy to space MINUS things that absorb energy into the system
Climate Forcing
an imposed, natural, or anthropogenic perturbation of the Earth’s energy balance with space (e.g., the sun’s energy output). Ex. sun’s energy output, earth’s orbital mechanics (eccentricity, obliquity, and precession), aerosols (cataclysms), and land use change
Climate Feedback
an interaction in which a perturbation in one
climate quantity causes a change in a second, and the change in the second quantity ultimately leads to an additional change in the first. A negative feedback is one in the changes weaken the initial perturbation; a positive feedback is one in which the changes enhance the initial perturbation. ex. clouds, albedo, and precipitation
Total Solar Irradiance
the amount of solar radiation received outside the earth’s atmosphere on a surface normal
to the incident radiation, and at the earth’s mean distance from the sun. The generally accepted value is 1368 W m-2 with an accuracy of about 0.2%. Variations of a few tenths of a percent are common, usually associated with the passage of sunspots across the solar disk.
Eccentricity
Earth’s orbit around the
Sun grows increasing / decreasingly
egg-shaped over 100K to 400k years
Obliquity
Earth’s axis tilts increasingly
away from and then back toward the
Sun, oscillating on roughly 41,000-year
cycles.
Precession
Earth has a “wobble” in its
spin, which traces out an imaginary
circle in an imaginary plane above it on
roughly 21,000-year cycles.
Albedo
the fraction of solar radiation reflected by a surface or object, often expressed as a percentage. ex. Forest clearing for agriculture generally increases albedo because bare ground reflects more than trees, but the global forcing effect is small.
Greenhouse Effect
the infrared radiative effect of all infrared-absorbing constituents in the atmosphere.