Earth's energy budget
From Wikipedia, the free encyclopedia
Earth's energy budget or
Earth's radiation balance describes the net flow of energy into
Earth in the form of
shortwave radiation and the outgoing
infrared longwave radiation into
space.
[2] Thus, the energy fluxes are important to understand
climate change, defined by changes in Earth's energy balance.
[3]
http://upload.wikimedia.org/wikipedia/commons/3/3b/NPP_Ceres_Longwave_Radiation.ogv
Received radiation is unevenly distributed over the planet, because the Sun heats equatorial regions more than polar regions. Energy is absorbed by the atmosphere and hydrosphere, known as Earth's heat engine, coupled processes which constantly even out solar heating imbalances through evaporation of surface water, convection, rainfall, winds, and ocean circulation, when distributing heat around the globe. When incoming solar energy is balanced by an equal flow of heat to space, Earth is in
radiative equilibrium and global temperatures become relatively stable.
Disturbances of Earth's radiative equilibrium, such as the rise of
heat-trapping gases, change global temperatures in response, because of the
greenhouse effect, since energy radiated back to space is in part absorbed by greenhouse gas molecules.
[4] However, Earth's energy balance and heat fluxes depend on many factors, such as the atmospheric chemistry composition (mainly aerosols, and greenhouse gases), the
albedo (reflectivity) of surface properties, cloud cover, and vegetation and land use patterns. Changes in surface temperature due to Earth's energy budget do not occur instantaneously, due to the inertia (slow response) of the
oceans and the
cryosphere to react to the new energy budget. The net heat flux is buffered primarily in the
ocean's heat content, until a new equilibrium state is established between incoming and outgoing radiative forcing and climate response.
[5]
...
Earth's energy imbalance
If the incoming energy flux is not equal to the outgoing thermal (infrared) radiation, the result is an energy imbalance, resulting in net heat added to the planet (if the incoming flux is larger than the outgoing). Earth's energy imbalance measurements provided by
Argo floats detected accumulation of
ocean heat content (OHC) in the recent decade. The estimated imbalance is 0.58 ± 0.15 W/m².
[10]
Several
satellites have been launched into Earth's
orbit that indirectly measure the energy absorbed and radiated by Earth, and by inference the energy imbalance. The
NASA Earth Radiation Budget Experiment (ERBE) project involves three such satellites: the
Earth Radiation Budget Satellite (ERBS), launched October 1984; NOAA-9, launched December 1984; and NOAA-10, launched September 1986.
[11]
Today the NASA satellite instruments, provided by CERES, part of the NASA's
Earth Observing System (EOS), are especially designed to measure both solar-reflected and Earth-emitted radiation from the top of the
atmosphere (TOA) to the Earth's surface.
[12]
http://en.wikipedia.org/wiki/Earth's_energy_budget#Earth.27s_energy_imbalance