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Related Concept Videos

What is Climate?01:16

What is Climate?

Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Energy Diagrams - II01:10

Energy Diagrams - II

Energy diagrams are important to understand the dynamics of a system. The topology of an energy diagram helps illustrate the equilibrium points of the system.
The point in the energy diagram at which the system’s potential energy is the lowest is known as the local minima. The system tends to stay in this position indefinitely unless acted upon by a net force. The slope of the potential energy diagram at the local minima is zero, indicating that zero net force is acting on the system. The slope...
Variation in Acceleration due to Gravity near the Earth's Surface01:20

Variation in Acceleration due to Gravity near the Earth's Surface

An object's apparent weight is its weight measured by a spring balance at its location. It is different from its true weight, the force with which the Earth pulls it, because of the Earth's rotation. Mathematically, an object's apparent weight equals its true weight minus the centripetal force that keeps it in a circular motion along with the Earth's surface every 24 hours.
The difference between the true and apparent weights is proportional to the square of the Earth's angular speed. Since the...
Energy of a Satellite in a Circular Orbit01:11

Energy of a Satellite in a Circular Orbit

Thousands of artificial satellites orbit the Earth every day at various distances from the Earth. Satellites that orbit the Earth below an altitude of 1,600 km are considered to be orbiting in low-Earth orbit (LEO). Research satellites and Earth observation satellites are usually placed in LEO, and mostly orbit the Earth in elliptical orbits. Navigation satellites are placed in medium-Earth orbit (MEO), ranging from 2,000 km to 36,000 km from the surface of the Earth. Meanwhile, communication...
Radiation: Applications01:17

Radiation: Applications

The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
Conservation of Mechanical Energy01:05

Conservation of Mechanical Energy

The mechanical energy E of a system is the sum of its potential energy U and the kinetic energy K of the objects within it. What happens to this mechanical energy when only conservative forces cause energy transfers within the system—that is, when frictional and drag forces do not act on the objects in the system? Also assume that the system is isolated from its environment; in other words no external force from an object outside the system causes energy changes inside the system.
When a...

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Related Experiment Video

Updated: Jul 8, 2026

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data
09:55

Surface Renewal: An Advanced Micrometeorological Method for Measuring and Processing Field-Scale Energy Flux Density Data

Published on: December 12, 2013

Earth's energy imbalance: confirmation and implications.

James Hansen1, Larissa Nazarenko, Reto Ruedy

  • 1NASA Goddard Institute for Space Studies, New York, NY 10025, USA. jhansen@giss.nasa.gov

Science (New York, N.Y.)
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Earth is absorbing excess solar energy due to greenhouse gases, causing a significant energy imbalance. This indicates future warming and accelerated sea level rise, necessitating proactive climate change mitigation strategies.

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Area of Science:

  • Climate science
  • Earth system science
  • Atmospheric physics

Background:

  • The Earth's energy balance is influenced by greenhouse gases and aerosols.
  • Accurate measurement of energy imbalance is crucial for climate projections.

Purpose of the Study:

  • To quantify the current energy imbalance of the Earth.
  • To project future climate change impacts based on observed energy imbalance.

Main Methods:

  • Utilized a climate model driven by forcings like greenhouse gases and aerosols.
  • Confirmed model calculations with 10 years of ocean heat content measurements.

Main Results:

  • Calculated Earth is absorbing 0.85 +/- 0.15 W/m² more solar energy than it emits.
  • Observed increasing ocean heat content corroborates the calculated energy imbalance.

Conclusions:

  • Projected global warming of 0.6°C without further atmospheric changes.
  • Highlighted the climate system's lag, requiring anticipatory climate action.
  • Indicated accelerated ice sheet disintegration and sea level rise are likely.