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EARTH'S HEAT BUDGET. The Sun is the star located at the center of our planetary system. It is composed mainly of hydrogen and helium. In the. Sun's interior, a thermonuclear fusion reaction converts the hydrogen into helium releasing huge amounts of energy. The energy created by this reaction is converted into thermal
The Global Energy Budget. •Comments on previous overhead: •31% of the incoming solar radiation is reflected or scattered back to space – the ALBEDO. •235 Wm-2 warms the Earth and atmosphere, 168 Wm-2 of which warms the surface. •235 Wm-2 corresponds to a black body temperature of -19 C, thermal emission at
Increase in ocean temperature should be due to an advection of warm water, or an increase in heat input. • Decrease in temperature should be due to the advection of cooler water or an increase in heat loss. • Hence the change in temperature is due to either advection or net heat input. • The amount of heat into or out
1. Earth's Heat Budget. • The Seasons. • Earth's Heat Budget. • Coriolis Effect. • Ocean and. Atmospheric. Circulation. The Seasons. Draw: 1) Seasons - tilt of axis. 2) Incident Solar Radiation vs. Latitude
Jun 21, 2012 SOLAR RADIATION, HEAT BALANCE. AND TEMPERATURE. Do you feel air around you? Do you know that we live at the bottom of a huge pile of air? We inhale and exhale but we feel the air when it is in motion. It means air in motion is wind. You have already learnt about the fact that earth is surrounded
Print Friendly and PDF. Main Tasks Complete the Task Sheet: The Heat Budget and Insolation - click here to download. Complete this missing word task on 'The Earths Energy Budget' by clicking here. Then print your answers. Prepare a presentation or report that comments on the latitudinal variation of insolation shown in
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2 Earth's Surface Heat Budget. All heat received on earth surface from the sun. Energy falling outside the earth's atmosphere > Solar constant 1368 Wm?2. Figure 2 shows the annual energy balance for the earth-atmosphere system. Less energy is received at the surface because of absorption, scattering, reflection.
CHAPTER 4 • THE ATMOSPHERE, TEMPERATURE, AND THE HEAT BUDGET. 96. Convection currents flow with the boiling water. Conduction heats the metallic pot. Radiation emitted from the pot and boiling H2O. Latent heat of condensation. Water turns to steam. Stove. 0 FIGURE 4.13. Mechanisms of heat transfer.
The Surface Energy Budget. • Determines amount of energy available for evaporation of surface water and to change the surface temperature. • Contributes to overall energy balance of Earth. • More complex than top of the atmosphere energy budget. – Latent and Sensible heat fluxes. • Depends on insolation (incoming
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