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  2. Earth's internal heat budget - Wikipedia

    en.wikipedia.org/wiki/Earth's_internal_heat_budget

    Earth's internal heat budget is fundamental to the thermal history of the Earth. The flow of heat from Earth's interior to the surface is estimated at 47±2 terawatts (TW) [1] and comes from two main sources in roughly equal amounts: the radiogenic heat produced by the radioactive decay of isotopes in the mantle and crust, and the primordial ...

  3. Geothermal gradient - Wikipedia

    en.wikipedia.org/wiki/Geothermal_gradient

    The heat of Earth is replenished by radioactive decay at a rate of 30 TW. [26] The global geothermal flow rates are more than twice the rate of human energy consumption from all primary sources. Global data on heat-flow density are collected and compiled by the International Heat Flow Commission (IHFC) of the IASPEI/IUGG. [27]

  4. Earth's energy budget - Wikipedia

    en.wikipedia.org/wiki/Earth's_energy_budget

    The geothermal heat flow from the Earth's interior is estimated to be 47 terawatts (TW) [12] and split approximately equally between radiogenic heat and heat left over from the Earth's formation. This corresponds to an average flux of 0.087 W/m 2 and represents only 0.027% of Earth's total energy budget at the surface, being dwarfed by the 173 ...

  5. File:Earth Energy Budget with GHE.svg - Wikipedia

    en.wikipedia.org/wiki/File:Earth_Energy_Budget...

    This is why the numbers in the heat flow and energy flow diagrams on the NASA webpage Climate and Earth’s Energy Budget are different. The heat flow numbers are what you are left with after you cancel out opposing radiation energy flows. Q: I've seen the 342 W/m 2 downward thermal radiation flux described as being the greenhouse effect.

  6. Thermal history of Earth - Wikipedia

    en.wikipedia.org/wiki/Thermal_history_of_Earth

    is the surface heat flow [W] at the surface of the Earth (and mantle), = / is the secular cooling heat from the mantle, and , , and are the mass, specific heat, and temperature of the mantle. Q rad {\displaystyle Q_{\text{rad}}} is the radiogenic heat production in the mantle and Q cmb {\displaystyle Q_{\text{cmb}}} is the heat flow from the ...

  7. What is heat index? How hot does it really feel outside? Use ...

    www.aol.com/news/heat-index-hot-does-really...

    That's the heat index. Here's how it works. The temperature on a summer day may be in the 80s or 90s. So why does it feel so much hotter? That's the heat index. Here's how it works.

  8. File:Atmospheric heat flow profile.svg - Wikipedia

    en.wikipedia.org/wiki/File:Atmospheric_heat_flow...

    English: Heat flow profile of Earth's atmosphere, showing (a) radiative cooling and thermal radiation fluxes, (b) non-radiative heat flow, (c) balance of atmospheric heating and cooling, and (d) temperature profile. The figure is intended to support qualitative understanding. Quantitative values may or may not be representative of current-day ...

  9. Mishmash of how US heat deaths are counted complicates ... - AOL

    www.aol.com/news/mishmash-us-heat-death-counted...

    Carla Gates said she's sure heat was a factor in her 66-year-old husband's death, even though she's still waiting for the autopsy report. When Eugene Gates died on June 20, the temperature was 98 ...

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