Research news on heat flow (earth)

Heat flow (Earth) refers to the conductive and convective transfer of thermal energy from Earth’s interior to its surface, quantified as heat flux (typically in mW/m²). It arises from the decay of radiogenic isotopes (primarily U, Th, K) in the crust and mantle, residual primordial heat from accretion and core formation, and secular cooling of the core. Measured using borehole temperature gradients and thermal conductivity of rocks, terrestrial heat flow constrains models of lithospheric thickness, mantle convection, plate tectonics, and the global energy budget, and is spatially heterogeneous, with elevated values at mid-ocean ridges and volcanic regions and lower values in stable cratons.

Study reveals Hawaiian hotspot is getting hotter

Contrary to conventional geological thinking, the Hawaiian mantle plume has gotten hotter by about 250°C (480°F) over the past 47 million years. This discovery, led by Earth scientists at the University of Hawai'i at Mānoa, ...

Earth's energy imbalance has doubled—here's why that matters

Heat waves across Europe and South Asia have dominated the news recently. But these events are really a surface expression of more fundamental changes affecting our planet: Earth itself is accumulating heat faster than ever ...

How traffic makes cities warmer

More than half the world's population now lives in cities that are often much hotter than their rural surroundings. Roads, buildings and paved surfaces absorb and store heat during the day, then release it slowly after sunset. ...

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