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In recent decades, though, the temperature profile of Alaska's permafrost has drooped.
In the atmosphere, the temperature profile with height determines whether free convection occurs or not.
Terrestrial ectotherms utilize the complex temperature profile of the terrestrial environment to derive warmth.
Figure 2 Typical temperature profile.
Therefore, temperature profile will increase.
(a) Temperature profile and (b) mesh structure.
(a) Temperature profile; (b) current density profile.
(a) Temperature profile of rPHY US417.
The resulting temperature profile was significantly flatter.
a Temperature profile of the Martian North Pole.
Figure 2 Equilibrium temperature profile obtained from GPK-2.
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