释义 |
isothermal atmosphere isothermal atmosphere[¦ī·sə¦thər·məl ′at·mə‚sfir] (meteorology) An atmosphere in hydrostatic equilibrium, in which the temperature is constant with height and the pressure decreases exponentially upward. Also known as exponential atmosphere. isothermal atmosphereA standard atmosphere in which the air is assumed to be dry and to have the same standard temperature of 10°C. |