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Earth and Space Sciences · 术语表

什么是 Standard atmosphere?

Definition 26.1 University Earth and Space Sciences — Year 1 · 第 26 章 — Structure of the Atmosphere and the Ocean

A standard atmosphere is a profile of temperature, pressure and density against height fixed by convention: dry air of constant molar mass, an ideal gas in hydrostatic balance, with given values at sea level and a temperature that varies linearly with height in successive layers. The 1976 standard atmosphere takes 288.15 K288.15\,\mathrm{K} and 101 325 Pa101\,325\,\mathrm{Pa} at sea level, M0=28.9644 kg kmol−1M_0 = 28.9644\,\mathrm{kg}\,\mathrm{kmol}^{-1}, R∗=8314.32 J kmol−1 K−1R^* = 8314.32\,\mathrm{J}\,\mathrm{kmol}^{-1}\,\mathrm{K}^{-1} and g0=9.806 65 m s−2g_0 = 9.806\,65\,\mathrm{m}\,\mathrm{s}^{-2}.

LayerBase (km)dT/dz\mathrm dT/\mathrm dz (K/km)TT at base (K)pp at base (hPa)
1 (troposphere)0−6.5-6.5288.151013.25
2 (stratosphere)110.0216.65226.32
3 (stratosphere)20+1.0+1.0216.6554.75
4 (stratosphere)32+2.8+2.8228.658.68
Table 26.1. The four lowest layers of the 1976 standard atmosphere. The gradients and the sea-level values are defining values; the temperatures and pressures at the bases are computed from them with Proposition 26.2.
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