The phrase "a scale of height" is correct and usable in written English.
It can be used when discussing measurements or comparisons related to height, such as in contexts involving growth, architecture, or physical attributes.
Example: "The architect presented a scale of height for the new building, indicating how it would compare to the surrounding structures."
Alternatives: "a height measurement scale" or "a height range".
Some have racial preferences, a height requirement, a scale of good looks.
The initial spatial distribution is vertically inhomogeneous, since the CN number density function decreases exponentially with a scale height of 2 km above an altitude of 2 km (Khain and Sednev 1996).
The white dashed lines in a,b are the Clausius Clapeyron relationship for near-surface air temperature and PWV from ref. 29, assuming a relative humidity (with respect to liquid) of 100% and a scale height of 3 km.
The black line is the Clausius Clapeyron relationship for near-surface air temperature and PWV following ref. 29 and assuming a relative humidity (with respect to liquid) of 100% and a scale height of 3 km.
The highest convective heat transfer coefficient achieved is 47.9 kW/m2·K, using the FS profile with a scale height of 0.21 mm and scale pitch of 2.1 mm, at Reynolds number of about 4400.
Figure 3 represents a ray tracing simulation of HF propagation in a simplified situation of a single Chapman layer with a maximum density located at 300-km anditude and a scale height of 30 km.
This estimation was based on the assumption of a hydrostatic equilibrium with a scale height of 100 km and that the recorded background to be fully contributed by the resonance fluorescence emission.
In the previous work, the neutral oxygen corona was spherically symmetric like ours, but had a scale height of 1100 km and a manually given O+ photoionization production rate within the simulation box of ~6 ∙ 1023 s−1023
The model that we will consider has an axisymmetrical tabular-shaped low V s heterogeneity that has a maximum anomaly of 3.5 % at the CMB and that exponentially decays upward with a scale height of 500 km (Fig. 9c, bottom right).
The atmospheric pressure on Earth's surface averages 101.325 kPa, with a scale height of about 8.5 km.
