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I don't think there is such a thing as a typical upper boundary height. The idea of both of these variables is to get their values before any (near-)surface processes come into effect (but after things like scattering from clouds), and this seems in line with RDRS stated purpose:

The desired outputs from this system are hourly time series, available on a ∼10 km regular grid of 
the main meteorological variables that are required in order to operate surface and hydrology models: 
near-surface air temperature, near-surface air humidity, surface pressure, wind speed and direction, 
incoming infrared flux at the surface, downward solar flux at the surface, and finally precipitation.

Gasset e…

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wknoben
Apr 16, 2025
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@kasra-keshavarz
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