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Overall, the zonal mean background temperature climatology is in very good agreement between eCMAM30 and SABER.
The first step in the model validation is a comparison of the simulated zonal mean background temperature with the observations.
The mean background temperature in the mesosphere is largely determined by the radiative balance between the absorption and emission of solar radiation (Gavrilov and Roble, 1994).
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In order to avoid temperature effects on EC, water temperature during the tests was maintained either within the range of the background test's water temperature or below the mean background water temperature (Hayashi 2004).
The solution makes use of a series expansion and is valid for only low Mach numbers of mean flow and small relative changes in the background temperature.
Before each fitting, the daily zonal mean temperature is de-trended to minimize the aliasing of seasonal variation in background temperature on the migrating tide.
Figure 1 Climatology of background temperature (in Kelvin).
Both CAQ and PAQ were corrected for mean background counts.
General background signal in the GFP channel was corrected by automatic mean background subtraction.
The mean background (blank) MFI was then subtracted, generating netMFI.
Mean, background subtracted fluorescence was averaged for triplicate infections.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com