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Further, the locations of these scintillation events are consistent with the background climatology of the global EFI occurrence for the June solstice months reported by Carter et al. (2013) (see their Fig. 5) and Burke et al. (2004) (see their Fig. 1); post-sunset EPBs are commonly detected over the African and Pacific longitude sectors during this time of year.
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Overall, the zonal mean background temperature climatology is in very good agreement between eCMAM30 and SABER.
First, the daily variability is effectively "superimposed" on top of the background occurrence climatology.
On one side of the "controversy" are credentialed climatologists who publish in reputable, peer-reviewed scientific journals and agree that the planet is warming and that humans are to blame; on the other are fossil-fuel-industry-funded "experts" who tend to have little background in climatology and who publish non-peer-reviewed papers in junk magazines disputing established truths.
The background model of climatology utilized in retrieving GPS-RO profiles and the assumptions of the linear combination between L1 and L2 bending angles may control the apparent diversity between the three GPS-RO profiles in Fig. 12 (Schreiner et al. 2011; Zeng et al. 2016).
Figure 1 Climatology of background temperature (in Kelvin).
The newly nudged eCMAM30 temperature data (from January 1979 to June 2010) is used to study the climatology of background mean temperature and diurnal tides in the stratosphere and MLT region.
In 'Results and discussion' , we present the results, starting with the climatology of eCMAM30 background temperature and its comparison with SABER.
In this paper, we focus on the climatology of the background temperature field and the diurnal tidal components from eCMAM30 and the extent to which they match the equivalent parameter obtained using SABER observations.
The model includes realistic background ozone and water vapour climatologies and a long-term mean stationary planetary wave forcing from Met Office analyses.
Number densities of the background atmosphere are taken from the NRLMSISE-00 climatology.
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