Most of the studies are emphasizing more on the climatological thermal structure over a given location.
As seen in previous sections, the climatological latitudinal-altitudinal structure and seasonal variation of Dw1 from eCMAM30 are in excellent agreement with SABER.
This is followed by the climatological altitudinal-latitudinal structures of the migrating diurnal tide Dw1 and three nonmigrating diurnal tides De3, Dw2, and Ds0 from both datasets.
In this section, we present the climatological altitude-latitude structures of the migrating component Dw1 and three nonmigrating components De3, Dw2, and Ds0 from both eCMAM30 and SABER.
The climatological altitude-latitude structures of the migrating diurnal tide Dw1 and three nonmigrating diurnal tides De3, Dw2, and Ds0 from the eCMAM30 and SABER are generally in very good agreement.
We investigated the role of demographic factors (population size and sex-biased dispersal) and physical features (geographic distance, island size and climatological winds) on patterns of genetic structure and gene flow for two lineages of Greater Antillean bats.
This is in agreement with the earlier climatological study of the middle atmospheric thermal structure over Gadanki, which showed equinoctial maxima at Gadanki (Sivakumar et al. 2003), and over Mt. Abu, summer maximum was reported (Chandra et al. 2005).
The historical city structure was then reconstructed virtually and the climatological measurements for 2010 2013 were fed into the RayMan model to produce thermal comfort information (PET, Physiologically Equivalent Temperature).
It has the purpose of identifying desirable adaptations of structure to meet human comfort needs under specific climatological conditions.
The T profiles of atmPrf2013 are useful for climatological analysis of UTLS, although they may not capture the fine structure of the tropopause because of the smoothing over 500 m.
