Sentence examples for stratospheric influence from inspiring English sources

The seasonal cycles of tropospheric O3 have been argued as a clue to understanding the contributions from the stratospheric influence and the tropospheric photochemistry.

Because the stratospheric influence generally increases with an increase of altitude, PYR was frequently influenced by STE in spring (Bracci et al. 2012; Cristofanelli et al. 2009a).

"Tropospheric N2O isotopic composition: Instrumentation development and preliminary data for the constraint of the N2O global budget and stratospheric influence" by Kat Potter Pros: A clever and simple idea.

In more recent years, chemistry transport models, evaluated against the seasonal cycles of tropospheric O3, predicted that photochemical production and stratospheric influence were 4974 ± 223 and 556 ± 154 Tg(O3) yearespectivelyively, thereby highlighting the importance of photochemical production of O3 (e.g., Stevenson et al. 2006; Sudo and Akimoto 2007).

Forcings have been prescribed separately and together to assess their individual influence on stratospheric ozone and temperature.

Cristofanelli et al. (2006) investigated the influence of stratospheric intrusion by using 7Be, relative humidity, potential vorticity (PV), and total column O3.

Halocarbons, such as CFC-11, CFC-12 and HCFC-22, are important trace gases in the atmosphere through their role as greenhouse gases and their influence on stratospheric ozone chemistry.

It is increasingly accepted that, in order to produce models which fully include all of those stratospheric processes which can influence weather and climate, the upper altitude ceiling of these models needs to be raised to upper atmospheric heights, so that the geospace processes capable of creating odd hydrogen and odd nitrogen species can be fully included (e.g. Roble 2000, Schmidt et al. 2006).

Based on the aforementioned methods, Cristofanelli et al. (2015) reconstructed the frequency of days influenced by stratospheric intrusion at CMN for the period from 1996 to 2011.

They determined that JFJ was influenced by stratospheric intrusion during 19 and 18%% of the total annual time and by intercontinental transport from North American PBL during 13 and 12 % of the total annual time, as indicated by FLEXPART and LAGRANTO, respectively.

The equatorial electrojet and ionospheric foF2, hmF2 were found to oscillate at periods around 26 27 months, which was attributed to the influence of the stratospheric QBO (Olsen 1994; Kane 1995).