THE EXTRATROPICAL UPPER TROPOSPHERE AND LOWER STRATOSPHERE
By Andrew Gettelman, P. Hoor, L. Pan, William J. Randel, M. Hegglin, T. Birner. 2011
379 citations recorded by the source corpus.
Subfields: Atmospheric Science, Global and Planetary Change
View Paper: https://www.semanticscholar.org/paper/14847df3c00a8e662d06d24a9df3e086ddaea9db
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In Atmospheric Science
In Global and Planetary Change
- P. Konopka
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- Fuqing Zhang
- Riwal Plougonven
- S. Fueglistaler
- Juanzhen Sun
Citations in the corpus
- Horizontal water vapor transport in the lower stratosphere from subtropics to high latitudes during boreal summer (2013, background): “[4] In the extratropical UTLS [e.g., Gettelman et al., 2011], air is a mixture of aged air masses, which have been transported with the stratospheric (Brewer-Dobson) circulation through the deep stratosphere, and of young air masses, which have been transported isentropically from low to high…”
- Internal gravity waves from atmospheric jets and fronts (2014, background): “This may be relevant as the upper-tropospheric jet-stream is indeed just below the tropopause and its sharp jump in stratification [Birner et al., 2002; Gettelman et al., 2011].”