Seasonal variation of water vapor in the lower stratosphere observed in Halogen Occultation Experiment data
By William J. Randel, Fei Wu, Andrew Gettelman, J. Russell, J. Zawodny, S. Oltmans. 2001
164 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/c69c273eb3c6822c92317661e933fc0d4b38add3
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Astronomy and Astrophysics
In Atmospheric Science
- William J. Randel
- S. Fueglistaler
- Douglas E. Kinnison
- Andrew Gettelman
- T. Dunkerton
- P. Konopka
- P. Haynes
- R. Garcia
Citations in the corpus
- Impact of monsoon circulations on the upper troposphere and lower stratosphere (2004, background): “Randel et al. [2001] noted that while similarly high water vapor associated with both Asian and American monsoon circulations (5 parts per million by volume or ppmv), ozone concentrations over the Indian subcontinent and Southeast Asia in July–September (100 parts per billion by volume or ppbv) are”
- Seasonal variation of methane, water vapor, and nitrogen oxides near the tropopause: Satellite observations and model simulations (2004, methodology): “These data have been used to study climatological variability in numerous studies [e.g., Rosenlof et al., 1997; Jackson et al., 1998; Randel et al., 1998, 2001; Beaver and Russell, 1998].”
- Stratospheric water vapor predicted from the Lagrangian temperature history of air entering the stratosphere in the tropics (2005, background): “…to other measurements [World Meteorological Organization, 2000], and their limited vertical resolution of about 2 km could attenuate the observed annual cycle [Randel et al., 2001], although recent model calculations suggest that this effect may be small (B. Randel, personal communication, 2004).”
- Horizontal water vapor transport in the lower stratosphere from subtropics to high latitudes during boreal summer (2013, background): “This aspect may be of importance to the radiative formation of the summer inversion layer [e.g., Randel et al., 2007; Kunz et al., 2009] and requires further attention.”
- Horizontal transport and the dehydration of the stratosphere (2001, unknown): “+ 0 2 2 1 180 2π (1) Dq Dt q q K q z E Cv v v= − − + + −α ∂ ∂ ( ˜) 2 2 (3) Here, (= 6 ppmv) designates the mean subtropical lower stratospheric water vapor mixing ratio [Randel et al., 2001].”