Control of interannual and longer‐term variability of stratospheric water vapor

By S. Fueglistaler, P. Haynes. 2005

233 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/0d365fc12fa2e823804693c1cb0a33426ffda160

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Citations in the corpus

Observed poleward expansion of the Hadley circulation since 1979 (2007, background): “, Rosenlof, 2002; Fueglistaler and Haynes 2005). Moreover, Hudson et al. (2006) showed that about 35% of the observed total ozone trend in the Northern Hemisphere since 1979 is due to northward movements of subtropical and polar fronts in the upper troposphere.”
Tropical tropopause layer (2009, background): “The vacillations of equatorial zonal wind associated with the QBO are attenuated below 50 hPa but are still discernible in the upper part of the TTL [e.g., Giorgetta and Bengtsson, 1999; Randel et al., 2000; Fueglistaler and Haynes, 2005].”
Simulation of secular trends in the middle atmosphere, 1950–2003 (2007, background): “, 2004; Fueglistaler and Haynes, 2005]. [64] The effect of ENSO on the simulation of water vapor in WACCM3 is illustrated in Figure 17, which shows the behavior of water vapor anomalies in the tropics from 1950 to 2003 (Figure 17a), and their correlation with the Niño-3.4 (N3.4) index as a function ”
Stratospheric water vapor trends over Boulder, Colorado: Analysis of the 30 year Boulder record (2011, background): “Attempts to connect the 1980–2000 stratospheric water vapor increase over Boulder to changes in tropical tropopause temperatures have been largely unsuccessful [e.g., Simmons et al., 1999; Randel et al., 2000; Zhou et al., 2001; Seidel et al., 2001; Randel et al., 2004; Fueglistaler and Haynes, 200”
Decreases in stratospheric water vapor after 2001: Links to changes in the tropical tropopause and the Brewer‐Dobson circulation (2006, background): “, 2004, hereinafter referred to as R04] and model calculations [Giorgetta and Bengston, 1999; Geller et al., 2002; Fueglistaler and Haynes, 2005].”
The Teleconnection of El Niño Southern Oscillation to the Stratosphere (2019, background): “…measuring stratospheric water vapor (i.e., the events in 1997/1998 and 2015/2016) clearly preceded moistening of the tropical lower stratosphere (Avery et al., 2017; Fueglistaler & Haynes, 2005), though the observed impact of more moderate events is less clear (Garfinkel, Gordon, et al., 2018).”
State of the climate in 2010 (2011, background): “…this large and rapid decrease supports the idea that tropical tropopause temperatures control stratospheric water vapor entry (Randel et al. 2004; Fueglistaler and Haynes 2005; Rosenlof and Reid 2008), trends in tropical cold point temperatures cannot explain the long-term increase in the NH…”
An update of observed stratospheric temperature trends (2009, unknown): “[35] Temperature variations in the tropical lower stratosphere are of special interest because of their influence on stratospheric water vapor [e.g., Randel et al., 2004; Fueglistaler and Haynes, 2005 ].”