Abstract

The Stratosphere: Geophysical Mon Copyright 2010 b 10.1029/2009GM Long-term variability and trends in global stratospheric temperature are described, based on radiosonde observations since the 1960s and satellite measurements since 1979. New radiosonde-based data sets are available that include adjustments for instrumental inhomogeneities, and these data show good agreement with satellite measurements in the lower stratosphere. The stratosphere exhibits well-known transient warming linked to large volcanic eruptions, plus long-term cooling with magnitudes ~ 0.5 K/decade in the lower stratosphere to ~ 1.2 K/decade in the upper stratosphere. Observations of stratospheric water vapor are also analyzed, based on satellite measurements for 1993–2010. Observed interannual variability is dominated by the quasi-biennial oscillation, plus a step-like drop after 2001. For the observed satellite record, variability in stratospheric water vapor is closely tied to temperature anomalies near the equatorial cold point tropopause.

Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call