Fig. 2: Stratospheric water vapor anomaly and its contributors averaged over three periods. | Communications Earth & Environment

Fig. 2: Stratospheric water vapor anomaly and its contributors averaged over three periods.

From: Multi-decadal variability controls short-term stratospheric water vapor trends

Fig. 2

SWV anomaly (unit: ppmv) averaged over the first wet decade 1990–1997 (a and d); the dry decade 1998–2009 (b and e) and the second wet decade 2010–2020 (c and f) for SWOOSH (ac) and CLaMS simulations (df). Regions with more than 50% missing values are blanked for SWOOSH. Following the procedure described in the method section and also in Hegglin et al.11 (see their Eq. 2), ∆H2O is decomposed into contributions from changes in H2O entering the stratosphere (gi), circulation changes (jl), changes in methane entering the stratosphere (mo) and the residuum (pr). Black contours in af show anomalies relative to the climatological means (unit: %). The gray contours on gi are the mean age of air (AoA) for each period (unit: year). The red and blue contours on jl are positive and negative anomalies of AoA averaged over each period (unit: year). The magenta thick line indicates the climatological tropopause.

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