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Stationary Eddies and Zonal Variations of the Global Hydrological Cycle in a Changing Climate

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Figure 1.1: The general circulation in ERA-Interim reanalysis (1979-2012). a) Zonal-mean zonal wind (colors), potential temperature (contours, interval = 20 K), and tropopause height determined from the 2 K km −1 lapse rate criterion (dark green line)
Figure 2.2: Annual-mean hydrological cycle from ERA-Interim reanalysis. (a, b) Precipitation P (c, d) evaporation E and (e, f) P − E
Figure 2.7: (a,c,e) Moisture budget terms for JJA. (b,d,f) Moisture budget terms for DJF.
Figure 2.8: Dominant terms in the ERA-Interim zonally anomalous vertically-integrated vorticity budget (from surface to 850 mbar) multiplied by [q sfc ] /f such that the stretching term gives the stationary-eddy divergence contribution to P ∗ − E ∗
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Dynamics of stationary-eddy vertical motion Implications for sea surface salinity Changes in zonal variance of net precipitation Connection to Part II Conclusions Estimating gross moist stability Forcing of extratropical Rossby waves Discussion and Conclusions Appendix 6A: Derivation of vertical velocity mode

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