Relationships between tropospheric water vapor and surface temperature as observed by radiosondes

Using radiosonde data from 50 stations for 1973–1990, we quantify relationships between surface air temperature (Ts) and precipitable water vapor (W) for different time scales. Monthly mean observations are fairly well described by an equation of the form ln W = A + B Ts, but the coefficients A and B depend on the Ts range considered. At high Ts, the relationship is poor. This relationship and relationships between sea surface temperature (SST) and W based on satellite microwave observations over oceans are in remarkably good agreement over restricted SST ranges. Monthly and annual anomalies of W and Ts are well correlated only outside the tropics, but on longer time scales, there is some evidence of positive trends in both W and Ts at most of the stations studied. Thus the relationship between W and Ts depends on the time scales and geographic region considered.

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