Atmospheric water vapour residence time (WVRT) is an essential indicator of how atmospheric dynamics and thermodynamics mediate hydrological cycle responses to climate change. WVRT is also important in estimating moisture sources and sinks, linking evaporation and precipitation across spatial scales. In ...
But the relative rate of increase is slower than that of global mean water vapor content in the atmosphere. Accordingly, the mean residence time of water vapor in the atmosphere becomes longer. In terms of mass flow per unit time, the water cycle accelerates. But in terms of efficiency of ...
Changes in lake level not explained by river flows plus exchanges with the atmosphere must be due to the net difference between what seeps into the lake from the groundwater and what leaks into the groundwater. Note the word "net": measuring the actual amounts of groundwater seepage into ...
Residence time and spatial variability for gases in the atmosphere . Tellus 35B , 295 – 303 .Hamrud, M., Residence time and spatial variability for gases in the atmosphere. Tellus 35B, 295-303, 1983.Hamrud, M. 1983. Residence time and spatial vari- ability for gases in the atmosphere....
However, the residence times of dust in the atmosphere are much shorter than the timescales of mineral weathering in source areas, which likely limits the effect of atmospheric transport on CIA values. Thus, we believe that the variability in dust CIA values shown by samples is probably related...
When discussing the circulation of sulfur and other compounds in the atmosphere, especially in connection with the study of dispersion from an antropogenic source, a fundamental quantity to be considered is the residence time of the compound in the atmosphere. This time-scale is obviously a ...
There is precipitation falling out of the atmosphere. There is evaporation providing water to the atmosphere, and our system is the atmosphere itself, and we'd like to understand something about the residence time of water vapor in the Earth's atmosphere. I can take a balloon with an ...
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Analysis of these data and their comparison with results from experiments on 102Rh suggest that the mean residence time of finely divided aerosols in the atmosphere above 21 km from sources above 100 km is 14 years. Analysis of the 238Pu fallout data indicates that the mean residence time of...
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