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The monthly isotopic variations have been used to describe known regional annual cycle of precipitation and atmospheric moisture circulation.
This weaker precipitation could be resulted from the strong coupling between the low-level moisture circulation and precipitation, which is enhanced by adding the shallow convection.
The internal design of the bioreactors was shown to produce different air and moisture circulation patterns within the bioreactor compost-sample mix.
The stable isotope data provide a tool for groundwater recharge studies while the isotopic correlation with regional rainfall cycle demonstrate their use as markers of moisture circulation and detecting climatic changes in precipitation.
They are also useful in climatological studies including the study of atmospheric moisture circulation (Njitchoua et al. 1999; Taupin et al. 2000; Bony et al. 2008; Risi et al. 2008).
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The sea ice reductions also result in increased transfer of energy between the ocean and atmosphere, a decreased strength of the Arctic atmospheric temperature inversion, and increased evaporation, with consequences to atmospheric moisture, atmospheric circulation, and precipitation [e.g., Screen et al., 2013; Vihma, 2014].
In this model, the only prognostic variable is moisture anomaly; the circulation is a passive Gill-like (Gill 1980) response.
Reconstructing topography of our planet not only advances our knowledge of the geodynamic processes that shape the Earth's surface; equally important it adds a key element towards understanding long-term continental moisture transport, atmospheric circulation and the distribution of biomes and biodiversity.
To avoid problems with moisture and air circulation, you should place a sill gasket before installing the sill.
The rates of evaporation and precipitation depend on solar energy, as do the patterns of circulation of moisture in the air and currents in the ocean.
Since the 1980s when rainfall measurements began in the west Greenland town of Kangerlussuaq, the focus of the study, the proportion of precipitation now falling as rainfall rather than snow has both increased and extended into the late summer and autumn in line with increased circulation and moisture availability within a warmer, more energetic atmosphere.
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