Abstract:
Ground level vapour (GLV) samples were collected at Roorkee, Uttarakhand, India using two methods: liquid condensation (LC)
at 0 C and cryogenic trap (CT) at 78 C for the period 2009–2011. The study reveals that there is a considerable fluctuation in
stable isotopic composition of GLV throughout the year. The study area receives complex moisture source during different
seasons, which is evident from the moisture flux received during different seasons. The isotopic composition of the GLV in both
methods shows depleted nature during rainout process. CT method shows exact isotopic signature of GLV because of maximum
trapping of air moisture and its condensation, whereas LC method shows depleted or enriched character because of the
prevalence of kinetic and diffusive fractionation. The d value shows that LC method acts as magnifier of the CT method and
clearly shows seasonal effect than the clustered CT method. Hence, to decipher the original isotopic signature of GLV, isotopic
composition of GLVLC can be converted to GLVCT by deriving an empirical relationship with changing season and locations.
Meteorological parameters show varied behaviour with GLVCT and LC because of moisture sources in all seasons. The GLVCT and LC
method shows significant correlation with meteorological parameters when the region is dominated by single moisture source.
The GLVLC method magnifies the correlation with meteorological parameters when the region is influenced by more than one
source. The study shows that the GLVLC methods can be used in place of GLVCT when the objective is to understand the
influence of different moisture sources on GLV. Copyright © 2012 John Wiley & Sons, Ltd.
