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Approximately 3% of the excretion from pinniped colonies is expected to be volatilized as NH3 into the atmosphere [16], with some of this nitrogen returned to the sea via wet atmospheric deposition.
Over several years, mosses collect and accumulate dry, occult and wet atmospheric deposition.
We present first results on the estimated site coordinates and the zenith total and wet atmospheric delays.
With a WVR, the wet atmospheric delay can be inferred from measurements of the thermal radiation from the sky at a few frequencies.
The application of mosses as biological samplers for dry, occult and wet atmospheric deposition has several advantages: in addition to the long-term accumulation of atmospheric deposition without physiological damages, this method is cost effective and time saving.
This is due to specific properties: Since soil-inhabiting ectohydric moss species do not have real roots and a weakly developed cuticle, grow slow and show minimal morphological changes during lifetime, element concentrations measured in moss integrates fairly well dry, occult and wet atmospheric deposition.
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During dry-, andrage-, and wet-years, atmospheric circulation patterns (i.e., North Atlantic Oscillation and Pacific/North American Pattern) explain more variance than total seasonal precipitation (PRISM), which is not true in the majority of the all-years models.
Wang et al. (2013) conducted a statistical test of the CDAAC atmospheric wet profiles (wetPrf) version 2010.2640.
Wet and dry atmospheric depositions are the major pathway of accumulation of heavy metals in aquatic ecosystems (Öztürk et al. 2009).
Wet and dry atmospheric deposition were investigated from weekly data, 1986–99 (1986–97 for dry deposition) at the Panola Mountain Research Watershed (PMRW), a forested research site 25 km, southeast of Atlanta, Georgia.
In other regions, with a higher number of wet days, an atmospheric Circulation Pattern (CP) based method is likely to lead to further improvements.
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