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Three "standard" Nolan Pollak (N P) and a modified N P design condensation nucleus (CN) counters were included in the Vienna Workshop on Intercomparison of Condensation Nuclei and Aerosol Particle counters.
The "quality" of the alignment algorithms, i.e. mutual concordance of algorithmic and GS alignments, was analyzed from different points of view; in most cases, alignments based on intercomparison of three-dimensional structures were used as the GS alignments.
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Moreover, these indicators are an improvement tool based on the intercomparison between laboratories (benchmarking).
Based on the intercomparison data, we find an approximate 1-sigma precision of 20% for the emission rates derived from the various SO2 cameras.
This was certainly recognized in the HRDI results referenced above, where the importance of differences in time and space averaging, the short-term variability of tides, mean winds, and other motions, and the presence of non-migrating tides and other longitudinal irregularities on the intercomparison were noted.
A note is presented on specific calculation methods to be adopted for intercomparison and survey analysis of these systems.
Two past scenarios were considered: LIG (~120,000 140,000 years BP), based on Otto-Bliesner et al. [ 88], and LGM (~21,000 years BP), based on Paleoclimate Modelling Intercomparison Project Phase II [ 89] considering the CCSM3 model [ 90].
Results of the recent intercomparison exercises on Irish Sea sediment (IAEA-385) and a mixed fish sample from the Irish and North Seas (IAEA-414) are compared and discussed.
In the framework of the IAVCEI International Association of Volcanologyy and Chemistry of the Earth Interior) intercomparison study on volcanic plume models, we present three-dimensional (3D) numerical simulations carried out with the ASHEE (ASH Equilibrium Eulerian) model.
The ratio of the total deposition over the Japanese land area to the total atmospheric emission was estimated as 20±6%6%, according to the airborne monitoring conducted by the Ministry of Education, Culture, Sports, Science, and Technology, Japan (MEXT 2011), whereas the ratio was calculated as 27 ± 10% based on the multi-model intercomparison by the Science Council of Japan (SCJ 2014).
The analysis of counting and catching errors of both catching and non-catching types of rain intensity (RI) gauges was possible for the first time over a wide variety of measuring principles and instrument design solutions based on the recent Field Intercomparison of Rainfall Intensity Gauges promoted by WMO, the World Meteorological Organisation.
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