Examples of atmospheric measurements at several remote and urban sites are presented.
A microwave and RF plasma torch, capacitively coupled, atmospheric pressure plasma, are well-known examples of atmospheric plasma sources[1, 2, 3, 4, 5, 6, 7, 8].
In the United States, for example, removals of atmospheric carbon due to changes in forest product pools are currently on the order of 50 Tg C per year [1, 2].
In the United States, for example, removals of atmospheric carbon due to changes in forest product pools are currently on the order of 50 Tg C per year [ 1, 2].
An example of the atmospheric hollow cathode plasma application for the NOx conversion is given.
This question is investigated for a specific example of dry atmospheric convection, namely the simulation of warm air bubbles.
This paper reports the impacts from the FDNPP accident over approximately 3 years in Tsukuba, Ibaraki (approximately 170 km southwest from the accident site), as a typical example of the atmospheric pollution from the accident.
Calibration can be, for example, in terms of atmospheric pressure or altitude above sea level.
An example of distribution of atmospheric particles showing the relevant and typical properties of DPM.
For example, the rate of atmospheric Pb deposition in the Jura Mountains of Switzerland has been affected appreciably by human activity over the last 2,100 years, with rates of deposition during this period being at least 10 times that of the original natural flux (Shotyk et al. 1998).
