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   <subfield code="a">Scaling and correlation of atmospheric acid deposition evolutions</subfield>
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   <subfield code="c">[Jianlin Zhu, Guangming Zeng]</subfield>
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   <subfield code="a">Detrended fluctuation analysis (DFA) and power spectrum density are applied to verify the presence of temporal scaling behavior and long-range persistence (LRP) of weekly hydrogen ion deposition (WHD), NO 3 - and SO 4 2- deposition series in National Atmospheric Deposition Program, USA, for the period 1978-2001. The results show a common scaling behavior for all sites analyzed. Two distinct scaling regions are identified by DFA1, one corresponding to 1 month to 1 year and the other to 1 year to 5 years. The WHD series obey power-law in two temporal regimes respectively with mean DFA1 scaling exponents α 1≈0.68 and α 2≈0.45, implying the presence of LRP in the acid deposition series and there is a tendency for a large deposition event to be followed by another large event, and vice versa. For DFA2-DFA4, however, the annual crossover, which divides the temporal scale into two regimes, disappears gradually with the order q of DFAq increasing, and the two scaling regimes turn to share the same scaling exponent close to α 1. The result indicates that the scaling behavior exits in the two regimes with the same scaling exponent α 1, and LRP prevails during the examined 1-month to 5-years scale. NO 3 - and SO 4 2- deposition evolve the same way as WHD does, implying the pollutants involving in acid deposition may share some prominent mechanism controlling their evolutions. We ascribe the long-range power-law scaling of acid deposition evolutions to the self-organized critical behavior of atmosphere under pollution stress and it should be considered in the trend prediction of acid deposition as an important factor.</subfield>
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