Premium
Feature extraction of climate variability, seasonality, and long‐term change signals in persistent organic pollutants over the Arctic and the Great Lakes
Author(s) -
Zhao Yuan,
Wang Li,
Huang Tao,
Mo Jingyue,
Zhang Xiaodong,
Gao Hong,
Ma Jianmin
Publication year - 2017
Publication title -
journal of geophysical research: atmospheres
Language(s) - English
Resource type - Journals
eISSN - 2169-8996
pISSN - 2169-897X
DOI - 10.1002/2017jd026937
Subject(s) - north atlantic oscillation , arctic , environmental science , climatology , climate change , arctic oscillation , hexachlorobenzene , pollutant , atlantic multidecadal oscillation , seasonality , the arctic , pacific decadal oscillation , oceanography , sea surface temperature , ecology , geology , biology
We explored the interactions between climate variability and measured persistent organic pollutants (POPs) data in the frequency domain. The spectrum analysis identifies a power period of 1.5 to 7 years in sampled POPs data in the Great Lakes (GL) and Arctic in the 1990s to 2000s, coinciding with the power period of two climate variabilities, the North Atlantic Oscillation and the El Niño–Southern Oscillation. Results also reveal a decadal power period in monitored POPs time series, which is associated with air temperature and climate indices, demonstrating the connection between the dominant long‐term trend in sampled POPs data and climate change. We used a “cocktail party effect” and Fast Independent Component Analysis approaches to blindly separate and isolate the signals in POPs time series from different dynamic and environmental processes in the Arctic and the GL. Among seasonal, interannual, and decadal or longer‐term signals extracted from sampled POPs concentration data, the climate signals in hexachlorobenzene in the GL are associated with air temperature, El Niño–Southern Oscillation indices, and North Atlantic Oscillation (NAO). The signals in α ‐hexachlorocyclohexane (HCH) and polychlorinated biphenyls observations at three Arctic sites correspond to a Niño 3.4 and the NAO. The other two signals are associated with the longer term and seasonal cycle of POPs. We show that the seasonal cycle and climate change are important factors, buffering the declining trend of α ‐HCH. The signals feature extraction from POPs historical data provides a tool to deconstruct the POPs time series and enhance our understanding of the potential effects of climate variations on POPs environmental cycling.