Home > News & Events : News > 2018.02 > Nitrate flux in the Arctic not following the decreasing NOx emissions in neighboring countries

Nitrate flux in the Arctic not following the decreasing NOx emissions in neighboring countries

February 19, 2018

Released on January 23, 2018 (in Japanese)

Hokkaido University
Nagoya University
University of the Ryukyus
Tokyo Institute of Technology
The University of Tokyo
Yamagata University


The camp at Southeastern Greenland Dome for drilling the ice core and its location shown on the map (Collage provided by Shohei Hattori, Tokyo Institute of Technology)

Aerosols less than 2.5 micrometers are known as particulate matter (PM) 2.5 and are hazardous to human health. Large aerosol particles, on the other hand, help form sun-blocking clouds that cool the Earth’s surface. Concentrations of sulfide oxide (SOx) and NOx which can form aerosols were on the rise from the Industrial Revolution of the mid-18th century to 1980, causing serious air pollution in the 1970s and 1980s.

But regulations imposed by the United States, European countries and other developed nations have led to a reduction in SOx and NOx emissions since 1990s. That said, emissions from emerging economies such as China and India have remained high so far.

The team including Yoshinori Iizuka of Hokkaido University and Toshitaka Suzuki of Yamagata University drilled a 90-meter ice core from the Southeastern Greenland Dome, an ice sheet dome in Greenland that has been used for research on atmospheric aerosol depositions in ice cores from 1957 to 2014. The core sample was kept frozen as it was transported to a cold room at the university’s Institute of Low Temperature Science in 2015. Analysis of the ice core began the following year by melting it to measure the concentration of ions such as sulfate and nitrate.

In a previous study, the team succeeded in determining the precise ages of ice core over the six decades with an accuracy of a few months. In the study published in the Journal of Geophysical Research: Atmospheres, they proposed a dating method based on matching oxygen isotope variations between ice core records and simulations using isotope-enabled climate models – the close similarity of which allowed the precise determination of the ages.   > View full press release icon_pdf.png

 

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