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Computational text analysis of emotional expressions related to non-suicidal self-injury in Chinese social media

Qi Zhou
Yue Tang
Guo Zhen Shen
ResearchOpen Access12 Apr 2026
Scientific Reports

P: 1-8
Continental outflow shapes the circum-Antarctic pattern of summertime atmospheric mercury depletion zones

Air flowing out from the Antarctic continent largely determines where summer atmospheric mercury depletion events (AMDEs) occur around Antarctica, making them most common in areas where Antarctic cold, downslope winds meet.

Zhouqing Xie
Fange Yue
Olivier Magand
ResearchOpen Access26 Dec 2025
Nature Communications

Volume: 17, P: 1-12
Marine phytoplankton and sea-ice initiated convection drive spatiotemporal differences in Arctic summertime mercury rebound

This study reveals that phytoplankton-driven dissolved organic matter dynamics, coupled with sea-ice melting induced local convection, govern the spatiotemporal disparities in atmospheric Hg(0) rebound observed during Arctic summer months.

Fange Yue
Hélène Angot
Zhouqing Xie
ResearchOpen Access02 Jul 2025
Nature Communications

Volume: 16, P: 1-13
Oceanic evasion fuels Arctic summertime rebound of atmospheric mercury and drives transport to Arctic terrestrial ecosystems

The Arctic summer mercury (Hg) rebound has been debated for decades. This study uses a process-based model to show sea ice melt drives Hg emissions and increases Hg deposition in Arctic tundra, highlighting its key role in Arctic Hg cycling

Shaojian Huang
Tengfei Yuan
Yanxu Zhang
ResearchOpen Access21 Jan 2025
Nature Communications

Volume: 16, P: 1-14
The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime

Oceanic evasion, which mainly occurs in the Marginal Ice Zone, is the main cause of the summertime maximum of gaseous elemental mercury in the central Arctic Ocean

Fange Yue
Hélène Angot
Zhouqing Xie
ResearchOpen Access14 Aug 2023
Nature Communications

Volume: 14, P: 1-13
A 1500-year record of mercury isotopes in seal feces documents sea ice changes in the Antarctic

The stable mercury isotopic composition of sediments containing seal feces indicates that sea ice cover around the Antarctic Peninsula decreased during a warm period 700–1000 years ago, according to analyses of a 1500-year sediment profile on the Fildes Peninsula, King George Island.

Hongwei Liu
Wang Zheng
Zhouqing Xie
ResearchOpen Access14 Jul 2023
Communications Earth & Environment

Volume: 4, P: 1-10

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Computational text analysis of emotional expressions related to non-suicidal self-injury in Chinese social media

Continental outflow shapes the circum-Antarctic pattern of summertime atmospheric mercury depletion zones

Marine phytoplankton and sea-ice initiated convection drive spatiotemporal differences in Arctic summertime mercury rebound

Oceanic evasion fuels Arctic summertime rebound of atmospheric mercury and drives transport to Arctic terrestrial ecosystems

The Marginal Ice Zone as a dominant source region of atmospheric mercury during central Arctic summertime

A 1500-year record of mercury isotopes in seal feces documents sea ice changes in the Antarctic

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