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Growth and Differentiation of Adult Hippocampal Arctic Ground Squirrel Neural Stem Cells
Published on: January 7, 2011
Decadal increase in Arctic dimethylsulfide emission.
Martí Galí1, Emmanuel Devred2, Marcel Babin3,4
1Takuvik Joint International Laboratory (Université Laval), Biology Department, Université Laval, Québec, QC, G1V 0A6, Canada; marti.gali.tapias@gmail.com.
Dimethylsulfide (DMS) emissions from Arctic waters are increasing due to sea-ice loss. This rise in DMS, a key aerosol precursor, could significantly impact Arctic climate and cloud formation.
Area of Science:
- * Atmospheric Chemistry
- * Oceanography
- * Climate Science
Background:
- * Dimethylsulfide (DMS) is a crucial biogenic gas produced by marine microbes.
- * DMS influences aerosol formation, impacting cloud radiative forcing and precipitation.
- * Arctic ecosystems are undergoing rapid changes, necessitating an assessment of DMS emissions.
Purpose of the Study:
- * To quantify trends in summertime pan-Arctic DMS emissions (EDMS) from ice-free waters.
- * To assess the impact of sea-ice retreat on EDMS.
- * To provide constraints for understanding future Arctic climate feedbacks.
Main Methods:
- * Utilized a remote sensing algorithm to analyze summertime EDMS data.
- * Analyzed data north of 70°N between 1998 and 2016.
- * Correlated EDMS trends with sea-ice extent and atmospheric measurements of methane sulfonic acid.
Main Results:
- * Summertime EDMS from ice-free Arctic waters increased by 13.3 ± 6.7 Gg S decade⁻¹ (∼33% decade⁻¹).
- * The observed trend is primarily driven by sea-ice reduction.
- * Extrapolation suggests a potential 2.4-fold increase in EDMS in an ice-free Arctic summer.
Conclusions:
- * Arctic sea-ice retreat is significantly increasing DMS emissions.
- * Future EDMS may deviate from predictions due to ecosystem regime shifts.
- * Increasing DMS emissions and subsequent aerosol-cloud interactions may moderate or accelerate Arctic warming.
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