Antarctic landfast sea ice (fast ice) is stationary sea ice that is attached to the coast,
grounded icebergs, ice shelves, or other protrusions on the continental shelf. Fast ice forms …

The Arctic is warming–fast. Microbes in the Arctic play pivotal roles in feedbacks that magnify
the impacts of Arctic change. Understanding the genome evolution, diversity and dynamics …

The increasing accessibility to navigation and offshore oil exploration brings risks of
hydrocarbon releases in Arctic waters. Bioremediation of hydrocarbons is a promising …

Continuing losses of multi-year sea ice (MYI) across the Arctic are causing first-year sea ice
(FYI) to dominate the Arctic ice pack. Melting FYI provides a strong seasonal pulse of …

Climate change has resulted in an accelerated decline of Arctic sea ice since 2001 resulting
in primary production increases and prolongation of the ice-free season within the Northwest …

Intertidal areas support extensive diatom-rich biofilms. Such microphytobenthic (MPB)
diatoms exude large quantities of extracellular polymeric substances (EPS) comprising …

The cellular exterior that a single-celled microorganism presents to its surroundings marks
its first line of defense against environmental pressures, from energy deprivation, shifts in …

Carbohydrates, originating from marine microorganisms, enter the atmosphere as part of
sea spray aerosol (SSA) and can influence fog and cloud microphysics as cloud …

Diatoms are significant primary producers in sea ice, an ephemeral habitat with steep
vertical gradients of temperature and salinity characterizing the ice matrix environment. To …

We present a holistic examination of tropospheric OH reactivity (OHR) in South Korea using
comprehensive NASA DC-8 airborne measurements collected during the Korea–United …