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 …

Oceanographic parameters, such as sea surface temperature, surface chlorophyll-a
concentration, sea surface ice concentration, sea surface height, etc., are listed as Essential …

Although Antarctic sea ice is undergoing a slight increase in overall extent, major regional
changes are occurring in its spatio-temporal characteristics (most notably in sea ice …

In tropical forests, leaf phenology—particularly the pronounced dry-season green-up—
strongly regulates biogeochemical cycles of carbon and water fluxes. However …

Landfast sea ice (fast ice) is an important though poorly understood component of the
cryosphere on the Antarctic continental shelf, where it plays a key role in atmosphere–ocean …

This study presents the first continuous, high spatiotemporal resolution time series of
landfast sea ice extent along the East Antarctic coast for the period March 2000–December …

Landfast sea ice (fast ice) is an important component of the Antarctic nearshore marine
environment, where it strongly modulates ice sheet-ocean-atmosphere interactions and …

Variability in dense shelf water formation can potentially impact Antarctic Bottom Water
(AABW) production, a vital component of the global climate system. In East Antarctica, the …

Sea ice leads (fractures) play a critical role in the exchange of mass and energy between the
ocean and atmosphere in the polar regions. The thinning of Arctic sea ice over the last few …

Sea ice leads promote mass and energy exchange between the atmosphere and the Arctic
Ocean. The continuous thinning of sea ice and the enhanced sea ice mobility in the past …