For example, in the southern Weddell Sea so much
sea ice forms during the autumn and winter months that the amount of salt released in the process turns the water around and below the 450,000 km2 Filchner - Ronne Ice Shelf into a massive protective sheath.
Not exact matches
The land bridge
forms during ice ages, when much of the water on the planet becomes part of growing continental glaciers, making the
sea level much lower than it is today,» explained Shapiro.
The upper part of the modern Arctic Ocean is flushed by North Atlantic currents while the Arctic's deep basins are flushed by salty currents
formed during sea ice formation at the surface.
During glaciation, water was taken from the oceans to
form the
ice at high latitudes, thus global
sea level drops by about 120 meters, exposing the continental shelves and
forming land - bridges between land - masses for animals to migrate.
Ice formed during the
Ice Age is being given back to the
sea in our naturally warmer geological period, and man is making matters worse by pouring so much carbon dioxide into the atmosphere that more heat is being trapped within it.
It was
formed as a limestone cave system
during the last
ice age when
sea levels were much lower.
The park covers 140 km ², of which 16 km ² is granite islands,
formed by upwellings of hot magma
during the Tertiary - Cretaceous period some 65 million years ago, then later smoothed by glacial
ice and wave action of the
sea.
Like other
sea - holes or «vertical caves,» the Great Blue Hole in Belize's Lighthouse Reef actually
formed on dry land,
during a past
ice age when the
sea level was a lot lower than it is today.
...
Sea ice, especially
during the sunlit seasons, serves as habitat for an
ice - specific food web (sympagic foodweb)[1] that includes bacteria, viruses, unicellular algae, which often
form chains and filaments, and invertebrates sufficiently small to traverse the brine network.
Sea ice is critical for polar marine ecosystems in at least two important ways: (1) it provides a habitat for photosynthetic algae and nursery ground for invertebrates and fish
during times when the water column does not support phytoplankton growth; and (2) as the
ice melts, releasing organisms into the surface water [3], a shallow mixed layer
forms which fosters large
ice - edge blooms important to the overall productivity of polar
seas.
Most of the first - year
ice formed in the Beaufort and eastern Chukchi
Sea during winter has now been removed by melt.
They generally
form during the winter, blocking the transport of
sea ice from the Lincoln Sea into Baffin B
sea ice from the Lincoln
Sea into Baffin B
Sea into Baffin Bay.
In contrast,
sea ice in 2008 (Fig. 4) has a slightly greater extent than 2007 and not all first - year
sea ice that
formed in winter 2008 melted out
during the summer, providing a basis for
forming second - year
sea ice during winter 2009 and beyond.
If northern Siberia does not heat up, then the necessary depressions may not
form in the northern part of the Urals and the coming melting season could look more like 2007 and 2012 with significant high pressure areas over the
sea ice during summer months.
Sea level has risen as the vast continental glaciers
formed during the last
ice age melted.
Sea ice in Antarctica is quite different as it is
ice which
forms in salt water primarily
during the winter months.
As your references point out,
during summer,
sea -
ice melts and ponds
form, thus the
sea -
ice albedo declines sharply.
Ice bridges are static structures composed of tightly packed sea ice that can form during the course of its flow through a narrow stra
Ice bridges are static structures composed of tightly packed
sea ice that can form during the course of its flow through a narrow stra
ice that can
form during the course of its flow through a narrow strait.