Results 161 to 170 of about 3,641 (214)

Massive losses and gains of northern land carbon stocks since the Last Glacial Maximum. [PDF]

Sci Adv
Lindgren A, Kuhry P, Holloway M, Lu Z, Tanski G, Hugelius G.   +5 more
europepmc   +1 more source

Erratum for the Research Article, "Unexpected fish and squid in the central Arctic deep scattering layer" by P. Snoeijs-Leijonmalm <i>et al</i>.

Sci Adv
europepmc   +1 more source

Ice shelves and icebergs - an overview

, 1989
openaire   +1 more source

Some of the next articles are maybe not open access.

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Ice shelves and ice flow

Nature, 1975
New data on the Ross Ice Shelf provide an insight into the importance of the momentum with which an ice stream enters the shelf for the overall velocity field.
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Theory of shallow ice shelves

Continuum Mechanics and Thermodynamics, 1999
zbMATH Open Web Interface contents unavailable due to conflicting licenses.
Weis, M., Greve, R., Hutter, K.
openaire   +2 more sources

The area of ice shelves in Antarctica

Polar Record, 1964
In Polar Record, Vol 11, No 75,1963, p 735, I. A. Suyetova made calculations of the area of Antarctica and of its major ice shelves based on published and unpublished material available up to 1961. Suyetova's estimate of the area of the ice shelves, excluding attached islands and ice rises, is 1–38 × 106 km2.
Mario B. Giovinetto, John C. Behrendt
openaire   +1 more source

Flow Law for Antarctic Ice Shelves

Nature Physical Science, 1971
ICE shelves are floating glaciers which are attached to an inland ice sheet or to land. They creep under their own weight, the creep rates being dependent on the ice flow law at low stresses.
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On meltwater under ice shelves

Journal of Geophysical Research: Oceans, 1995
The basic features of the flow of meltwater under ice shelves can be described by a set of simple relations and length scales. The flow may be divided into two regions, with different basic processes dominating in each. In the first region, melting of the underside of the ice shelf is important and the temperature and salinity of the current tend ...
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The Flow of Ice Sheets and Ice Shelves

1993
A brief survey of the mathematical and numerical modelling of ice sheet and ice shelf flows is presented, emphasising the developments over the last decade. For the very slow gravity driven flow of natural ice masses over time scales of thousands of years, the ice is modelled by an incompressible non-linearly viscous fluid with a temperature dependent ...
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Asymptotic Theories of Ice Sheets and Ice Shelves

2007
In climate dynamics of the Globe the atmosphere, hydrosphere and cryosphere interplay with one another with various different time scales, typically from years to several millennia. Ice sheets and ice shelves, which are the grounded and floating components of the large ice masses such as Greenland and Antarctica and the former Fennoscandinavian and ...
D.R. Baral, K. Hutter
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