Results 171 to 180 of about 35,654 (218)

ArcTiCA: Arctic tidal constituents atlas. [PDF]

Sci Data
Hart-Davis MG, Howard SL, Ray RD, Andersen OB, Padman L, Nilsen F, Dettmering D.   +6 more
europepmc   +1 more source

Sea-ice melt determines seasonal phytoplankton dynamics and delimits the habitat of temperate Atlantic taxa as the Arctic Ocean atlantifies. [PDF]

ISME Commun
Oldenburg E, Popa O, Wietz M, von Appen WJ, Torres-Valdes S, Bienhold C, Ebenhöh O, Metfies K.   +7 more
europepmc   +1 more source

Concurrent superimposed ice formation and meltwater runoff on Greenland's ice slabs. [PDF]

Nat Commun
Tedstone A, Machguth H, Clerx N, Jullien N, Picton H, Ducrey J, van As D, Colosio P, Tedesco M, Lhermitte S.   +9 more
europepmc   +1 more source

Administration of 1-kestose to beluga reduces intestinal Turicibacter and collagenase gene levels, and blood creatinine levels.

J Vet Med Sci
Fujii T, Kamio T, Akune Y, Takahashi H, Kondo N, Funasaka K, Ohno E, Hirooka Y, Tochio T.   +8 more
europepmc   +1 more source

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Transport measurements in the arctic ice-pack

Letters in Heat and Mass Transfer, 1980
Abstract The characteristics of the Polar Pack are generally thought to have a large influence on terrestrial weather. Yet the environment of the sea ice and its dynamic response to the seasonal cycle, as well as to gradually changing average conditions, have received little study or transport modelling. A specific measurement program was devised and
Benjamin Gebhart, Tore Audunson
openaire   +2 more sources

Acoustically derived ice-fracture velocity in central Arctic pack ice

The Journal of the Acoustical Society of America, 2000
Sounds radiated by fractures in Arctic ice (called acoustic events) are used to estimate fracture velocity. Both speed and orientation are obtained by measuring Doppler shifts induced by source motion. Data from the SIMI experiment of 1994 in the central Arctic are used in the frequency window 10 to 350 Hz.
Ira Dyer, Catherine Stamoulis
openaire   +3 more sources

Vibrational Motion of Arctic Pack Ice,

1997
Abstract : There are many physical mechanisms responsible for vibrations of sea, and they force motions in a very wide band of frequencies from less than 0.01 Hz to greater than 100 Hz. Detailed measurements of the vertical velocity in this frequency band were previously shown to be produced by gravity waves, ridging events and wind turbulence. In this
John Dugan, William D. Morris, Zandy Williams   +2 more
openaire   +2 more sources

HF radar observations of Arctic pack-ice breakup

IEEE Journal of Oceanic Engineering, 1986
This paper describes the first reported high-resolution remote measurements of sea-ice velocities during the summer Arctic pack-ice breakup, made with a high-frequency (HF) radar system (CODAR, for Coastal Ocean Dynamics Applications Radar) located on Cross Island, Alaska. Each 36-min observation also gives the positions of the ice edge, the moving ice,
B. Lipa, R. Crissman, D. Barrick
openaire   +2 more sources

Upwelling: Oceanic Structure at the Edge of the Arctic Ice Pack in Winter

Science, 1979
Observations taken on an expedition into the Arctic Ocean north of Spitsbergen indicated the existence of a region of wind-driven upwelling along the edge of the ice pack. Models underestimate the 12-kilometer width of the upwelling region.
Johnny A. Johannessen, Lars Petter Røed, T. Gammelsrød, J. R. Buckley, Ola M. Johannessen   +4 more
openaire   +3 more sources