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Coccolithophore dynamics in non-bloom conditions during late summer in the central Iceland Basin (July-August 2007)
Coccolithophore dynamics non-bloom conditions late summer central Iceland Basin
2014/4/17
Measurements of primary production (PP), calcification (CF), and coccolithophore abundance were made during late summer (July-August 2007) in the Iceland Basin. Low numbers of coccolithophore cells an...
Sedimentation of acantharian cysts in the Iceland Basin: Strontium as a ballast for deep ocean particle flux, and implications for acantharian reproductive strategies
acantharian cysts a ballast for deep ocean particl
2014/4/16
Acantharian cysts were discovered in sediment trap samples from spring 2007 at 2000 m in the Iceland Basin.
Although these single-celled organisms contribute to particulate organic matter flux in the...
The Iceland–Faroe Front：A Synergistic Study of Hydrography and Altimetry
Iceland–Faroe Front hydrographic surveys
2008/12/17
Two triangular hydrographic surveys were conducted in the Iceland-Faroes region with sampling corresponding to the ERS-1 3-day commissioning-phase orbit. The CTD, XBT, and ADCP data show a very active...
Amplification of Tidal Currents by Overflow on the Iceland-Faeroe Ridge
Tidal Currents Iceland-Faeroe Ridge Overflow
2008/12/15
During several days in July 1990, there was an abrupt increase in semidiurnal tidal current in the upper part of the water column seaward of the steep continental rise southeast of Iceland. This tidal...
Hydrographic Variability in the Bottom Layer of the Iceland Basin
Hydrographic Variability Iceland Basin Bottom Layer Subpolar Mode Water
2008/12/12
The variability of the lowest 400 dbar in the Deep Iceland Basin has been studied for the years 1988–1991. It appears that hydrographic parameters of the Iceland–Scotland Overflow Water in the lowest ...
Quasigeostrophic Forecasting and Physical Processes of Iceland-Faroe Frontal Variability
Iceland-Faroe Front Iceland-Faroe Frontal Variability Quasigeostrophic Forecasting
2008/12/12
Using a hydrocast survey of the Iceland-Faroe Front (IFF) from October 1992, quasigeostrophic forecasts are studied to validate their efficacy and to diagnose the physical processes involved in the ra...
A Topographic–Rossby Mode Resonance over the Iceland–Faeroe Ridge
Iceland–Faeroe Ridge Topographic–Rossby Mode
2008/12/11
An array of current meter moorings along 12°W on the southern side of the lceland-Faeroe Ridge reveals a narrowband barotropic oscillation with period 1.8 days in spectra of velocity. The signal is co...
Potential Vorticity and Vertical Velocity at the Iceland-Færœs Front
Potential Vorticity Iceland-Fæ rœ s Front Vertical Velocity
2008/12/11
Using data from high-resolution surveys of the Iceland- Færœs Front, the authors have calculated synoptic maps of the geostrophic velocity, vorticity, and potential vorticity on isopycnal s...
The Flux of Dense Cold Overflow Water Southeast of Iceland
Dense Cold Overflow Water Iceland
2008/12/3
From the period commencing midsummer 1990 and lasting for 13 months, 13 current meters were deployed on seven moorings at depths between 1000 and 2300 m southeast of Iceland (63°09′N, 17°18′W to 61°44...