Ice floes' clashing as the source for acoustic ambient noise in the marginal ice zone of the Arctic Ocean

2019 ◽  
Vol 146 (4) ◽  
pp. 2807-2808
Author(s):  
Chi-Fang Chen
Keyword(s):  
Arctic Ocean ◽  
Ambient Noise ◽  
The Arctic ◽  
Marginal Ice Zone ◽  
The Arctic Ocean ◽  
Ice Floes

Ambient noise in the Arctic Ocean measured with a drifting vertical line array

2015 ◽  
Vol 138 (3) ◽  
pp. 1744-1744
Author(s):  
Peter F. Worcester ◽  
Matthew A. Dzieciuch ◽  
John A. Colosi
Keyword(s):  
Arctic Ocean ◽  
Ambient Noise ◽  
Vertical Line ◽  
The Arctic ◽  
Line Array ◽  
The Arctic Ocean

Ambient noise in the Arctic Ocean measured with a drifting vertical line array

2014 ◽  
Vol 136 (4) ◽  
pp. 2149-2149
Author(s):  
Peter F. Worcester ◽  
Matthew A. Dzieciuch ◽  
John A. Colosi ◽  
John N. Kemp
Keyword(s):  
Arctic Ocean ◽  
Ambient Noise ◽  
Vertical Line ◽  
The Arctic ◽  
Line Array ◽  
The Arctic Ocean

Dissolved Neodymium Isotopes Trace Origin and Spatiotemporal Evolution of Modern Arctic Sea Ice

2020 ◽  
Author(s):  
Georgi Laukert ◽  
Dorothea Bauch ◽  
Ilka Peeken ◽  
Thomas Krumpen ◽  
Kirstin Werner ◽  
...  
Keyword(s):  
Sea Ice ◽  
Arctic Ocean ◽  
Surface Waters ◽  
Ice Cores ◽  
Arctic Sea Ice ◽  
The Arctic ◽  
Spatiotemporal Evolution ◽  
Arctic Sea ◽  
The Arctic Ocean ◽  
Ice Floes

<p>The lifetime and thickness of Arctic sea ice have markedly decreased in the recent past. This affects Arctic marine ecosystems and the biological pump, given that sea ice acts as platform and transport medium of marine and atmospheric nutrients. At the same time sea ice reduces light penetration to the Arctic Ocean and restricts ocean/atmosphere exchange. In order to understand the ongoing changes and their implications, reconstructions of source regions and drift trajectories of Arctic sea ice are imperative. Automated ice tracking approaches based on satellite-derived sea-ice motion products (e.g. ICETrack) currently perform well in dense ice fields, but provide limited information at the ice edge or in poorly ice-covered areas. Radiogenic neodymium (Nd) isotopes (ε<sub>Nd</sub>) have the potential to serve as a chemical tracer of sea-ice provenance and thus may provide information beyond what can be expected from satellite-based assessments. This potential results from pronounced ε<sub>Nd</sub> differences between the distinct marine and riverine sources, which feed the surface waters of the different sea-ice formation regions. We present the first dissolved (< 0.45 µm) Nd isotope and concentration data obtained from optically clean Arctic first- and multi-year sea ice (ice cores) collected from different ice floes across the Fram Strait during the RV POLARSTERN cruise PS85 in 2014. Our data confirm the preservation of the seawater ε<sub>Nd</sub>signatures in sea ice despite low Nd concentrations (on average ~ 6 pmol/kg) resulting from efficient brine rejection. The large range in ε<sub>Nd</sub> signatures (~ -10 to -30) mirrors that of surface waters in various parts of the Arctic Ocean, indicating that differences between ice floes but also between various sections in an individual ice core reflect the origin and evolution of the sea ice over time. Most ice cores have ε<sub>Nd</sub> signatures of around -10, suggesting that the sea ice was formed in well-mixed waters in the central Arctic Ocean and transported directly to the Fram Strait via the Transpolar Drift. Some ice cores, however, also revealed highly unradiogenic signatures (ε<sub>Nd</sub> < ~ -15) in their youngest (bottom) sections, which we attribute to incorporation of meltwater from Greenland into newly grown sea ice layers. Our new approach facilitates the reconstruction of the origin and spatiotemporal evolution of isolated sea-ice floes in the future Arctic.</p>

Algal bloom in a melt pond on Canada Basin pack ice

Polar Record ◽  
2015 ◽  
Vol 52 (1) ◽  
pp. 114-117 ◽  
Author(s):  
Ling Lin ◽  
Jianfeng He ◽  
Fang Zhang ◽  
Shunan Cao ◽  
Can Zhang
Keyword(s):  
Arctic Ocean ◽  
Algal Bloom ◽  
Canada Basin ◽  
The Arctic ◽  
Arctic Warming ◽  
Melt Pond ◽  
Melt Ponds ◽  
Pack Ice ◽  
The Arctic Ocean ◽  
Ice Floes

ABSTRACTMelt ponds are common on the surface of ice floes in the Arctic Ocean during spring and summer. Few studies on melt pond algae communities have been accomplished. These studies have shown that these melt ponds were ultra-oligotrophic, and contribute little to overall productivity. However, during the 6th Chinese Arctic Cruise in the Arctic Ocean in summer 2014, a closed coloured melt pond with a chlorophyll a concentration of 15.32 μg/L was observed on Arctic pack ice in the Canada Basin. The bloom was caused by the chlorophyte Carteria lunzensis at an abundance of 15.49×106 cells/L and biomass of 5.07 mg C/L. Primary production within surface melt ponds may need more attention along with Arctic warming.

Oceanographic Features of the Canadian Archipelago

1957 ◽  
Vol 14 (5) ◽  
pp. 731-769 ◽  
Author(s):  
W. B. Bailey
Keyword(s):  
Arctic Ocean ◽  
Beaufort Sea ◽  
The Arctic ◽  
Temperature Structure ◽  
Vertical Temperature ◽  
Baffin Bay ◽  
The North ◽  
The Arctic Ocean ◽  
North Water ◽  
Ice Floes

Oceanographic data collected during the first cruise of H.M.C.S. Labrador to the Canadian Arctic in August and September 1954 permit comparisons of the vertical temperature and salinity structures in Baffin Bay, the Canadian Archipelago and the Arctic Ocean. From a comparison of the temperature–salinity characteristics of the waters in the Arctic Ocean (Beaufort Sea) with those in Baffin Bay, it is found that: (a) the surface waters of the Arctic Ocean are much less saline than those in Baffin Bay, but minimum temperatures are the same (−1.8 °C), (b) the waters of the upper 200 m. in Baffin Bay are denser than those found at corresponding depths in the Arctic Ocean, (c) below 200 m., Arctic waters are the denser, and below 500 m. they are denser than any waters found in Baffin Bay, and (d) waters found at 250 m. in the Beaufort Sea, at 500 m. in Smith Sound, and at 1250 m. in central Baffin Bay, have identical temperature and salinity characteristics (−0.3 °C., 34.4‰).In addition the data permitted limited investigations into the effect of drifting ice floes on the vertical temperature structure of the water, the origin of the "north water", long-term variations in the oceanographic conditions in Baffin Bay, and dynamic calculations of currents and volume transports of the waters through the channels leading into Baffin Bay.

Higher frequency ambient noise in the Arctic Ocean

1988 ◽  
Vol 84 (4) ◽  
pp. 1444-1455 ◽  
Author(s):  
James K. Lewis ◽  
Warren W. Denner
Keyword(s):  
Arctic Ocean ◽  
Ambient Noise ◽  
The Arctic ◽  
The Arctic Ocean

Modelled Stokes drift in the Marginal ice zones of the Arctic Ocean

2020 ◽  
Author(s):  
Jingkai Li
Keyword(s):  
Arctic Ocean ◽  
Chukchi Sea ◽  
Surface Current ◽  
Reanalysis Data ◽  
Stokes Drift ◽  
The Arctic ◽  
Bulk Wave ◽  
Wave Parameters ◽  
The Arctic Ocean ◽  
Ice Floes

<p>The Stokes drift in the marginal ice zones (MIZ) of the Arctic Ocean is modelled by WAVEWATCH III. Applying two viscoelastic and one empirical frequency-dependent wave-ice models, the modelled wave parameters and spectrum are compared with field observations in the Beaufort-Chukchi Sea. Three wave-ice parameterizations show similar abilities to produce the surface Stokes drift estimated from buoy measurements. By using five-year (2015-2019) hindcasted directional spectra of the autumn Arctic, we present and discuss the monthly mean surface Stokes drift (1-10 cm/s), e-folding depth (1-14 m) and vertically integrated transport (0.1-0.4 m2/s) in the marginal ice zones, which are stronger in October than in September. When bulk wave parameters are adopted to estimate the Stokes drift fields, the surface Stokes drift will be underestimated by about 44-59% with mean ice concentration smaller than 60%, and the Stokes e-folding depth will be overestimated by about 1.4 to 5.0 times increasing from the interior to the edge of the ice cover. Since the Stokes drift may be an important component of the total surface current, we compare the modelled surface Stokes drift with the Eulerian current from reanalysis data, which shows that the mean surface Stokes drift is typically about 30% of the Eulerian current over large parts of the MIZ in Arctic Ocean, and is of the same order or even larger in some sea areas of the Chukchi, E. Siberian and Laptev Seas. It indicates that the Stokes drift is necessary to be considered to better model the dynamic processes of the sea ice, especially for the drift of ice floes.</p>

scholarly journals Observation of a fast ozone loss in the marginal ice zone of the Arctic Ocean

2006 ◽  
Vol 111 (D15) ◽  
Author(s):  
Hans-Werner Jacobi ◽  
Lars Kaleschke ◽  
Andreas Richter ◽  
Alexei Rozanov ◽  
John P. Burrows
Keyword(s):  
Arctic Ocean ◽  
The Arctic ◽  
Ozone Loss ◽  
Marginal Ice Zone ◽  
The Arctic Ocean
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