The new study gathered
sea ice samples near Greenland in 2014 and 2015 that the researchers then analyzed in a lab, comparing them to previously gathered cores from there and elsewhere in the Arctic.
Not exact matches
Participants in a
sea ice measurement campaign including the Max Planck Institute for Meteorology, are taking
samples of the Arctic
sea ice at Spitzbergen.
Examining these
samples helps them to better understand the factors that influence the development of
sea ice.
If a future orbiter could collect some material from a plume, that would allow us to
sample the
seas without the difficult task of landing and drilling into the
ice, says Phillips: «If there are life forms, they would be in the liquid layer.
The winch, pedaled by crew members and scientists, gradually deploys water -
sampling equipment that delivers
samples central to the mission: to characterize and understand the currents below the
sea ice on which the scientists» tents rest.
The researchers studied water
samples taken during cruises by Chinese
ice breaker XueLong, (meaning «snow dragon») in summer 2008 and 2010 from the upper ocean of the Arctic's marginal
seas to the basins as far north as 88 degrees latitude, just below the North Pole, as well as data from three other cruises.
Hawkings and his collaborators spent three months in 2012 and 2013 gathering water
samples and measuring the flow of water from the 600 - square - kilometer (230 - square - mile) Leverett Glacier and the smaller, 36 - square - kilometer (14 - square - mile) Kiattuut Sermiat Glacier in Greenland as part of a Natural Environment Research Council - funded project to understand how much phosphorus, in various forms, was escaping from the
ice sheet over time and draining into the
sea.
Surprise find The team's actual mission was to survey ocean currents near the Ross
Ice Shelf, a slab of ice extending more than 600 miles (970 kilometers) northward from the grounding zone of the West Antarctic Ice Sheet into the Ross Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment sampl
Ice Shelf, a slab of
ice extending more than 600 miles (970 kilometers) northward from the grounding zone of the West Antarctic Ice Sheet into the Ross Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment sampl
ice extending more than 600 miles (970 kilometers) northward from the grounding zone of the West Antarctic
Ice Sheet into the Ross Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment sampl
Ice Sheet into the Ross
Sea, to model the behavior of a drill string, a length of pipe extending to the seafloor which delivers drilling fluids and retrieves sediment
samples.
If a probe could catch some material from the plume, that would allow us to
sample the
seas without the difficult task of landing and drilling into the
ice, says Cynthia Phillips at the SETI Institute in Mountain View, California.
The researchers used 16s rRNA sequencing to characterize the microbial population in stool
samples donated by 19 inhabitants of the Hamlet of Resolute Bay, a Canadian Arctic village on the southern end of Cornwallis Island accessible only by plane (and, when the
sea ice breaks up, by boat).
To do so, they had also taken
sea -
ice samples.
For up to a month after
sea ice had melted, krill
samples from transitional zones had high concentrations of IPSO25 and HBI III.
Scientists collect
samples among the
sea ice and melt ponds of the Arctic's Chukchi S
sea ice and melt ponds of the Arctic's Chukchi
SeaSea.
The
sampling issues arise from the fact that
sea ice is highly dynamic with lots of spatial and seasonal variability so that measurements from individual moorings, submarine sonar tracks, and aircraft flights can only construct an incomplete picture of the evolution of the total Arctic
sea ice volume.
In our new take on the song, David added whale - ish notes on his bass clarinet along with
samples of the crackle and shoosh of floating
sea ice and we added two new verses taking the story from the
ice - locked end of the little
ice age to this era of warming, melting and opening seaways.
>... there are still ways of discovering the temperatures of past centuries,... tree rings... Core
samples from drilling in
ice fields... historical reconstruction... coral growth, isotope data from
sea floor sediment, and insects, all of which point to a very warm climate in medieval times.
Scientists dig deep into the rock and sand of the
sea floor to
sample Earth's climate history many millions of years ago, since the oldest
ice cores go back only 850,000 years.
For example, although the
sample size has been very small, studies of radio - collared seals in the Bering and Chukchi
Seas observed those seals rarely hauled out at all, on land or
sea ice, even when occupying
ice covered areas.
The
sampling locations ranged from the innermost area of the fjord just seaward from the modern
ice shelf to locations farther out to
sea that the shelf would have covered 2 millennia ago.
Minzoni and her fellow scientists had sailed to the Amundsen
Sea to study other parts of WAIS, but bad weather turned into good luck, forcing their sediment
sampling activities into a more protected area near the Cosgrove
Ice Shelf.
Aerial thickness surveys and ground - based
sampling in the western Beaufort and eastern Chukchi
Sea in April this year indicate that level
ice in the region is well over 3 m thick and strong (due to low salt content; www.sizonet.org).
And scientists can
sample ice cores, permafrost records, and tree rings to make some assumptions about the
sea ice extent going back 1,500 years.
High concentrations of both the
sea ice proxy IP25 and the phytoplankton biomarker brassicasterol were measured in
samples representing the late MIS 6 and the interstadials MIS 5e, 5c and 5a.
Sampling areas were split according to their
ice cover: North - West (less
sea ice cover), South - East (larger amplitude in
sea ice extent) and North - East / South - West (NESW) as bears from that zone are more mobile among all regions of Svalbard.
Scientists collect
samples among the
sea ice and melt ponds of the Arctic's Chukchi S
sea ice and melt ponds of the Arctic's Chukchi
SeaSea.
The approach to the
Sea Ice Outlook is a modified Delphi Method (i.e., using questionnaire responses from a panel of indendent experts) that: (1)
samples independent expert opinion and rationale on an issue, (2) communicates the results, and (3) iterates on the process with feedback from the expert participants.
Kaminski, T., F. Kauker, H. Eicken, and M. Karcher (2015), Exploring the utility of quantitative network design in evaluating Arctic
sea -
ice thickness
sampling strategies.
The
sea ice the authors
sampled would have had to travel freely through the Nares Strait to make it to Baffin Bay and eventually to Newfoundland, which could only have happened if
ice arches had failed to form, according to the study.
Proxy data such as those generated from
ice core
samples, measurements of tree rings intervals, bore
samples taken from sediments from the ocean and
sea floor, and measurement of gases from bubbles trapped in
ice are some examples of preserved physical characteristics of the past used by scientists to reconstruct prevailing climatic conditions in the past.
Scientists are collecting lake sediment, rock, water and plant
samples to explore linkages among Arctic
sea ice, atmospheric uptake, and changes in snowfall on the Greenland Ice She
ice, atmospheric uptake, and changes in snowfall on the Greenland
Ice She
Ice Sheet.
Over four years, it is reasonable to expect at least some warming (or cooling) below 900 m as well as in regions that Argo does not
sample such as under the
sea ice.
Uncertainties should decrease closer to near - current dates (e.g. from denser and more accurate
sampling)-- but note that these products also employ different QC and analysis methods, rely to varying degrees on satellite data, on
sea -
ice data to constrain polar SST, and on bias adjustments for historical changes in measurement methods.
These estimates resulted from studies of air bubbles recovered in
ice cores from deep within Antarctica, Greenland and other glaciers, as well as chemical analyses of coral
samples from beneath the
sea.