A state - of - the - art continuous ice core analytical system was used to analyze samples from ~ 1.5 to ~ 577 m depth in the recently collected WAIS Divide
deep ice core from West Antarctica.
A state - of - the - art continuous ice core analytical system was used to analyze ~ 3 cm by ~ 3 cm longitudinal samples from ~ 1300 to ~ 3404 m depth in the recently collected WAIS Divide
deep ice core from West Antarctica.
Not exact matches
Clow measured twice, once in 2011 and again in 2014, the temperature in a 3.4 - kilometer -
deep (2 - mile -
deep) borehole
from which the West Antarctic Sheet Divide
ice core had been drilled during an eight - year project that ended in 2011.
Core samples
from deeper in the Lake Towuti sediment will show whether this drying evident during the last
ice age also happened in previous
ice ages.
Gard found similar fossils
deeper down in the sediment
cores, indicating that the Arctic
ice partially cleared at various times
from about 128 000 to 71 000 years ago — a period covering the latest interglacial and the early part of the latest
ice age.
We show that DNA and amino acids
from buried organisms can be recovered
from the basal sections of
deep ice cores, enabling reconstructions of past flora and fauna.
Analysing new data
from marine sediment
cores taken
from the
deep South Atlantic, between the southern tip of South America and the southern tip of Africa, the researchers discovered that during the last
ice age,
deep ocean currents in the South Atlantic varied essentially in unison with Greenland
ice -
core temperatures.
Ice cores extracted
from deep within a Himalayan glacier leave little doubt that the earth's temperatures are on the rise.
Now, new evidence
from a marine sediment
core from the
deep Pacific points to warmer ocean waters around Antarctica (in sync with the Milankovitch cycle)-- not greenhouse gases — as the culprit behind the thawing of the last
ice age.
The simple fact is that every scientist now involved in climate science,
from the study of isotope ratios in
deep ice cores to the emission of methane
from tropical forests, is not only a scientist, but a political commentator and activist.
Ancient biomolecules
from deep ice cores reveal a forested southern Greenland.
Five millennia of surface temperatures and
ice core bubble characteristics
from the WAIS Divide
deep core, West Antarctica.
Ancient biomolecules
from deep ice cores reveal a forested southern Greenland Willerslev, E., E. Cappellini, W. Boomsma, R. Nielsen et al. 2007.
Five millennia of surface temperatures and
ice core bubble characteristics
from the WAIS Divide
deep core, West Antarctica, Paleoceanography, 31 (3), p. 416 - 433.
I've just returned
from the
deep field site at Aurora Basin where the Australians are drilling a new 400 - meter
ice core which we will analyze in my lab in Reno.
For example, the following paper http://ocean.mit.edu/~cwunsch/papersonline/milankovitchqsr2004.pdf finds that
deep - sea and
ice core records are formally indistinguishable
from stochastic data even if the data are artificially tuned to Milankovitch cycles.
The interactions (feedbacks) between THC shifts and sea
ice and glacial calving (as indicated by
ice - rafted debris in
deep sea
core records) would tend to seriously magnify the climate changes compared to what would be expected
from a similar THC shift today.
She and her colleagues created a model that accurately (to 97 %) replicates known historic solar activity (
from ice cores, tree ring data,
deep sea floor
cores, etc.).
Study of the
ice core recovered by Russian scientists
from deep Antarctic holes has revealed that in the last 450,000 years the Earth has had at least four peaks of temperature upsurge with fluctuations of 10 to 12 degrees.
I have some knowledge of biological processes and indeed, bacteria are at work even somewhere at the most harsh places on earth:
from boiling geisirs to
deep freezing
ice cores...
There are some detailed pages of information that have been meticulously reconstructed after having passed through the cross-cut shredder of geological history: the information
from ice cores and the
deep sea sediment
cores are obvious examples.
... The evidence comes
from a close correlation between inferred changes in production rates of the cosmogenic nuclides carbon - 14 and beryllium - 10 and centennial to millennial time scale changes in proxies of drift
ice measured in
deep - sea sediment
cores.
Evidence
from ice cores and
deep - sea sediment has shown that the Northern climate also cooled before the Southern climate during these abrupt changes, creating a «bipolar seesaw,» with the North cool while the South was warm, and the South cooling as the North warmed.
(28) + The emerging picture of severe instability was reinforced by studies of
cores drilled
from the Greenland and Antarctic
ice caps, and by
deep - sea
cores that covered much longer times.
Imputities are a main problem in Greenland
ice cores where a mix of seasalt / carbonate and acidic dust
from Icelandic volcanoes can produce CO2 in situ, but is less of interest in
deep inland Antarctic
ice cores, except during the
deepest times of glacials, when far more dust is deposited.
The air has been sealed off in the bubbles when the
ice was laid down, and extracted
from cores drilled
deep within the layered
ice deposits.
Visible gas hydrate and possible pore - space hydrate samples have been recovered for the first time in North America
from within
ice - bonded permafrost in a 451 - m -
deep core hole in the Mackenzie Delta, Northwest Territories, Canada.
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.
His personal contribution to these programmes encompasses a very large spectrum of topics
from a direct involvement in
deep drilling activities to the more theoretical aspects of the interpretation of
ice core data.
Nice plot: http://www.climate-change-theory.com/planetcycles.jpg When do you expect the next
deep freeze that empties 125m of water
from the seas to
ice in the polar and N / S latitudes per the Ice Core 120,000 y cycling patte
ice in the polar and N / S latitudes per the
Ice Core 120,000 y cycling patte
Ice Core 120,000 y cycling pattern?