Atmospheric mercury deposition during the last 270 years:
A glacial ice core record of natural and anthropogenic sources
Not exact matches
Ice core records are rich archives of the climate history during
glacial - interglacial cycles over timescales of up to ~ 800 kyr before the current age.
Readers can look for themselves at the Greenland
ice core record and decide whether there's anything of consequence going on around 41K before present that looks any different from other
glacial - interglacial cycles.You can look at the GISP data yourself by downloading
Methane changes much more quickly than CO2 in the
ice core records, through the Younger Dryas for example, which lasted 1000 years, methane goes back to
glacial values while CO2 sort of hovers in place.
Ice core records show that atmospheric CO2 varied in the range of 180 to 300 ppm over the
glacial - interglacial cycles of the last 650 kyr (Figure 6.3; Petit et al., 1999; Siegenthaler et al., 2005a).
Marine sediment
cores will reveal
records of past
glacial - interglacial cycles while lake sediments and peat
cores will reveal climate
records since the last
ice age.
An ultra-high resolution continuous
record of methane variations during the last
glacial - interglacial transition from the WAIS Divide
ice core.
Methane changes much more quickly than CO2 in the
ice core records, through the Younger Dryas for example, which lasted 1000 years, methane goes back to
glacial values while CO2 sort of hovers in place.
Ice -
core records of
glacial - interglacial cycles provide considerable insight into the coupling of the carbon cycle and climate....
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.
But for me the strongest evidence that small flucuations can have tremendous impact comes from the
ice core and sediment
records of the
glacial / interglacial cycles.
And according to scientists who have 800,000 years of carbon
records derived from
glacial ice core samples, there is a strong link between earth temperatures and increased carbon dioxide levels in the atmosphere.
Figure 2 shows our data together with earlier results from the Dome C (650 — 390 kyr bp4 and 22 — 0 kyr bp5), Vostok1, 2,3 (440 — 0 kyr bp) and Taylor Dome6 (60 — 20 kyr bp)
ice cores resulting in a composite CO2
record over eight
glacial cycles.
Rather, the
ice core record shows clearly that changes in temperature precede changes in carbon dioxide throughout the
glacial - interglacial cycle (Mudelsee, 2001), and that for the last half million years the climate system has oscillated in a self - limiting way between
glacials and interglacials by about 6 deg.
The climate
record obtained from two long Greenland
ice cores reveals several brief climate oscillations during
glacial time.
The 800 year lag is observed in
ice core records following (and prior to)
Glacial Minima (Gm).
The researchers did not notice an obvious relationship between the accumulation of
ice recorded in the
ice core and
glacial fluctuation.
Tree rings, coral skeletons, and
glacial ice cores (Figure 3) are proxies for annual temperature
records, while boreholes (holes drilled deep into Earth's crust) can show temperature shifts over longer periods of time.
The ubiquitous character of certain events further confirms their importance: «the Younger Dryas and a large number of abrupt changes during the last
ice age called Dansgaard / Oeschger events (23 abrupt changes into a climate of near - modern warmth and out again, during the last
glacial period) have been corroborated in multiple
ice cores from Greenland, Antarctica and tropical mountains, marine sediments from the North Atlantic Ocean, the tropical Atlantic, eastern Pacific, and Indian Oceans, and from various
records on land.
[13] Hubertus Fischer, Martin Wahlen, Jesse Smith, Derek Mastroianni, Bruce Deck, «
Ice Core Records of Atmospheric CO2 around the Last Three
Glacial Terminations,» Science, vol.
John Philips: «The fastest rate of warming
recorded in the
ice cores occurs as we emerge from a
glacial to an interglacial period.
Note that regional proxies, such as the oxygen - isotope temperature reconstructions from the Greenland
Ice Core Project that
record Dansgaard - Oeschger events, often indicate faster regional rates of climate change than the overall global average for
glacial - interglacial transitions, just as today warming is more pronounced in Arctic regions than in equatorial regions (Barnosky et al., 2003; Diffenbaugh and Field, 2013).
We will present a carbon dioxide
record from 40 - 35 and 28 - 9 ka from the last
glacial and deglacial periods from a new
ice core from West Antarctica with an average sampling resolution of 25 - 50 yrs.
That includes
records of bird migration patterns and the dates that cherry trees bloom, as well as analyses of air bubbles sealed inside
glacial ice cores and of the shells of foraminifera, single - celled sea creatures.
Glacial / interglacial changes in mineral dust and sea - salt
records in polar
ice cores: Sources, transport, and deposition
Is the temperature chronology of the
ice cores and global proxies consistent with the well - dated, global
glacial record?
[DOI: 10.1126 / science.1177840]-RRB- correlated speleotherm,
ice core, and marine
records to show a sequence of events that led to termination of
glacials in the past: 1.
Such as another fascinating paper by Don J. Easterbrook, Professor Emeritus in the Deptment of Geology at Western Washington University: «Solar Influence on Recurring Global, Decadal, Climate Cycles
Recorded by
Glacial Fluctuations,
Ice Cores, Sea Surface Temperatures, and Historic Measurements Over the Past Millennium» — Hat tip to Anthony Watt's Watts Up with That.
Readers can look for themselves at the Greenland
ice core record and decide whether there's anything of consequence going on around 41K before present that looks any different from other
glacial - interglacial cycles.You can look at the GISP data yourself by downloading
The discovery in
ice core records that atmospheric concentrations of two potent greenhouse gases, carbon dioxide and methane, have decreased during past
glacial periods and peaked during interglacials indicates important feedback processes in the Earth system.