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range between 1 and 220,970 (not every profile has been rated). International Geophysical Year (19571958). These have been collected by a robotic "vacuum cleaner" and examined, leading to improved estimates of their flux and mass distribution. These locations make samples available for testing. Byrd Station in Antarctica. 64 Isotopic analysis edit The isotopic composition of the oxygen in a core can be used to model the temperature history of the ice sheet. Encyclopedia of Quaternary Science.

Readme; Users gender; Rating matrix; Zipped rating and gender data, questions and comments: Vaclav Petricek petricek(at)acm.
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Coastal areas are more likely to include material of marine origin, such as sea salt ions. 81 Material from Laki can be identified in Greenland ice cores, but did not spread as far as Antarctica; the 1815 eruption of Tambora in Indonesia injected material into the stratosphere, and can be identified in both Greenland and Antarctic ice cores. Years of field work were required to determine the ideal location for a deep core; the field work included several intermediate-depth cores, at Dye 3 (372 m in 1971 Milcent (398 m in 1973) and Crete (405 m in 1974 among others. The subsequent North Greenland Eemian ( neem ) project retrieved a 2537 m core in 2010 from a site further north, extending the climatic record to 128,500 years ago; 111 neem was followed by Eastgrip, which began in 2015 in east Greenland and is expected. Some have been designed for working in cold ice; they have high power consumption and the heat they produce can degrade the quality of the retrieved ice core. Washington DC: National Academies Press.

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