<p indent="0mm">Remarkable scientific discoveries have been made from the studies of ice cores drilled in polar ice sheets and mountain ice caps. These samples serve as the most accurate archives of the past atmospheric composition thus far. Two milestone achievements of ice cores include a continuous record of atmospheric greenhouse gas concentrations over the past eight glacial cycles (800 ka) and the discovery of abrupt climate change events on millennial timescale, both made possible by deep drilling in polar ice sheets. Yet, this conventional approach of deep drilling is faced with challenges from prohibitive logistical and operational cost and limited sample supply, particularly with greater depth. To address these challenges, shallow coring in blue ice areas has emerged as an appealing alternative. Two significant advances have been recently achieved from blue ice studies. Ice older than <sc>800 ka</sc> from the Allan Hills Blue Ice Area was discovered and the trapped gases inside the ice allow, for the first time, for the direct observation of atmospheric carbon dioxide concentrations (pCO<sub>2</sub>) before <sc>800 ka.</sc> The data show no long-term decline in atmospheric pCO<sub>2</sub>, and consequently, the Mid-Pleistocene Transition is not the result of cooling resulting from a decreasing pCO<sub>2</sub>. Moreover, large-volume samples retrieved by a large-diameter ice drill (“Blue Ice Drill”) in the Taylor Glacier Blue Ice Area allow for novel geochemical analyses such as the radiocarbon (<sup>14</sup>C) content of methane (CH<sub>4</sub>). The <sup>14</sup>C of CH<sub>4</sub> trapped in the Taylor Glacier ice suggests that old carbon reservoirs were not responsible for the deglacial rise of CH<sub>4</sub> in the last glacial cycle. Another example of new geochemical methods enabled by the unprecedented sample availability offered by the blue ice areas is the elemental ratios of xenon, krypton, and nitrogen which are sensitive to the mean ocean temperature (MOT). Taylor Glacier ice samples dating back to the penultimate glacial period record <sc>1.1±0.3°C</sc> warmer-than-modern MOT values at <sc>129 ka</sc>, near the end of the penultimate deglaciation. Despite these advances, several challenges and limits remain. First, to accurately establish a chronology for the blue ice samples requires methods of absolute dating, which have considerable uncertainties at present. A precise chronology can be established via timescale synchronization with existing deep ice cores only when the blue ice is younger than <sc>800 ka.</sc> Second, the original deposition site of the blue ice field is not always known, complicating the interpretations of climate proxies that are sensitive to depositional environments such as the stable water isotopes of the ice. Third, glacial flows disrupt the chronology of the ice and could lead to the incomplete and biased preservation of climate signals. In light of these issues and shortcomings, stratigraphically continuous ice cores cannot be fully replaced by temporally discrete samples from the blue ice areas, although blue ice records hold the potentials to provide snapshots of the critical intervals of the Quaternary climate. Future progress in blue ice research may be made in three directions: (1) The prospecting of new blue ice fields and identification of blue ice areas containing the climate records of key understudied intervals; (2) numerical simulations of glacial dynamics to better the interpretation of blue ice records; and (3) the development of novel analytical techniques that reveal new climate information.
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