Reconstructing Paleoclimates on West Antarctic Ice Sheet Using Ice Core Bubble Number-Density
A new paleoclimatic indicator based on ice core bubble number-density shows a ~1.7°C cooling from ~257 B.C.E. to ~1686 C.E. at the WAIS Divide site in West Antarctica. Independent estimates of paleoclimatic variables increase our confidence in reconstructions. It is known that density increase and g...
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Language: | English |
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Penn State
2010
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Online Access: | http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-4735/index.html |