Climate record data set of ice core in Karakoram area
Among many indicators reflecting climate and environmental change, the stable isotope index of ice core is an indispensable parameter in the study of ice core record, and is one of the most reliable and effective ways to recover the past climate change. Ice core accumulation is a direct record of precipitation on glaciers, and high resolution ice core records ensure the continuity of precipitation records. Therefore, ice core records provide an effective means to recover precipitation changes. The isotope and accumulation of ice cores drilled from the Qinghai Tibet Plateau can be used to reconstruct the changes of temperature and precipitation, which is a good record of climate and environment. This data set provides stable isotope records of hushe ice core in Karakoram area and provides data support for the study of climate change in Qinghai Tibet Plateau.
The stable isotope depth series of ice core are stored in Excel format
Xu, B. (2020). Climate record data set of ice core in Karakoram area. A Big Earth Data Platform for Three Poles, DOI: 10.11888/Glacio.tpdc.270935. CSTR: 18406.11.Glacio.tpdc.270935. (Download the reference： RIS | Bibtex )
Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.
Pan-Third Pole Environment Study for a Green Silk Road-A CAS Strategic Priority A Program (No:XDA20000000)
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| East: 78.00 | West: 74.00 |
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| South: 34.00 | North: 36.00 |
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