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Evaluation of the hydrological contributions of permafrost to the thermokarst lakes on the Qinghai-Tibet Plateau using stable isotopes
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文摘

It firstly explores the isotopic hydrology in thermokarst lakes on the QTP.

The sublimation of ice is calculated for the estimation of contribution ratios.

The isotopic mass balance model is used to assess recharge of thawing permafrost.

The contributions of thawing permafrost to thermokarst lakes were of significance.

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