Spatial and temporal variability of snow chemical composition and accumulation rate at Talos Dome site (East Antarctica)
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文摘

Firn core decontamination is proved to be efficient for all the ions except ammonium.

Post-depositional storage effects are found for MSA, NO3−, NH4+.

Relatively high accumulation rate allows preservation of nitrate and MSA.

Undisturbed deposition allows annual snow layer counting by NO3−, nssSO42 − and MSA.

Spatial variability is lower than temporal variability at 5% significance level.

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