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- W4232631239 abstract "Abstract. Two ice cores recovered from the Himalayan East Rongbuk (ER) Glacier on the northeast saddle of Mt. Qomolangma (Everest) (28° 01' N, 86° 58' E, 6518 m a.s.l.) give access to a tentative record of past Himalayan atmospheric mixing ratio of CH4 spanning the past 1200 yr. The major part of the record is affected by artefacts probably due to in-situ production. After selecting what may represent the true atmospheric mixing ratio, an average of 749 ± 25 ppbv of CH4 is estimated for the late preindustrial Holocene, which is ~ 36 ± 17 (~ 73 ± 18) ppbv higher than the atmospheric levels recorded respectively in Greenland and Antarctic ice cores. A comparison of these new data with model simulations of the CH4 latitudinal gradient suggests either that the models do not get a correct balance between high and low latitude CH4 sources, or that the filtered CH4 profile from the ER cores remains infected by small artefacts." @default.
- W4232631239 created "2022-05-12" @default.
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- W4232631239 date "2013-05-13" @default.
- W4232631239 modified "2023-09-28" @default.
- W4232631239 title "A new Himalayan ice core CH<sub>4</sub> record: possible hints on the preindustrial latitudinal gradient" @default.
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- W4232631239 doi "https://doi.org/10.5194/cpd-9-2471-2013" @default.
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