The Atmosphere and Ocean non-tidal De-aliasing Level-1B (AOD1B) product is widely used in satellite gravimetry to correct for transient effects of atmosphere-ocean mass variability that would otherwise alias into monthly-mean global gravity fields. In this presentation we give a short overview of recent and upcoming technical changes to the delivery of AOD1B. This includes the introduction of change-logs to indicate changes to previously delivered AOD files as well as an outlook of future work in terms of processing stability.
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Shihora et al. (2024) studied this question.
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