English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

. Estimating the contribution of marine ice sheets to sea-level rise iscomplicated by ice grounded below sea level that is replaced by ocean waterwhen melted. The common approach is to only consider the ice volume abovefloatation, defined as the volume of ice to be removed from an ice column tobecome afloat. With isostatic adjustment of the bedrock and externalsea-level forcing that is not a result of mass changes of the ice sheetunder consideration, this approach breaks down, because ice volume abovefloatation can be modified without actual changes in the sea-levelcontribution. We discuss a consistent and generalised approach forestimating the sea-level contribution from marine ice sheets.

Brief communication: On calculating the sea-level contribution in marine ice-sheet models