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

. The Middle Miocene Climate Transition was characterized by major Antarcticice sheet expansion and global cooling during the interval∼ 15–13 Ma. Here we present two sets of boundary conditions forglobal general circulation models characterizing the periods before (MiddleMiocene Climatic Optimum; MMCO) and after (Middle Miocene Glaciation; MMG)the transition. These boundary conditions include Middle Miocene globaltopography, bathymetry, and vegetation. Additionally, Antarctic ice volumeand geometry, sea level, and atmospheric CO2 concentration estimates forthe MMCO and the MMG are reviewed. The MMCO and MMG boundary conditions havebeen successfully applied to the Community Climate System Model version 3(CCSM3) to provide evidence of their suitability for global climate modeling.The boundary-condition files are available for use as input in a wide varietyof global climate models and constitute a valuable tool for modeling studieswith a focus on the Middle Miocene.

Boundary conditions for the Middle Miocene Climate Transition (MMCT v1.0)