Data from: The role of Southeast Asian island topography on Indo-Pacific climate and silicate weathering

The modern configuration of the South East Asian Islands (SEAI) evolved
over the last fifteen million years, as a result of subduction, arc
magmatism, and arc-continent collisions, contributing to both increased
land area and high topography.  The presence of the additional
land area has been postulated to enhance convective rainfall, facilitating
both increased silicate weathering and the development of the modern-day
Walker circulation.  Using an Earth System Model in conjunction
with a climate-silicate weathering model, we argue instead for a
significant role of SEAI topography for both effects.  This
dataset archives model output used in this investigation, including
simulations using the Community Earth System Model version 1.2, and the
climate-silicate weathering model GEOCLIM.