The ocean is warming, losing oxygen and being acidified, primarily as a result of
anthropogenic carbon emissions. With ocean warming, acidification and deoxygenation …

Great advances have been made in the last decade in quantifying and understanding the
spatiotemporal patterns of terrestrial gross primary production (GPP) with ground …

Anthropogenic climate change is projected to lead to ocean warming, acidification,
deoxygenation, reductions in near-surface nutrients, and changes to primary production, all …

We describe the baseline coupled model configuration and simulation characteristics of
GFDL's Earth System Model Version 4.1 (ESM4. 1), which builds on component and coupled …

Projections of climate change impacts on marine ecosystems have revealed long-term
declines in global marine animal biomass and unevenly distributed impacts on fisheries …

Droughts that exceed the magnitudes of historical variation ranges could occur increasingly
frequently under future climate conditions. However, the time of the emergence of …

Results from the fully-, biogeochemically-, and radiatively-coupled simulations in which CO
2 increases at a rate of 1% per year (1pctCO2) from its pre-industrial value are analyzed to …

Although the terrestrial biosphere absorbs about 25 per cent of anthropogenic carbon
dioxide (CO2) emissions, the rate of land carbon uptake remains highly uncertain, leading to …

Two questions motivated this study: 1) Will meteorological droughts become more frequent
and severe during the twenty-first century? 2) Given the projected global temperature rise, to …

International trade enables us to exploit regional differences in climate change impacts and
is increasingly regarded as a potential adaptation mechanism. Here, we focus on hunger …