Source Themes

Relating patterns of added and redistributed ocean warming
Ocean warming patterns are a primary control on regional sea level rise and transient climate sensitivity. However, controls on these …
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The Influence of Warming Patterns on Passive Ocean Heat Uptake
The climate s response to forcing depends on how efficiently heat is absorbed by the ocean. Much, if not most, of this ocean heat …
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GCM-Filters: A Python Package for Diffusion-based Spatial Filtering of Gridded Data
GCM-Filters is a python package that allows scientists to perform spatial filtering analysis in an easy, flexible and efficient way. …
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Evaluation of the Local Sea-Level Budget at Tide Gauges Since 1958
Although global mean sea-level rise since 1900 and regional mean sea-level change since the 1960s have been accounted for in terms of …
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Deep Learning of Unresolved Turbulent Ocean Processes in Climate Models
Climate models are an approximate representation of the laws of physics describing the evolution of the ocean and atmosphere dynamics. …
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Stochastic-Deep Learning Parameterization of Ocean Momentum Forcing
Coupled climate simulations that span several hundred years cannot be run at a high-enough spatial resolution to resolve mesoscale …
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What causes the spread of model projections of sea level change in response to greenhouse gas forcing?
Sea levels of different atmosphere–ocean general circulation models (AOGCMs) respond to climate change forcing in different ways, …
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Resolving and Parameterising the Ocean Mesoscale in Earth System Models
Although the choice of ocean resolution in Earth System models will always be limited by computational considerations, for the …
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The causes of sea-level rise since 1900
The rate of global-mean sea-level rise since 1900 has varied over time, but the contributing factors are still poorly understood1. …
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Heat and carbon coupling reveals ocean warming due to circulation changes
Anthropogenic global surface warming is proportional to cumulative carbon emissions1,2,3; this relationship is partly determined by the …
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