The oceans play an important role in regulating our climate and its change by absorbing heat and carbon. Scientists from the Department of Physics at Oxford University have discovered that the influence of circulation changes on shaping ocean warming will diminish in the future. This is despite having been identified and modelled as a key factor over the past 60 years.
The implications of their results, published today in Nature, are significant because regional sea level, affecting coastal populations around the world, depends on patterns of ocean warming. In this study they show how these patterns are likely to change.
The results imply widespread ocean warming and sea level rise, compared to the past, including increased warming near the Eastern edges of ocean basins leading to more sea level rise along the Western coastlines of continents in the North Atlantic and Pacific Oceans.
In the future, the imprint of rising atmospheric temperatures on ocean warming will likely dominate that of changes in ocean circulation.
Co-author, Laure Zanna, Visiting Professor in Climate Physics at Oxford University and Professor in the Center of Atmosphere Ocean Science at NYU Courant, said: ‘In the future, the imprint of rising atmospheric temperatures on ocean warming will likely dominate that of changes in ocean circulation. Initially, we might think that as the climate warms more, changes in ocean currents and their impact on ocean warming patterns will become larger. However, we show that that this is not the case in several regions of the ocean.’
A new method, developed by scientists at Oxford University, uses climate models to suggest that ocean warming patterns will increasingly be influenced by simple uptake of atmospheric warming – making them easier to predict. This is in contrast to now and the past when circulation changes were key factors in shaping ocean warming patterns.
Changes in ocean warming due to the simple uptake of atmospheric warming are easier to model and so the scientists hope that where previous models have struggled, they might become more accurate for future projections.
Better prediction of warming patterns implies better prediction of regional sea level rise, which will help to mitigate climate impacts such as flooding on individual communities.
Lead author, Dr Ben Bronselaer, who began conducting this research while a PhD student at Oxford University, said: ‘I think it is an encouraging possibility that climate models, which struggle to simulate past ocean warming, might be better at predicting future warming patterns. Better prediction of warming patterns implies better prediction of regional sea level rise, which will help to mitigate climate impacts such as flooding on individual communities. Of course, we do need to understand predictions of ocean circulation better to solidify this result.
‘During our research, we found a surprising relationship between ocean heat and carbon storage which appears to be unique. While there is a connection between these two quantities that is not yet fully understood, we think we have made significant progress towards uncovering it.’
The Nature study shows that the global ocean heat and carbon uptake go hand-in-hand, and the uptake rates are set by the present state of the ocean. This relationship is at the core of the method developed in this study. As humans change the ocean state by adding more heat and carbon, the ability of the ocean to take up both heat and carbon will be altered. A possible implication could be that the later emissions are reduced, the slower the reductions in atmospheric surface temperature are likely to be, due to the coupling between heat and carbon uptake by the ocean.
These results highlight a deep and fundamental connection between ocean and carbon uptake, which has implications for atmospheric heat and carbon. While ocean carbon and heat are separate systems, this study shows that they are deeply interconnected, via the capacity of the ocean to absorb these quantities. These results help explain why atmospheric warming depends linearly on cumulative carbon emissions.
Prof Laure Zanna said: ‘We find that the ocean’s capacity to absorb heat and carbon are coupled, and constrained by the ocean state. This implies that the present ocean state will regulate surface warming whether CO2 emissions continue to rise or decline.
‘The rates of ocean warming over the past 60 years have been significantly altered by changes in ocean circulation, particularly in the North Atlantic and parts of the Pacific Ocean, where we can identify cooling over some decades. However, in the future changes in ocean currents appear to play a smaller role on patterns of ocean warming, and the oceans will transport the excess anthropogenic heat in the ocean in a rather passive manner in these regions.’
The modelling in this study relied on a set of creative simulations done by colleagues at The Geophysical Fluid Dynamics Laboratory (GFDL), and other published work. Using these simulations, the scientists were able to draw hypotheses on how the patterns of heat and carbon are related and how they differ.
Building on this research, the scientists will now attempt to understand how the storage of heat and carbon in the ocean will affect the decline of atmospheric temperature and CO2 levels if carbon emissions start going down.
They will also use the component of ocean warming that is driven by circulation changes to better understand ocean circulation changes, which are difficult to measure directly, and their impact on regional sea level in the Tropics.