The Heat Is Online

Ocean Current Shutdown Could Occur in Two Decades

Ocean Current Shutdown Could Occur in Two Decades

Nature,Vol. 399, 523-524 June 10, 1999

Shifting seas in the greenhouse?

By Stefan Rahmstorf

The effect that global warming might have on the circulation of the Atlantic Ocean has been a topic of much speculation and research. Onpage 572 of this issue, Wood et al ("Changing spatial structure of thermohaline circulation in response to atmospheric CO2 forcing in a climate model").1 present greenhouse warming scenarios computed with a climate model that, for the first time, gives a realistic simulation of the large-scale ocean currents without requiring artificial adjustments of the air-sea fluxes.

Of more immediate interest to those outside the modelling business, Wood and colleagues' results show a dramatic change in the Atlantic occurring over the next few decades: a complete shutdown of one of the two main 'pumps' driving the formation of North Atlantic Deep Water, namely the one in the Labrador Sea (Fig. 1).

In 1987, in an article entitled "Unpleasant surprises in the greenhouse?", Broecker2 warned that the response of the climate system to greenhouse warming might involve 'mode switches' of the Atlantic circulation. He drew this inference from palaeoclimatic data, indicating that such events had occurred in the past, and from early ocean modelling results. Initially, the idea was simply that a positive feedback meant that the large-scale overturning motion of the Atlantic (sometimes popularly dubbed the 'conveyor belt', in which warm surface waters flow northwards and cold deep water returns south throughout the Atlantic, acting like a central-heating system for Europe; seeFig. 1) could exist in two distinct states -- switched on (as at present) or switched off.

Later work revealed a more complex picture, by showing that individual sites of oceanic convection could also have a tendency towards flip-flop behaviour (switching between quasi-stable states with convection 'on' or 'off')3,4. Given that there are two main sites of convection linked to the formation of North Atlantic Deep Water, in the Greenland Sea and in the Labrador Sea, this led to speculation that global warming could switch off one of these convection sites5.

Wood et al. provide the first clear modelling result indicating that this could indeed be the response to increasing concentrations of greenhouse gases. The team works at the Hadley Centre in Britain, and their climate model is remarkable in several respects. Certain improvements, including a higher resolution of the ocean and parameterizations of eddy mixing and of the flow of bottom currents over marine sills, mean that the model provides a more realistic representation of the main ocean currents than previous coupled ocean-atmosphere models. In particular, the partitioning of the deep-water formation between the Greenland and Labrador Seas is in good agreement with observations. Furthermore, unlike most previous climate models, this model does not use or require 'flux adjustments' at the air-sea interface, which involve adding a prescribed heat or freshwater flux to make up for a mismatch between ocean and atmosphere components of the climate model. Flux adjustments had to be used in the past to prevent the model climate from drifting slowly to unrealistic conditions, but they may distort the stability of the ocean circulation6.

The authors subject their model to two greenhouse-gas scenarios: an artificially rapid increase in atmospheric concentrations by 2% per year up to a quadrupling of CO2, and a more realistic 'business as usual' scenario starting in 1860 and extending to the year 2100. In both cases, the overall volume of water transported by the Atlantic conveyor belt (Atlantic overturning) decreases by around 25%, but it does not reach the point of collapse. This is consistent with most simulations by other groups (Fig. 2, overleaf). Previous studies indicate that the threshold for a complete conveyor-belt shutdown could be crossed in the twenty-second century if precipitation and meltwater runoff into the North Atlantic are strongly enhanced7, diluting the surface waters to the point where the high-latitude sinking motion stops. This, however, is a point on which large uncertainty remains in climate models.

What is new in Wood and colleagues' simulation1 is the shutdown in Labrador Sea convection and the associated collapse of the Labrador Current, which occurs between the years 2000 and 2030. If such a collapse did occur, it could have serious consequences for marine ecosystems, including seabird populations in the region, as they depend not only on specific temperature conditions but also on nutrients supplied by oceanic mixing and currents.

But how likely is this change in ocean circulation? From a single model simulation, even one carried out with an advanced climate model, it is difficult to assess the range of uncertainty. Many regional aspects of the ocean circulation, including the energetic synoptic eddies, cannot at present be resolved by this (or any other) climate model. Synoptic eddies are the ocean's equivalent of the high- and low-pressure systems that make up weather in the atmosphere, and they play an important role in mixing ocean waters and in transporting heat in some regions. High-resolution ocean models exist, but their severe computational cost means that they cannot yet be used in climate simulations. Owing to the lack of relevant controlled experiments comparing high- and low-resolution models, it is still an open scientific question to what extent the results of climate models would change if oceanic eddies were resolved explicitly.

Another caveat is the uncertainty in regional precipitation changes due to global warming, as the input of fresh water from increased precipitation would have a considerable effect on oceanic convection by changing the surface water density. Different models of atmospheric behaviour predict widely differing changes in precipitation. The Hadley Centre model also does not take into account the fresh water entering the Labrador Sea from the north, through the Canadian archipelago.

Given these uncertainties, the results of Wood et al. should be interpreted as a warning that a regional shut-down of convection could occur and that it could even occur soon, without taking the specific timing and location as a definitive prediction. The Labrador convection site may indeed be more vulnerable to greenhouse warming than the Greenland Sea site, given that the deep water formed in the Labrador Sea is already the less dense of the two, which could mean that a relatively small reduction in surface density could stop convection altogether. This hypothesis needs to be confirmed by future modelling studies.

So far, however, observations show no sign of a systematic weakening of convection in the Labrador Sea. On the contrary, after a weak phase in the late 1960s, convection in the 1990s has been favoured by the high phase of the North Atlantic Oscillation8, the dominant mode of natural variability in the region. Both North Atlantic convection regions need to be continuously monitored, as planned in the international CLIVAR (Climate Variability and Predictability) programme.

The simulated ending of Labrador Sea convection found in the Hadley Centre model is perhaps the most convincing demonstration so far of a qualitative threshold being crossed because of global warming. Such nonlinear effects are increasingly receiving attention in climate research, following the 1995 IPCC report's9 warning that "future climate change may also involve 'surprises'". Another possible 'surprise' (the term is a misnomer, as the element of surprise lessens the more it is discussed) is that the West Antarctic Ice Sheet could become unstable and slide into the ocean, causing sea level to rise by several metres10.

To evaluate the risk of such events it is not enough to compute a few 'best guess' projections of future climate change. More sophisticated and systematic approaches to risk assessment are required, taking the full range of uncertainty in current knowledge and models into account. This is a difficult task, not helped by the fact that many climate models operate at the limits of available computer power. Nevertheless, it needs to be tackled. As in any risk assessment, it is not just the most likely outcome of global warming that affects how we should handle the problem, but also the 'tail ends' of the probability distribution of possible futures: events with a low probability but a high damage potential. Take the risk of nuclear power stations for comparison: the most likely scenario is that everything works just fine, but large investments are nevertheless made to insure against the tiny probability of a catastrophic failure.

Although many global warming risks are still difficult to quantify, the work of Wood and colleagues is a reminder that now is the time to invest in a 'full-cover insurance policy' by reducing greenhouse gas emissions.

Stefan Rahmstorf is at the Potsdam Institute for Climate Impact Research (PIK), PO Box 60 12 03, 14412 Potsdam, Germany.

  1. Wood, R. A., Keen, A. B., Mitchell, J. F. B. & Gregory, J. M. Nature 399, 572-575 (1999). Links
  2. Broecker, W. Nature 328, 123-126 (1987). Links
  3. Lenderink, G. & Haarsma, R. J. J. Phys. Oceanogr. 24, 1480-1493 (1994). Links
  4. Rahmstorf, S. Nature 378, 145-149 (1995). Links
  5. Rahmstorf, S. Nature 388, 825-826 (1997). Links
  6. Marotzke, J. & Stone, P. H. J. Phys. Oceanogr. 25, 1350-1364 (1995). Links
  7. Rahmstorf, S. & Ganopolski, A. Clim. Change (in the press). Links
  8. Dickson, B. Nature 386, 649-650 (1997). Links
  9. Houghton, J. T. et al. (eds) Climate Change 1995: The Science of Climate Change (Cambridge Univ. Press, 1996). Links
  10. Oppenheimer, M. Nature 393, 325-332 (1998). Links
  11. Boer, G. J., Flato, G. M. & Ramsden, D. Clim. Dyn. (submitted). Links
  12. Hirst, A. C., Gordon, H. B. & O'Farrell, S. P. Geophys. Res. Lett. 23, 3361-3364 (1996). Links
  13. Knutson, T. R., Delworth, T. L., Dixon, K. & Stouffer, R. J. J. Geophys. Res. (submitted). Links
  14. Hegerl, G. et al. Clim. Dyn. 13, 631-634 (1997). Links

Nature © Macmillan Publishers Ltd 1999 Registered No. 785998 England