NY Times: Scientists Say Slower Atlantic Currents Could Mean a Colder Europe Forum: The Environment Some climate experts have said the potential cooling of Europe was paradoxically consistent with global warming caused by the accumulation of heat-trapping "greenhouse" emissions. But several experts said it was premature to conclude that the new measurements, to be described today in the journal Nature, meant that such a change was already under way. The currents, branching off from the Gulf Stream, are part of an oceanic system that disperses tropical heat toward the poles and makes Northern Europe far warmer than its latitude would suggest. Warming, in theory, could stall the salty, sun-heated, north-flowing currents by causing fresh water to build up in high-latitude seas as ice melts and more precipitation falls. The scientists, from the National Oceanography Center in Britain, measured sea temperature, currents and other conditions across the Atlantic from the Bahamas to Africa last year and found a 30 percent drop in the flow of warming waters since a similar set of measurements were taken in 1957. The team, led by Harry L. Bryden, wrote that even though they had measurements from only 5 years out of the past 50, the pattern of change seen at various depths supported the idea that the shift was a significant trend and not random variability. They also cited independent measurements of a long-term decline in the flow of water between some Arctic seas and the North Atlantic as evidence that a slowing of the overall Atlantic circulation was under way. In an accompanying commentary in Nature, Detlef Quadfasel of the University of Hamburg, who was not involved with the British study, said it provided "worrying support for computer models that predict just such an effect in a world made warmer by greenhouse-gas emissions." Other scientists were more cautious. Gavin A. Schmidt, a climate modeler at the National Aeronautics and Space Administration Goddard Institute for Space Studies, said that the estimated decline in ocean circulation should have produced a perceptible decline in surface temperatures, but that no such dip had yet been measured. Robert Dickson, of the British Center for Environment, Fisheries and Aquaculture Science, said that given the complexity and variability of the seas, much more data was needed to determine whether a slowdown was under way. "However much statistical rigor is brought to bear, five transocean sections is still a small number on which to depend," he said.