In the Ocean, Clues to Change. The startling reality is that in 2014, we know more about the surface of Mars than about the depths of the ocean. And that deficit is a huge problem as scientists try to understand how human activity is changing the planet. As many people know, the warming of the earth’s surface has slowed sharply over recent years. That slowdown did not match past computer projections of what the climate was supposed to do under the influence of greenhouse gases, and scientists have been struggling to explain it. Their inability to do so raises questions about the reliability of the computer models on which long-term climate projections are based. Moreover, that scientific problem has become a political problem. “Global warming stopped 15 years ago!” is the favorite battle cry for climate-change skeptics these days, continually cited by politicians who want to block action on emissions. In fact, global warming has not stopped. The greenhouse gases released by humans are still trapping heat, and the vast bulk of it is being absorbed by the ocean, as has always been the case. Researchers have deployed more than 3,000 robotic floats that can measure the temperature in the upper layers of the ocean, and they show continual warming there. This documented ocean warming is hard evidence that scientists have gotten the basic story right when it comes to the effects of human emissions. It is also a problem in itself, because water expands as it heats up, so the warming is a major factor behind the rise of sea level — which, in turn, has worsened flooding from storms like Hurricane Sandy. Despite the oceanic heating, it is true that at the surface of the planet, the increase of temperature has slowed quite a bit from the torrid pace of earlier decades. That has been a surprise, and trying to understand it has become an intense scientific focus. The natural variability of climate could be playing a big role. The Pacific Ocean, in particular, oscillates in ways that can strongly influence the temperature of the atmosphere. The cycling between El Niño and La Niña conditions is one of those oscillations, and over the past decade or so, La Niña, which has a cooling influence on global climate, has predominated. Some scientists think the deep ocean is playing a significant role, absorbing heat that would otherwise be showing up at the surface. And the available evidence suggests this is the case, but measurements of the deep ocean are scant. That is where the prototype robotic floats, developed at the Scripps Institution of Oceanography, come in. The idea is to supplement the older robots that are already prowling the ocean. That system, known as Argo, is one of the scientific triumphs of the age, but even the most advanced of the floats can dive only a little more than a mile, so they miss the bottom half of the sea. Developing robots able to go deeper has been a technical challenge, but scientists think they are about to lick it, permitting temperature measurements of virtually the entire ocean — a milestone in science. The experts say a replacement for the pollution-measuring satellite that exploded is also an urgent priority. While scientists scramble for better information, this might be the most important thing for citizens to know about the warming hiatus: It has happened before. In fact, surface warming has always proceeded in fits and starts, with the longest hiatus lasting roughly 30 years, from the 1940s to the 1970s. Scientists do not really understand that one, either. But it ended, and a period of extremely rapid warming followed. nytimes/2014/08/12/science/in-the-ocean-clues-to-change.html?ref=earth
Posted on: Sat, 30 Aug 2014 07:40:41 +0000
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