A new paper published in Nature finds climate change over timescales longer than 10 years is "primarily determined by the ocean," which skeptics, including famed Professor Emeritus of Atmospheric Science Dr. William Gray, have been saying for years. According to the paper, "the ocean significantly affects long term climate fluctuations, while the seemingly chaotic atmosphere is mainly responsible for the shorter-term, year-to-year changes."
According to the authors, "Our findings suggest that the predictability of mid-latitude North Atlantic air–sea interaction could extend beyond the ocean to the climate of surrounding continents," corroborating the many papers which have demonstrated that ocean oscillations control land-based climate as well. Ocean oscillations, in turn, have been correlated to solar activity.
According to the authors, "Our findings suggest that the predictability of mid-latitude North Atlantic air–sea interaction could extend beyond the ocean to the climate of surrounding continents," corroborating the many papers which have demonstrated that ocean oscillations control land-based climate as well. Ocean oscillations, in turn, have been correlated to solar activity.
North Atlantic region, dark blue area was used for temperature data, red area for the heat flux. (Credit: C. Kersten, GEOMAR)
July 25, 2013 — Why does hurricane activity vary from decade to decade? Or rainfall in the Sahel region? And why are the trans-Atlantic changes frequently in sync? A German-Russian research team has investigated the role of heat exchange between ocean and atmosphere in long-term climate variability in the Atlantic. The scientists analyzed meteorological measurements and sea surface temperatures over the past 130 years. It was found that the ocean significantly affects long term climate fluctuations, while the seemingly chaotic atmosphere is mainly responsible for the shorter-term, year-to-year changes.
The study appears in the current issue of the journal Nature, and provides important information on the predictability of long-term climate fluctuations.
How do the ocean and atmosphere communicate? What information do they exchange, and what are the results? These are questions that climate scientists must ask, especially if they want to understand the cause of natural climate fluctuations of varying duration. These fluctuations superimpose the general global warming trend since the beginning of industrialization and thus complicate the accurate determination of human influence on the climate. The causes and mechanisms of natural climate variability, however, are poorly understood. A study led by scientists at the GEOMAR Helmholtz Centre for Ocean Research Kiel shows that the ocean currents influence the heat exchange between ocean and atmosphere and thus can explain climate variability on decadal time scales.
The presumption of such predictability potential has been around for more than half a century. In 1964, the Norwegian climate researcher Jacob Bjerknes postulated different causes of climate variability on different time scales. While the atmosphere is mainly causing climate variations on shorter time scales, from months to years, the longer-term fluctuations, such as those on decadal time scales, are primarily determined by the ocean. The first part of this hypothesis has been well studied by now, but the second part still required some verification. "In the current study, we can utilize a new analysis of shipboard measurements, taken since the end of the 19th century, to verify the second part of the Bjerknes hypothesis," says Prof. Mojib Latif of GEOMAR, co-author of the study. "In particular, for the long-term climate variability in the Atlantic sector, the Gulf Stream circulation is of vital importance," said Latif.
Ocean currents affect the surface temperature of the oceans and thus the heat exchange with the atmosphere -- eventually causing climate variations on the adjacent continents. The most evident is an oscillation with a period of 60 years. "Such decadal climate fluctuations are superimposed on the general warming trend, so that at times it seems as if the warming trend slowed or even stopped. After a few decades, it accelerates once again," explains Prof. Latif. "It is important for us to understand these natural cycles, so that we can finally provide better climate predictions as well." One of the major problems, as Latif explained, is that there are just very few long-term oceanic measurements, thereby complicating the analysis and interpretation of climate change signals. Therefore, scientists are using increasingly refined statistical methods to extract more and more information from the available data sets.
"We need both, realistic model simulations and long-term data records, and really sophisticated analysis methods to produce reliable climate predictions. Our work is an additional piece in the giant puzzle of global climate variability, but I am confident that we will be able to extract the secrets underlying the natural climate fluctuations," says Prof. Latif.
Journal Reference:
North Atlantic Ocean control on surface heat flux on multidecadal timescales
- Nearly 50 years ago Bjerknes1 suggested that the character of large-scale air–sea interaction over the mid-latitude North Atlantic Ocean differs with timescales: the atmosphere was thought to drive directly most short-term—interannual—sea surface temperature (SST) variability, and the ocean to contribute significantly to long-term—multidecadal—SST and potentially atmospheric variability. Although the conjecture for short timescales is well accepted, understanding Atlantic multidecadal variability (AMV) of SST2, 3 remains a challenge as a result of limited ocean observations. AMV [Atlantic multidecadal variability] is nonetheless of major socio-economic importance because it is linked to important climate phenomena such as Atlantic hurricane activity and Sahel rainfall, and it hinders the detection of anthropogenic signals in the North Atlantic sector4, 5, 6. Direct evidence of the oceanic influence of AMV can only be provided by surface heat fluxes, the language of ocean–atmosphere communication. Here we provide observational evidence that in the mid-latitude North Atlantic and on timescales longer than 10 years, surface turbulent heat fluxes are indeed driven by the ocean and may force the atmosphere, whereas on shorter timescales the converse is true, thereby confirming the Bjerknes conjecture. This result, although strongest in boreal winter, is found in all seasons. Our findings suggest that the predictability of mid-latitude North Atlantic air–sea interaction could extend beyond the ocean to the climate of surrounding continents.
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