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Originally posted by soficrow
I am open to seeing some contradictory research. Got links?
Thanks, sofi
"Rate of Ocean Circulation Directly Linked to Abrupt Climate Change in North Atlantic Region"), we still have much to learn about the workings of the vast, unexplored and complex ocean before we can make reliable climate predictions WHOI
Influence of the Atlantic Subpolar Gyre on the Thermohaline Circulation
The new observations - record-high ocean temperatures and salinity - are ascribed to changes in the circulation of the North Atlantic. They have important implications for the climate in northern Europe. On the one hand, the high salinity of the water masses will secure that the strength of the Gulf Stream system is maintained in the upcoming decades. On the other hand, the high temperatures will enhance the impacts of global warming on the climate of the Northern Hemisphere.
Originally posted by soficrow
But earlier reports from a variety of sources said the North Atlantic Current did slow for a short time in 2004 and/or is slowing now.
I can't help noticing that the current spate of denials suspiciously parallels the kind o 'communications strategies' that occur in other scientific disciplines.
Originally posted by Regenmacher
Originally posted by soficrow
But earlier reports from a variety of sources said the North Atlantic Current did slow for a short time in 2004 and/or is slowing now.
I can't help noticing that the current spate of denials suspiciously parallels the kind o 'communications strategies' that occur in other scientific disciplines.
As for cherry picking data from a single short term observation of deep current eddies, I don't see how they can predict much of anything from it, or produce a viable algorithm.
Executive Summary
Recent scientific evidence shows that major and widespread climate changes have occurred with startling speed. For example, roughly half the north Atlantic warming since the last ice age was achieved in only a decade, and it was accompanied by significant climatic changes across most of the globe. Similar events, including local warmings as large as 16°C, occurred repeatedly during the slide into and climb out of the last ice age. Human civilizations arose after those extreme, global ice-age climate jumps. Severe droughts and other regional climate events during the current warm period have shown similar tendencies of abrupt onset and great persistence, often with adverse effects on societies.
Abrupt climate changes were especially common when the climate system was being forced to change most rapidly. Thus, greenhouse warming and other human alterations of the earth system may increase the possibility of large, abrupt, and unwelcome regional or global climatic events. The abrupt changes of the past are not fully explained yet, and climate models typically underestimate the size, speed, and extent of those changes. Hence, future abrupt changes cannot be predicted with confidence, and climate surprises are to be expected.
The new paradigm of an abruptly changing climatic system has been well established by research over the last decade, but this new thinking is little known and scarcely appreciated in the wider community of natural and social scientists and policy-makers. At present, there is no plan for improving our understanding of the issue, no research priorities have been identified, and no policy-making body is addressing the many concerns raised by the potential for abrupt climate change. Given these gaps, the US Global Change Research Program asked the National Research Council to establish the Committee on Abrupt Climate Change and charged the group to describe the current state of knowledge in the field and recommend ways to fill in the knowledge gaps.
Is the Atlantic overturning circulation slowing down? NERC RAPID
Analysis of the first year of data shows that the observing systems is working and able to measure the various components of the flow, using a combination of undersea cable measurements across the Florida Straits, satellite wind measurements,
temperature and salinity measurements from the mooring array, and bottom pressure data also from the array. These and observations at other geographical locations in the North Atlantic suggest that changes are occurring in the MOC, but distinguishing whether these changes are due to variability or persistent trends requires a longer continuous observational record. Model results confirm the need for long-term continuous observations of the MOC if we are to be able to detect whether significant change is occurring.
Carl Wunsch, The Economist and the Gulf Stream
Carl Wunsch usually has very interesting things to say about the climate system, and although his arguments don't necessarily win everyone completely over, they often generate an improvement in the level of scientific discussion. In this week's Economist, he has a letter printed concerning the mis-definition of the 'Gulf Stream' concept in the magazine's climate change survey a couple of weeks ago. This is essentially a reprint of his letter to Nature that was published in 2004, which stated correctly that the Gulf Stream is basically a wind driven phenomenon and will not stop or reverse while the wind still blows and the Earth still turns.
But if this deep circulation doesn't derive its energy from density contrasts, where does it get the energy from? Most of the energy in the oceans is derived from two sources, the winds and the tides. Both of these forces generate small scale turbulence and internal waves which cause mixing of ocean waters. It is this mixing which energetically fuels the deep ocean circulation.
Since the winds will continue to blow and the Earth continue to turn, does this mean that there can't be any changes to the MOC? Emphatically no. The circulation may well derive it's energy from the winds and tides, but it is heavily steered by density contrasts and the stratification of the ocean (witness the difference between the North Pacific and the North Atlantic).
Since the winds will continue to blow and the Earth continue to turn, does this mean that there can't be any changes to the MOC? Emphatically no. The circulation may well derive it's energy from the winds and tides, but it is heavily steered by density contrasts and the stratification of the ocean (witness the difference between the North Pacific and the North Atlantic). Changes in that modulation can have profound effects on the currents, and in particular, additions of fresh water from massive lake drainages (i.e. the 8.2 kyr event) or ice sheet collapses (the Heinrich events) most likely caused severe slowdowns or shutdowns of the MOC in the past. Wunsch is a little sceptical of this research (he calls fresh water the 'deus ex machina' of climate change), but in this he is probably mistaken - for instance, there is enough information from the 8.2 kyr event to reasonably attribute it to the drainage of Lake Agassiz into Hudson Bay.
Thus while density changes don't 'drive' the circulation (in an energetic sense) they can 'drive' (in a modulating sense) changes in that circulation. If this seems complicated, think of the example of greenhouse gases - they don't drive the climate in an energetic sense (the sun does), but they can drive changes in the climate (by modulating radiation flow in the atmosphere).
Originally posted by Regenmacher
Originally posted by khunmoon
This bogus piece of science I just don't buy.
Rather than slinging emotionalisms as proof of flawed science, let's stick to factual matters.
Originally posted by Edn
Regenmacher I don't think you understand how much a "few degrees" can affect a country.
Originally posted by Regenmacher
Originally posted by Edn
Regenmacher I don't think you understand how much a "few degrees" can affect a country.
I wouldn't worry about a long term cold spell anytime soon and your more likely to need a boat in the future.
Global warming: Stormy Scotland up to 72% wetter
Originally posted by soficrow
Sounds like an argument about which scenario is more likely: Waterworld or Day After Tomorrow.
Map of Europe were ocean levels have risen by 150 meters.
The Netherlands and Denmark are gone.
The Alsacian inland sea is rather interesting.
Paris and London are under water. source