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I have more than 2 answers (are you surprised?!)CriticalBill wrote: I have two questions
1. Are scientists ever wrong?
2. Are there any pieces of current or future evidence that could make hard core man made climate change believers change their mind and accept that people have little to no significant influence on the climate? What evidence would be needed or are scientists much like religious zealots who will accept nothing but their set-in-stone beliefs?
So, we didn't come from nothing, but the method by which we did come about will remain unanswered for a long time to come, and it may or may not come from science.I'm not saying I know any answers just as I have no clue how we were somehow created (or evolved) from nothing.
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RT, I would love, love, love it if you would add your constructive arguments (you can't say I didn't warn you well enough in advance to get up to speed on your global warming info!) rather than just your humorous distractions. Muchas gracias!residenttroll wrote: I am starting to think the climate change graphs are just Al Gore erection measurements during his massages.
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Yes, that's what I've read too. Wally Broecker's book, The Great Ocean Conveyor, was a great intro to that subject - he's been studying it since the 50's. http://www.amazon.com/Great-Ocean-Conve ... 0691143544lionshead2010 wrote: I had a chance to take introductory level meteorology and oceanography courses not too long ago and was fascinated by the connection between the Earth's prevailing winds and predicatable ocean currents.
As I recall, ocean currents are driven, at least in part, by the salinity of the sea and density issues (I'm no oceanographer).....so as the ice caps melt (either through man-made or natural causes) can we expect a change in ocean currents and prevailing winds? I would think so.
If I remember right, winters are predicted to get milder, unless the conveyor slows dramatically (that isn't expected to happen anytime soon), then it will be deep-freeze instead. Crops will definitely change - already there's talk of England becoming a great wine-growing region and France losing it's magic. Similarly, here in the US, Napa very well may go to crap, and Oregon and Washington become the premiere regions in several decades. Winds, ENSO, etc will all be affected and in turn affect regions differently, in what direction and to what extent is still largely unknown - improving those regional predictions are a hot item of current research. Too, it depends on how soon public opinion and political will is turned and fossil fuel use and deforestation curbed, as business as usual will increase the severity of effects seen in climate and weather, but mitigation will lessen effects seen. For example, the realization that the ozone hole existed, and subsequent drastic reduction in the use of CFC's which exacerbated it, reduced a good deal of warming that would've occurred had that policy not been implemented world-wide (CFCs are potent GHGs).I wonder what winter looks like in a place like the British Isles and Northern Europe if you alter the warming ocean currents that moderate their climate? I wonder if increased growing seasons in the northern climates will impact the ability of farmers in those regions to grow certain crops? How will the change in prevailing winds impact precipitation patterns....and how does that impact agriculture? I don't expect anyone to answer these question but the potential answers are mind boggling for those who like to ponder these things.
Past abrupt climate changes have usually meant reductions in the total number of species and bottle-necking of species that make it through. Already the number of plants and animals that are going extinct every year is increasing. I'm sure we'll survive, but with a great population reduction and drastic lifestyle change.What does global climate change REALLY mean to mankind and the many, many other species that roam this earth? That's the answer I seek.
Boring, maybe. To me, irrelevant, irritating, and frustrating that we continue to be so short-sighted and self-destructive as a species.This stuff makes shirtless congressmen boring. :VeryScared:
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The nature and origin of the AMO is uncertain, and it remains unknown whether it represents a persistent periodic driver in the climate system, or merely a transient feature. Here, we show that distinct, ∼55- to 70-year oscillations characterized the North Atlantic ocean-atmosphere variability over the past 8,000 years. We test and reject the hypothesis that this climate oscillation was directly forced by periodic changes in solar activity. We therefore conjecture that a quasi-persistent ∼55- to 70-year AMO, linked to internal ocean-atmosphere variability, existed during large parts of the Holocene. Our analyses further suggest that the coupling from the AMO to regional climate conditions was modulated by orbitally induced shifts in large-scale ocean-atmosphere circulation.
Paleophysical oceanography is the study of the behavior of the fluid ocean of the past, with a specific emphasis on its climate implications, leading to a focus on the general circulation. Even if the circulation is not of primary concern, heavy reliance on deep-sea cores for past climate information means that knowledge of the oceanic state when the sediments were laid down is a necessity. Like the modern problem, paleoceanography depends heavily on observations, and central difficulties lie with the very limited data types and coverage that are, and perhaps ever will be, available. An approximate separation can be made into static descriptors of the circulation (e.g., its water-mass properties and volumes) and the more difficult problem of determining transport rates of mass and other properties. Determination of the circulation of the Last Glacial Maximum is used to outline some of the main challenges to progress. Apart from sampling issues, major difficulties lie with physical interpretation of the proxies, transferring core depths to an accurate timescale (the "age-model problem"), and understanding the accuracy of time-stepping oceanic or coupled-climate models when run unconstrained by observations. Despite the existence of many plausible explanatory scenarios, few features of the paleocirculation in any period are yet known with certainty.
For the past several decades, oceanographers have embraced the dominant paradigm that the ocean’s meridional overturning circulation operates like a conveyor belt, transporting cold waters equatorward at depth and warm waters poleward at the surface. Within this paradigm, the conveyor, driven by changes in deepwater production at high latitudes, moves deep waters and their attendant properties continuously along western boundary currents and returns surface waters unimpeded to deepwater formation sites. A number of studies conducted over the past few years have challenged this paradigm by revealing the vital role of the ocean’s eddy and wind fields in establishing the structure and variability of the ocean’s overturning. Here, we review those studies and discuss how they have collectively changed our view of the simple conveyor-belt model.
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