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originally posted by: TheRedneck
a reply to: Rezlooper
I was referring to your response concerning the increase of ice mass in Antarctica.
But, if you want to play whack-a-link, we can.
Our global records do not go back 120 years. I am still not convinced our present measurements are truly representative of the global mean temperature. Humans live on land, which covers only 1/3 of the surface, and cannot survive in much of that area due to temperature extremes. Our measurements in those areas where we do not live are either satellite-based (which means indirect measurement) or sporadic weighted readings which are, by definition, subject to error. There is also the noise factor, since all the measurements give mean differentials which are orders of magnitude below typical daily fluctuations. Finally, the stability of the sensors themselves has not been verified to my satisfaction, since many of them are located in areas where the local environment has changed drastically due to expansion of civilization (parking lots instead of open fields, for example).
That is not a direct rebuttal of mean global surface temperature rise; it is a concern over the accuracy of the reports that mean global surface temperature is rising.
originally posted by: TheRedneck
a reply to: Greven
- 1)Water seeks its own level. It is not possible for water to 'pile up' in one location for any appreciable length of time. If you think it is, please take a picture of a pile of water a day post it here.
originally posted by: Greven
originally posted by: TheRedneck
Your source
A federal government report at the time found sea levels around Australia's west and far north have risen the most, with an eight-millimetre rise recorded since the early 1990s.
It is not physically possible to raise sea level in one area more than another without changing the gravitational constant. We do not have the technology to do that. The only known way the gravitational constant can change is by addition or subtraction of external masses (the moon creates high and low tides), and this effect is temporary.
That statement is fact no matter who reports otherwise.
What is orders of magnitude more likely is that the land has settled, lowering by the reported 8mm. Land does not have the viscosity of water and can raise or lower over time. Reclaimed land, especially if part of that reclamation included raising the surface via back filling, is especially susceptible to settling. Oceanfront land is also susceptible to settling as ocean currents tend to remove sediment, causing the land around to slowly settle.
I also find it strange that this problem has worsened to such a degree over about 1/4" of relative water/land level change. If that is so, the whole area has been on the verge of destruction since the 1990s. We can't even grade to that precision.
I hope the residents manage to correct their problems, but I consider those reporting this story to be nothing more than activists for political bull-shavings. It's just more doom-porn propaganda.
Hi. This post is very silly.
1) Sea level is a relative measurement (it's the mean sea level at a particular place - note that this is the mean of high and low tides).
2) Sea level is rising in some places and falling in others (glacial rebound vs land subsidence, for example).
3) There are a lot of gravitational anomalies on Earth anyway (and seen in satellite readings).
4) Currents alter sea levels greatly (if the Gulf Stream ceased flowing, the East Coast could suddenly become inundated with a few feet of water).
originally posted by: TheAmazingYeti
Sure the earth goes through heating a cooling cycles but to deny that we're outside the normal ranges is pure ignorance
originally posted by: TheRedneck
a reply to: Greven
- 4)Local pressure gradients can alter sea level. Current changes can alter pressure gradients for a short time. To maintain a pressure gradient would require something to do so, like a pump continually pumping sea water faster than it could disperse. Care to tell me where these massive pumps are located? We should unplug them.