biffvernon
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- Messages
- 4,607
- Location
- Lincolnshire
Your last point, Flyfisher, neatly sums up the state of politics. Politicians are more concerned about the five year than the 100 year plan. But taking the 'right' decision for the five year may mean that in 100 years billions of people will die. Politicians should be above the concerns of short termism and show leadership for the future of humanity. I wish.
On modelling, nothing is handed to the skeptics. The climate scientists have always been aware of the limitations of their models. There has, for many years, been the twin forecasts of what will happen under existing conditions and what will happen if conditions change. The first has been stated with considerable certainty, the latter hedged about with provisos. That is the nature of science. Here's a significant example; sea level rises with the thermal expansion of the oceans and with addition from meltwater. We can know rather accurately the rise attributable to thermal expansion for a given amount of global warming and we can measure tolerably accurately the rate of ice melt happening now. That lead to the sea level rise forecasts published by the IPPC in AR4 in 1997, complete with error ranges associated with the accuracy of our melt rate measurements. But added to the relevant paragraph was an admission of uncertainty about dynamic processes within the Greenland and West Antarctic Ice Sheets. This was not included in the figures published though the problem was recognised. What appears to be happening is that meltwater on the surface of the ice falls down crevasses and reaches the ice/rock interface at the bottom. This lubricates the glacier allowing it to accelerate, delivering ice to sea and then melting much more quickly. At the seaward end of glaciers, higher sea temperatures are melting the ice faster, reducing the damming effect of ice locked to the sea bed, again allowing the inland glaciers to flow seaward more quickly. These are dynamic effects, subject to positive feedback, accelerating with time. Models that assume constancy soon go awry.
This does present our politicians with a dilemma. In my part of the world, the Lincolnshire Marsh, planning decisions are being taken now on the basis of the published figures in AR4 as to where new building in allowed. With a projected sea level rise of 80cm in 100 years that's not too difficult. Decisions are not being taken on the possibility that we might see a rise of a few metres in that time frame and of a great many metres in a timescale rather shorter than the history of my local market town. Louth may become a port once more and it won't be as a result of the canal restoration society. Planning officers, who I know are scientifically literate, are aware of the possibilities. Elected council members, who ultimately take the decisions, may not be.
I'm interested in this subject for two reasons, My 250 year old house lies at present sea level and I keep it repaired and plant oak trees on my land, perhaps a little form of denial. One of my children is doing research for his Phd on improving the measurement of ice mass balance of Greenland and WAIS.
On modelling, nothing is handed to the skeptics. The climate scientists have always been aware of the limitations of their models. There has, for many years, been the twin forecasts of what will happen under existing conditions and what will happen if conditions change. The first has been stated with considerable certainty, the latter hedged about with provisos. That is the nature of science. Here's a significant example; sea level rises with the thermal expansion of the oceans and with addition from meltwater. We can know rather accurately the rise attributable to thermal expansion for a given amount of global warming and we can measure tolerably accurately the rate of ice melt happening now. That lead to the sea level rise forecasts published by the IPPC in AR4 in 1997, complete with error ranges associated with the accuracy of our melt rate measurements. But added to the relevant paragraph was an admission of uncertainty about dynamic processes within the Greenland and West Antarctic Ice Sheets. This was not included in the figures published though the problem was recognised. What appears to be happening is that meltwater on the surface of the ice falls down crevasses and reaches the ice/rock interface at the bottom. This lubricates the glacier allowing it to accelerate, delivering ice to sea and then melting much more quickly. At the seaward end of glaciers, higher sea temperatures are melting the ice faster, reducing the damming effect of ice locked to the sea bed, again allowing the inland glaciers to flow seaward more quickly. These are dynamic effects, subject to positive feedback, accelerating with time. Models that assume constancy soon go awry.
This does present our politicians with a dilemma. In my part of the world, the Lincolnshire Marsh, planning decisions are being taken now on the basis of the published figures in AR4 as to where new building in allowed. With a projected sea level rise of 80cm in 100 years that's not too difficult. Decisions are not being taken on the possibility that we might see a rise of a few metres in that time frame and of a great many metres in a timescale rather shorter than the history of my local market town. Louth may become a port once more and it won't be as a result of the canal restoration society. Planning officers, who I know are scientifically literate, are aware of the possibilities. Elected council members, who ultimately take the decisions, may not be.
I'm interested in this subject for two reasons, My 250 year old house lies at present sea level and I keep it repaired and plant oak trees on my land, perhaps a little form of denial. One of my children is doing research for his Phd on improving the measurement of ice mass balance of Greenland and WAIS.