Ireland is going to have to move property and key infrastructure such as railway lines away from coastal areas due to climate breakdown, according to Trinity College Dublin’s (TCD) first chair of climate science Prof Karen Wiltshire.
I should have clarified 15°C, which would be a shift of 27°F. It’s hard to overstate how devastating that would be to the ecology of Northern Europe, potentially sending Ireland near permafrost territory and ending agriculture and pastoralism as they know it
It slows down, an effect of cold water from melting ice passing south of greenland, which has a local cooling effect, while the atlantic as a whole gets warmer. Consequence is a greater heat contrast along that front, which may intensify the sequence of low pressures bringing wind and rain, which is what Ireland has just experienced this summer. But the high-resolution models do not show that AMOC stops abruptly, that was a feature of simpler models designed to replicate palaeoclimatic changes at the end of the ice ages, when the amount of ice available to melt was much higher.
Until the Atlantic Meridional Overturning Circulation stops, plunging Ireland’s temperatures by an average of 15°
As a Canadian with Irish grandparents I look forward to claiming my Irish citizenship.
15° cooler (C or F) would be lovely.
I should have clarified 15°C, which would be a shift of 27°F. It’s hard to overstate how devastating that would be to the ecology of Northern Europe, potentially sending Ireland near permafrost territory and ending agriculture and pastoralism as they know it
It slows down, an effect of cold water from melting ice passing south of greenland, which has a local cooling effect, while the atlantic as a whole gets warmer. Consequence is a greater heat contrast along that front, which may intensify the sequence of low pressures bringing wind and rain, which is what Ireland has just experienced this summer. But the high-resolution models do not show that AMOC stops abruptly, that was a feature of simpler models designed to replicate palaeoclimatic changes at the end of the ice ages, when the amount of ice available to melt was much higher.