| It is more nuanced than that. In any relatively short time span, we may see specific effects (higher temperatures for example) and we may see other effects (increase atmospheric CO2), but this doesn't mean that over a longer term we will continue to see these effects. The other aspect is that there are some very specific physics involved and I have yet to see any discussion over these specific effects. We have seen, in some areas, what appears to be increasingly variable climate conditions. Yet, if one is willing to look into and take the time to investigate the appropriate historical records, these variations have occurred before and were, in fact, much stronger. The affects from these conditions were not felt to the same extent as today because we have vastly different population distributions. Let me give you an example. When I was a child, we had a family regime every spring to prepare for the cyclones that would regularly hit the region in summer. As I moved into my latter teens and forward into my twenties, the regularity changed and we saw quite a diminished number and size of these events. Further time passed and the events grew less frequent but were significantly stronger. The general consensus was that climate variation was getting worse. I dug into the available historical records for the mid 19th century to the early 20th century for the same region. I found that the events during that time were significantly stronger. We talk about category 5 cyclones today and, honestly, I rather have a category 5 than the monster cyclones from 19th century. As far as Greenland is concerned, even with higher global temperatures (as specified by the IPCC), the amount of ice melt is still to be expected in the range of dead skin cells being rubbed off the back of an elephant. The energy requirements are just so unimaginable that if you were to put the entire world's nuclear arsenal to the task, it would barely be a pin prick. |
If you have a basic scientific education you know that any example starting by "when I was a child" is anecdotal evidence and have very limited value because it is akin to confirmation bias and cherry picking.
I'm curious as why you don't apply the principles you were bradishing to the 19th century meteorological data: http://www.isws.illinois.edu/pubdoc/CR/iswscr2011-02.pdf
About Greenland ice sheet disappearing your thinking is oversimplified by looking only at energy required to melt ice. There are several other mechanisms to take into account, for example the increase in cloud cover preventing refreeze at night, or the melted cover snow and ice running into moulins to the ground which then flow under the glacier lubricating it and acceleratiing its motion and thus glacial calving, etc.
When studying a system you need to have basic understanding of second order cybernetics and feedback loops. In climate change positive feedback loop are the reasons past a tipping point there's no stopping it.