The Science of Doom

In the last set of articles we’ve looked at past trends in extreme weather, following the flow of chapter 11 from the 6th assessment report of the IPCC.

How do we know the cause of any changes?

In recent years in most of the media everything that changes is “climate change” which is implicitly or explicitly equated with burning fossil fuels, i.e., adding CO2 into the atmosphere. It’s a genius catchphrase from a marketing point of view, not so helpful for scientific understanding.

I used to prefer the term “anthropogenic global warming” but it has its flaws as well, as some recent trends are believed to be anthropogenic but not from adding CO2 into the atmosphere. An example is changes that result from reduced aerosols in the atmosphere as a result of burning less biomass.

I’ll generally try and stay with “anthropogenic” or “from more CO2”, but there’s no copy editor, so let’s see.

Lots of changes in past climate metrics are simply natural variability. Understanding and quantifying natural variability is a big topic and our knowledge is always going to be imperfect.

For example, there were multi-decadal megadroughts in North America and Europe in the past 1000 years. They were probably “unprecendented” for their time, but clearly weren’t caused by burning fossil fuels.

Here is a reconstruction of the drought index over 1000 years of western North America..

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Global temperature has been rising since around 1900, and CO2 is the principal cause. The physics behind the inappropriately-named “greenhouse effect” is certain, so burning fossil fuels, which adds CO2 to the atmosphere, is certain to increase the surface temperature. I’ve written many articles on that topic on the original blog and shown how the equations are derived (see Notes).

So it should be no surprise to find that there are more extreme hot days and less extreme cold days.

If the temperature goes up, then the number of days with a temperature above say 35°C (86°F) or 40°C (95°F) – or whatever number you want to pick – will increase.

Likewise, the number of days with a temperature below say -10°C (14°F) or -20°C (-4°F) – again, pick a number for your region – will decrease.

Here’s a graph of global land and ocean temperature, extracted from a larger graph in chapter 2 of AR6 (see the Notes below for the full map of changes):

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In #10-#13 we looked at recent trends in droughts.

After covering Tropical Cyclones in #1-#6 it was worth doing a summary in part because AR6’s summary missed some good news from the report itself.

In #7-#9 we looked at extreme rainfall and floods and the summary was important because AR6’s summary missed some good news.

I’ve included the full text from p. 1575 below in the notes.

If you check the table in the notes section of #11 we can see that there were 8 regions identified with a rainfall deficit and 6 regions identified with a rainfall increase. These are also listed in the report section before the summary. However, the summary section only says:

There is medium confidence in increases in precipitation deficits in a few regions of Africa and South America.

Of course, people can read the section before and find out that there were places with a rainfall increase (a decrease in droughts). But anyone limiting themselves to only the “summary” would miss out on this good news.

On soil moisture droughts – agricultural and ecological droughts – they say:

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In #12 we saw that soil moisture droughts – agricultural and ecological droughts – have increased globally.

I’ve been following the flow of AR6 in their discussion of recent trends. They do go on to discuss hydrological droughts without much that’s definitive so perhaps we’ll have a brief look at that in another article, as I’m something of a completionist.

But there’s something important missing from the drought section.

Are plants dying? If not, is there really an increase in soil moisture drought?

Here’s a question from Alexis Berg & Justin Sheffield (2018) to put the problem in a broader context. Here and in all the other papers quoted, bold text is my change:

The notion that a warmer climate leads to a drier land surface, i.e., increased water stress, driven overwhelming by the effect of warmer temperatures on evaporative demand, appears, however, inconsistent with paleo-evidence and vegetation reconstructions for different colder and warmer past climates.

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In #11 we looked at “droughts from rainfall”, i.e., rainfall deficits. There were regional variations but no obvious global trend.

In fact, we expect more rainfall as the earth warms (warm air holds more moisture) so a question to return to in a later article is why there hasn’t been an obvious increase in rainfall, i.e., why there hasn’t been a reduction in “droughts from rainfalls”.

We can measure rainfall. Think – a little bucket that fills up with rain and someone comes around every day, takes a measurement, and writes that number down in a notebook. Of course, the measurement is often more sophisticated in recent times. But we can all appreciate it’s a measurement that can easily be taken.

The other side of soil moisture is evaporation. If it’s hotter, all other things being equal, we expect more evaporation and so on the margins, more places in droughts.

The probem? There is no simple instrument we can stick in the ground next to the rainfall bucket to measure evaporation.

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In #10 we saw an overview which included the idea that a rainfall deficit is one part of a soil moisture deficit. But it’s the part we can measure.

AR6 says, p.1573:

Global studies generally show no significant trends in SPI [drought index for rainfall] time series (Orlowsky and Seneviratne, 2013; Spinoni et al., 2014), and in derived drought frequency and severity data (Spinoni et al., 2019), with very few regional exceptions.

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