A provocative piece by @TedNordhaus in today's Wall Street Journal makes the case that effective climate policy is one that promotes human prosperity – particularly in poorer countries – while adopting policies to invest in and promote clean energy. wsj.com/articles/ignor… 1/7
The piece argues continuing political, economic and technological modernization, not a radical remaking of society, is key to both slowing climate change and adapting to it. It suggests a richer world is one of lower population growth, higher equality and adaptive capacity. 2/7
This is also the assumption underlying the future scenarios used by the IPCC. The most sustainable future (SSP1) with the easiest path to deep decarbonization is also one of the highest economic growth and lowest population scenarios considered: 3/7
Nordhaus argues "Long-term economic growth is associated with both rising per capita energy consumption and slower population growth. For this reason, as the world continues to get richer, higher per capita energy consumption is likely to be offset by a lower population." 4/7
Furthermore, a richer world is one where it is easier to decouple the growth of human welfare from environmental degradation, where "energy consumption should be less carbon-intensive than it would be in a poorer, less technologically advanced future." 5/7
There are strong linkages between growth and adaptive capacity: "In Bangladesh, 300,000 people died in Cyclone Bhola in 1970, when 80% of the population lived in extreme poverty. In 2019, with less than 20% in extreme poverty, Cyclone Fani killed just five people." 6/7
Of course, building human prosperity in a way that also reduces global emissions requires substantial policy interventions. The world has started bending the curve away from high emissions outcomes with investments in clean energy. This needs to have to expand dramatically: 7/7
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A recent viral graph found fewer days in the contiguous US above 95F/100F/105F today than in the 1930s.
But the graph is misleading – it fails to correct for changing measurement times and techniques, and overstates regional warmth. I take a deep dive at The Climate Brink.
First, the graph uses "raw" daily station data. But almost all US stations shifted their observation times from late afternoon to early morning between 1950 and 1980, resulting in a cool bias. New electronic sensors installed after 1980 also read maximum temps about 0.5C cooler.
Second, the viral graph (by CFACT analyst Chris Martz) does not provide a representative assessment of US temperatures. It draws from stations that are concentrated in the Midwest where the effects of the 1930s Dust Bowl era were most pronounced.
With all the July model runs now in, it is very likely that 2026 will see the largest El Niño event since records began in the late 1800s – and potentially by a truly mind-blowing margin. The median estimate is now 3.6C, roughly 0.8C hotter than the prior record (2.75C).
The 2026/2027 El Niño event has already grown faster than any prior events (at least on an ONI basis). Here its observed and projected future evolution compared to the strongest prior El Niño events in recorded history.
Currently 13 out of 14 dynamical models expect a record setting event based on the Niño 3.4 region sea surface temperature anomalies (ONI), with overall odds of a record sitting at 91% across all 667 model ensemble members.
Heat waves are driven by weather patterns but occur on the backdrop of a rapidly warming world. Without climate change the current European heat wave would have been ~3.2 °C (5.8 °F) cooler.
Heat impacts are non-linear, so this higher severity can lead to much greater suffering
Europe has been warming at a much faster rate than the world as a whole: roughly twice as fast as the global average, and 40% faster than the global land average.
This warming has been fastest in the winter months – driven in part by greater absorption of sunlight with less winter snow cover – but has been rapid year-round:
Today the @WMO released projections of where temperatures may end up over the next five years (baed on 13 different models and 250 ensemble members).
Their estimates for 2026 and 2027 are quite close to my (updated) ones:
My 2026 uncertainties are narrower as I'm using the first four months of data for the year to constrain my estimate. I also have a more up-to-date El Nino forecast than the WMO models (which are initialized considerably earlier and don't reflect the likely development of a very strong event.
@WMO I've also updated my estimates using data through April and the latest El Nino forecasts, which slightly bumped up the 2026 and 2027 central values compared to my last estimate that only used data through March: theclimatebrink.com/p/higher-warmi…
The arc of the scenario universe is long, but it bends inevitably toward more realistic emissions.
A new paper outlining the emissions scenarios we will be using in the upcoming IPCC AR7 report notes that "the CMIP6 high emission levels (quantified by SSP5-8.5) have become implausible".
It outlines a yet-to-be-released high emissions scenario notably lower than the one (SSP5-8.5) used in the prior IPCC 6th Assessment Report:
This is a change that a number of us in the community have long advocated, going back to Justin Ritchie's work in 2017.gmd.copernicus.org/articles/19/26…
And in 2020 Glen Peters and I published a piece in Nature arguing that high emissions scenarios were no longer "business as usual", and that more realistic emissions make for better climate policy: nature.com/articles/d4158…
El Niño is coming, and it is shaping up to be a big one.
Over at The Climate Brink I've put together a compilation of the latest forecasts by different modeling groups. They suggest that we might see an event comparable in strength to what we saw in 2016.
This is based on a collection of 11 different models (and 455 individual ensemble members) all updated since the start of March. I've put an interactive version of the data up on the Climate Dashboard here: dashboard.theclimatebrink.com/#enso
While there remains a big spread in models (and some models only run through August), more than half the runs show a strong (>1.5C Nino3.4) event developing by August and a very strong event (>2C) by the end of the year.