It's gonna get worse
University of Cambridge
Researchers have found that 2023 was the hottest summer in the Northern Hemisphere in the past two thousand years, almost four degrees warmer than the coldest summer during the same period.
Although 2023 has been reported as the hottest year on
record, the instrumental evidence only reaches back as far as 1850 at best, and
most records are limited to certain regions.
Now, by using past climate information from annually
resolved tree rings over two millennia, scientists from the University of
Cambridge and the Johannes Gutenberg University Mainz have shown how
exceptional the summer of 2023 was.
Even allowing for natural climate variations over
hundreds of years, 2023 was still the hottest summer since the height of the
Roman Empire, exceeding the extremes of natural climate variability by half a
degree Celsius.
"When you look at the long sweep of history, you can see just how dramatic recent global warming is," said co-author Professor Ulf Büntgen, from Cambridge's Department of Geography. "2023 was an exceptionally hot year, and this trend will continue unless we reduce greenhouse gas emissions dramatically."
The results, reported in the journal Nature,
also demonstrate that in the Northern Hemisphere, the 2015 Paris Agreement to
limit warming to 1.5C above pre-industrial levels has already been breached.
Early instrumental temperature records, from 1850-1900,
are sparse and inconsistent. The researchers compared early instrumental data
with a large-scale tree ring dataset and found the 19th century
temperature baseline used to contextualize global warming is several tenths of
a degree Celsius colder than previously thought. By re-calibrating this
baseline, the researchers calculated that summer 2023 conditions in the
Northern Hemisphere were 2.07C warmer than mean summer temperatures between
1850 and 1900.
"Many of the conversations we have around global
warming are tied to a baseline temperature from the mid-19th century,
but why is this the baseline? What is normal, in the context of a
constantly-changing climate, when we've only got 150 years of meteorological
measurements?" said Büntgen. "Only when we look at climate
reconstructions can we better account for natural variability and put recent
anthropogenic climate change into context."
Tree rings can provide that context, since they contain
annually-resolved and absolutely-dated information about past summer
temperatures. Using tree-ring chronologies allows researchers to look much
further back in time without the uncertainty associated with some early
instrumental measurements.
The available tree-ring data reveals that most of the
cooler periods over the past 2000 years, such as the Little Antique Ice Age in
the 6th century and the Little Ice Age in the early 19th century,
followed large-sulphur-rich volcanic eruptions. These eruptions spew huge
amounts of aerosols into the stratosphere, triggering rapid surface cooling.
The coldest summer of the past two thousand years, in 536 CE, followed one such
eruption, and was 3.93C colder than the summer of 2023.
Most of the warmer periods covered by the tree ring data
can be attributed to the El Niño climate pattern, or El Niño-Southern
Oscillation (ENSO). El Niño affects weather worldwide due to weakened trade
winds in the Pacific Ocean and often results in warmer summers in the Northern
Hemisphere. While El Niño events were first noted by fisherman in the 17th century,
they can be observed in the tree ring data much further back in time.
However, over the past 60 years, global warming caused by
greenhouse gas emissions are causing El Niño events to become stronger,
resulting in hotter summers. The current El Niño event is expected to continue
into early summer 2024, making it likely that this summer will break
temperature records once again.
"It's true that the climate is always changing, but
the warming in 2023, caused by greenhouse gases, is additionally amplified by
El Niño conditions, so we end up with longer and more severe heat waves and
extended periods of drought," said Professor Jan Esper, the lead author of
the study from the Johannes Gutenberg University Mainz in Germany. "When
you look at the big picture, it shows just how urgent it is that we reduce
greenhouse gas emissions immediately."
The researchers note that while their results are robust
for the Northern Hemisphere, it is difficult to obtain global averages for the
same period since data is sparse for the Southern Hemisphere. The Southern
Hemisphere also responds differently to climate change, since it is far more
ocean-covered than the Northern Hemisphere.
The research was supported in part by the European Research Council.