Back to the future of climate

October 27, 2020

Between 57 and 55 million years ago, the geological epoch known as the Paleocene ended and gave way to the Eocene. At that time, the atmosphere was essentially flooded by the greenhouse gas carbon dioxide, with concentration levels reaching 1,400 ppm to 4,000 ppm. So it's not hard to imagine that temperatures on Earth must have resembled those of a sauna. It was hot and humid, and the ice on the polar caps had completely disappeared.

The climate in that era provides researchers with an indication as to how today's climate might develop. While pre-?industrial levels of atmospheric CO2 stood at 280 ppm, today's measure 412 ppm. Climate scientists believe that CO2 emissions generated by human activity could drive this figure up to 1,000 ppm by the end of the century.

Using tiny siderite minerals in soil samples taken from former swamps, a group of researchers from ETH Zurich, Pennsylvania State University and CASP in Cambridge (UK) reconstructed the climate that prevailed at the end of the Paleocene and in the early Eocene. Their study has just been published in the journal Nature Geoscience.

The siderite minerals formed in an oxygen-free soil environment that developed under dense vegetation in swamps, which were abundant along the hot and humid coastlines in the Paleocene and Eocene.

To reconstruct the climatic conditions from the equator to the polar regions, the researchers studied siderites from 13 different sites. These were all located in the northern hemisphere, covering all geographical latitudes from the tropics to the Arctic.

Prevailing humidity

"Our reconstruction of the climate based on the siderite samples shows that a hot atmosphere also comes with high levels of moisture," says lead author Joep van Dijk, who completed his doctorate in ETH Professor Stefano Bernasconi's group at the Geological Institute from 2015 to 2018.

Accordingly, between 57 and 55 million years ago, the mean annual air temperature at the equator where Colombia lies today was around 41 °C. In Arctic Siberia, the average summer temperature was 23 °C.

Using their siderite "hygrometer", the researchers also demonstrated that the global moisture content in the atmosphere, or the specific humidity, was much higher in the Paleocene and Eocene eras than it is today. In addition, water vapour remained in the air for longer because specific humidity increased at a greater rate than evaporation and precipitation. However, the increase in specific humidity was not the same everywhere.

Since they had access to siderite from all latitudes, the researchers were also able to study the spatial pattern of the specific humidity. They found that the tropics and higher latitudes would have had very high humidity levels.

The researchers attribute this phenomenon to water vapour that was transported to these zones from the subtropics. Specific humidity rose the least in the subtropics. While evaporation increased, precipitation decreased. This resulted in a higher level of atmospheric water vapour, which ultimately reached the poles and the equator. And the atmospheric vapour carried heat along with it.

Climate scientists still observe the flow of water vapour and heat from the subtropics to the tropics today. "Latent heat transport was likely to have been even greater during the Eocene," van Dijk says. "And the increase in the transport of heat to high latitudes may well have been conducive to the intensification of warming in the polar regions," he adds.

Not enough time to adapt

These new findings suggest that today's global warming goes hand in hand with increased transport of moisture, and by extension heat, in the atmosphere. "Atmospheric moisture transport is a key process that reinforces warming of the polar regions," van Dijk explains.

 "Although the CO2 content in the atmosphere was much higher back then than it is today, the increase in these values took place over millions of years," he points out. "Things are different today. Since industrialisation began, humans have more than doubled the level of atmospheric CO2 over a period of just 200 years," he explains. In the past, animals and plants had much more time to adapt to the changing climatic conditions. "They simply can't keep up with today's rapid development," van Dijk says.

Strenuous search for siderite crystals

Finding the siderites was not easy. For one thing, the minerals are tiny, plus they occur solely in fossil swamps, which today are often found only several kilometres below the Earth's surface. This made it difficult or even impossible for the researchers to dig up siderites themselves. "We made several expeditions to sites where we believed siderites might occur but we found them at only one of those locations," van Dijk says.

Fortunately, one of the study's co-authors - Tim White, an American from Pennsylvania State University - owns the world's largest collection of siderite.
-end-


ETH Zurich

Related Atmosphere Articles from Brightsurf:

ALMA shows volcanic impact on Io's atmosphere
New radio images from ALMA show for the first time the direct effect of volcanic activity on the atmosphere of Jupiter's moon Io.

New study detects ringing of the global atmosphere
A ringing bell vibrates simultaneously at a low-pitched fundamental tone and at many higher-pitched overtones, producing a pleasant musical sound. A recent study, just published in the Journal of the Atmospheric Sciences by scientists at Kyoto University and the University of Hawai'i at Mānoa, shows that the Earth's entire atmosphere vibrates in an analogous manner, in a striking confirmation of theories developed by physicists over the last two centuries.

Estuaries are warming at twice the rate of oceans and atmosphere
A 12-year study of 166 estuaries in south-east Australia shows that the waters of lakes, creeks, rivers and lagoons increased 2.16 degrees in temperature and increased acidity.

What makes Saturn's atmosphere so hot
New analysis of data from NASA's Cassini spacecraft found that electric currents, triggered by interactions between solar winds and charged particles from Saturn's moons, spark the auroras and heat the planet's upper atmosphere.

Galactic cosmic rays affect Titan's atmosphere
Planetary scientists using the Atacama Large Millimeter/submillimeter Array (ALMA) revealed the secrets of the atmosphere of Titan, the largest moon of Saturn.

Physics: An ultrafast glimpse of the photochemistry of the atmosphere
Researchers at Ludwig-Maximilians-Universitaet (LMU) in Munich have explored the initial consequences of the interaction of light with molecules on the surface of nanoscopic aerosols.

Using lasers to visualize molecular mysteries in our atmosphere
Molecular interactions between gases and liquids underpin much of our lives, but difficulties in measuring gas-liquid collisions have so far prevented the fundamental exploration of these processes.

The atmosphere of a new ultra hot Jupiter is analyzed
The combination of observations made with the CARMENES spectrograph on the 3.5m telescope at Calar Alto Observatory (Almería), and the HARPS-N spectrograph on the National Galileo Telescope (TNG) at the Roque de los Muchachos Observatory (Garafía, La Palma) has enabled a team from the Instituto de Astrofísica de Canarias (IAC) and from the University of La Laguna (ULL) to reveal new details about this extrasolar planet, which has a surface temperature of around 2000 K.

An exoplanet loses its atmosphere in the form of a tail
A new study, led by scientists from the Instituto de Astrofísica de Canarias (IAC), reveals that the giant exoplanet WASP-69b carries a comet-like tail made up of helium particles escaping from its gravitational field propelled by the ultraviolet radiation of its star.

Iron and titanium in the atmosphere of an exoplanet
Exoplanets can orbit close to their host star. When the host star is much hotter than our sun, then the exoplanet becomes as hot as a star.

Read More: Atmosphere News and Atmosphere Current Events
Brightsurf.com is a participant in the Amazon Services LLC Associates Program, an affiliate advertising program designed to provide a means for sites to earn advertising fees by advertising and linking to Amazon.com.