Archives de catégorie : climate and geology

climate and geology

The Anthropocene is dead. Long live the Anthropocene

by P. Voosen, Mar 5, 2024 in AAASScience

For now, we’re still in the Holocene.

Science has confirmed that a panel of two dozen geologists has voted down a proposal to end the Holocene—our current span of geologic time, which began 11,700 years ago at the end of the last ice age—and inaugurate a new epoch, the Anthropocene. Starting in the 1950s, it would have marked a time when humanity’s influence on the planet became overwhelming. The vote, first reported by The New York Times, is a stunning—though not unexpected—rebuke for the proposal, which has been working its way through a formal approval process for more than a decade.

“The decision is definitive,” says Philip Gibbard, a geologist at the University of Cambridge who is on the panel and serves as secretary-general of the International Commission on Stratigraphy (ICS), the body that governs the geologic timescale. “There are no outstanding issues to be resolved. Case closed.”

 

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climate and geology

How Geology And Rocks Tell The Story Of Earth’s Climatic Past

by. J. Duhamel, Mar 4, 2024 in ClimateChangeDispatch

I am a geologist which means I have rocks in my head and some of those rocks have recorded the climate history of Earth. Here is their story.

We will start with the big picture.

The graphic below [after the jump] shows the estimated temperature and atmospheric carbon dioxide (CO2) content for the past 600 million years. [emphasis, links added]

The blue line is the estimated temperature; the black line is the estimated CO2 content of the atmosphere.

Notice that for much of the past 600 million years, the temperature has been about 12°C warmer than it is now and life has flourished. (Note that the climate crazies claim that if the global temperature increases by 2°C above present, we will die.)

CO2 temps graph

Click to enlarge

The dips in the temperature curve are ice ages. Ice ages have occurred on a cycle of about 145 million years. Ice ages consist of glacial epochs and warmer interglacial periods. We are now in an interglacial period. (In the popular vernacular, glacial epochs are often called “ice ages.”)

The glacial epoch cycle happens whenever our solar system, in its travels around the center of our galaxy, goes through some spiral arms of the galaxy with very dense clusters of stars that bombard the Earth with more cosmic rays, which produce more clouds and other effects in the atmosphere, which limit the amount sunlight that gets to Earth’s surface.

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climate and geology

Geologically Generated Ice Cycles And Climate-Related Phenomena

by J.E. Kamis, Feb 28, 2024 in ClimateChangeDispatch

The term “Ice Age” implies that covering Earth’s surface with ice and then melting it is a single event.

As explained below, this process is not a single event but rather a reoccurring cycle that has three distinct phases: Ice Melt/End Phase, Ice Increase/Recovery Phase, and Normal Ice Extent/Stable Phase.

Ice Melt/End Phase

Approximately every 100,000 years, the Earth’s glaciers and seas reach their maximum extent. Suddenly and within 5,000 years nearly all the ice melts. I term this the Ice Melt Phase.

So, what causes this rapid melting of the ice? It is a geologically induced pulse of heat and gas emitted from all of Earth’s geological features. A more detailed explanation of the Ice Melt Phase follows.

In 1941 Serbian mathematician Milutin Milankovitch discovered that every 100,000 years, the Earth’s orbit around the sun, tilt angle of its axis, and wobble-type movement around the axis changes. Scientists called this process a Milankovitch Cycle.

Milankovitch concluded that these astronomical changes affected Earth’s long-term climate. Others have shown that these astronomical changes also act to greatly increase the gravitational stress on Earth.

Figure 1. 50,000-mile-long interconnected network of ocean floor fault zones and ice extent during an Ice Cycle. (Image credit Wikipedia, some labeling by J. Kamis).

In my opinion, this stress activates all of Earth’s geological features, most importantly the 50,000-mile-long interconnected network of deep ocean-floor fault zones (Figure 1). These fault zones form the boundary between continents and large segments of ocean-floor rock layers.

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better to know...?, Biodiversity, climate and geology

A Curious Paleo Puzzle

by W. Eschenbach, Feb 23, 2024 in WUWT

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A final possibility, of course, is that the warming has little to do with CO2 and that the CO2 levels are a function of temperature and not the other way around …

I titled this post “A Curious Paleo Puzzle”. That’s the puzzle. How can an increase of 13 W/m2 in CO2 forcing cause an increase of 115 W/m2 of upwelling surface longwave radiation?

All suggestions welcome.

 

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climate and geology

Iceland, the island of danger

by B. Van Vliet-Lanoë & A. Préat, Feb 8, 2024 in ScienceClimatEnergie

Main topic : Iceland attracts tourists as much as it does scientists tasked with forecastingthe significant natural hazards inherent in its unique geological context. There’s not aweek goes by when Iceland doesn’t feature prominently in the media, and even more so today with the evacuation of the population on 11 November following the awakening ofthe volcano at Grindavik, 40km southwest of Reykjavik.

The current eruption has been forecast since 21 July 2023, and was activated in December and on 14 January 2024. This is neither the first nor the last time that volcanism has made or will make news. Grindavik isnot the only eruption underway: between 40 and 50 of the 1,330 known volcanoes on Earth are erupting at any one time. This eruptive activity is accompanied by ‘disastrous’ effects such as frequent earthquakes, sulphur and ash aerosols, sub-glacial melting of the ice caps, glacio-isostatic discharges, and uplift… Yes, Iceland is under close survey… because it is located on an active hot spot.

Laki or ‘Lakagigar’ is a volcanic system in the graben across Iceland. Colossal fissure erupti

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climate and geology, climate-debate

Mount Pinatubo eruption caused the major East China flood in 1991

by C. Xing & F. Liu, Jan 2023 in InnovativeGeoscience

The devastating flood of 2020 along the Yangtze River serves as a painful reminder of the 1991 East China’s largest flood. The latter event profoundly impacted the Yangtze-Huaihe River basins (YHRBs), causing extensive damage to both human lives and property1. The flood engulfed numerous villages and cities across seven provinces in East China, affecting over 15,000,000 hectares of farmland and approximately 100 million people. In response, millions of individuals in Anhui and Jiangsu provinces were forced to evacuate, with some seeking refuge on the banks of the Huaihe River. Gaining a comprehensive understanding of the contributing factors to this historically significant flood will enhance our ability to predict the East Asian summer monsoon and mitigate related climate disasters. Over the past three decades, this pursuit has been a persistent challenge1,2,3.

The 1991 East China flood was attributed to prominent intraseasonal oscillations, as evidenced by three episodes of heavy rain occurring from mid-May to mid-July over the YHRBs2, primarily linked to the persistent Meiyu front during early July1. The stable western Pacific subtropical high (WPSH), which plays a crucial role in influencing the East Asian monsoon by altering the convergence of southeasterly and southwesterly, provided substantial support for the prolonged existence of the Meiyu front in 19911; However, the reason behind the prolonged stability of the WPSH during that specific period remains a mystery.

No internal climate variability modes were reported to be in their most flood-favorable conditions during 1991, and the effect of external forcing on this flood disaster was not taken into consideration at all. Half a month before the flood, the Mount Pinatubo (located at 120.4ºE, 15.1ºN) in Luzon, the Philippines, explosively erupted on June 15th, 1991, which later is known as one of the strongest volcanic eruption in the past century. This eruption released approximately 20 Tg of SO2 into the tropical stratosphere4, which can form stratospheric aerosol that impact the global radiative balance. The stratospheric volcanic aerosol acts as a major forcing on the climate by cooling the global surface and slowing down the water cycle on annual to decadal timescales5. However, it remains unclear whether explosive volcanic eruptions have short-term impacts on the climate, particularly on the intraseasonal timescale.

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climate and geology

The MSM Has Memory-Holed Tonga’s Warming Effects On World Temps

by E. Erickson, Aug 14, 2023 in ClimateChangeDispatch

On Jan. 15, 2022, the underwater Hunga Tonga–Hunga Ha’apai volcano in the Pacific exploded. The volcano triggered tsunamis in the South Pacific and sent a massive plume of water vapor into the stratosphere.

Over the past year, scientists have increased the estimates of how much water vapor went into the stratosphere. That water vapor, every scientist agrees, warms the planet. [emphasis, links added]

Originally, scientists estimated 50 million metric tons of water went into the atmosphere.

Now, revised estimates are at 150 million metric tons, which equates to 40 trillion gallons of water injected into the stratosphere.

Over the past year, dozens of scientists have produced papers warning that the summer of 2023 and possibly into the next decade would be abnormally hot.

Scientists suggest the global temperature could increase more than 1.5 degrees Celsius.

In fact, that is exactly what is happening. Up until the summer heat wave, news reports noted the expected increase in temperatures due to the volcano.

But as the heat wave began, as predicted, the volcano and its water vapor disappeared from coverage.

Now, in the progressive spirit of never letting a crisis go to waste, the American and European press corpshave begun a full-court press on climate change.

Instead of the volcano, people, capitalism, and oil companies are to blame for the heat wave.

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better to know...?, climate and geology, climate-debate

Where Does Ocean Heat Come From?

by Dr M. Wielicki, May 24, 2023 in ClimateChangeDispatch

First, do we really know the temperature and thus heat content of the ocean?

The ocean is vast and covers ~70% of the Earth’s surface, making it the largest system on the planet. Despite its size, only a small portion of the ocean has been explored and mapped in detail.

It is estimated that <20% of the world’s oceans have been mapped and explored to date. [emphasis, links added]

This is largely due to the difficulties and challenges associated with ocean exploration, such as the high pressure and extreme environments found in the deep ocean, as well as the high cost of research vessels, equipment, and technology.

Most of the ocean that has been explored in detail is located near the coasts or in shallow waters, where it is more accessible to research vessels and equipment, but usually far away from the heat sources of mid-ocean ridges.

The deep ocean, which makes up the majority of the ocean’s volume, remains largely unexplored, with less than 5% of the ocean floor having been mapped in high resolution.

Advances in technology, such as underwater drones and submersibles, are helping to improve our understanding of the ocean and its ecosystems, and it is likely that our knowledge of the ocean will continue to expand in the coming decades.

Temperature measurements in the ocean are typically taken using a variety of instruments. These instruments can be deployed from research vessels or from moored or drifting buoys, and they collect temperature data at different depths throughout the ocean.

The amount of the ocean that is measured for temperature varies depending on the method of measurement and the specific objectives of the research.

However, it is estimated that significantly less than 10% of the world’s oceans have been sampled for temperatures at depths greater than 2,000 meters.

Despite the relatively limited coverage of temperature measurements in the deep ocean, there are ongoing efforts to improve our understanding of the ocean’s temperature structure and variability.

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climate and geology

New Book: ‘Geological Impacts On Climate’ Now Available

by T. Richard, Jul 5, 2023 in ClimateChangeDispatch

A new book by Climate Change Dispatch writer and contributor James Kamis is now available!

Kamis has been a leading proponent of the theory that geological events heavily influence the planet’s climate, something only now being recognized by the so-called science ‘gatekeepers.’

The book, “Geological Impacts on Climate,” provides evidence that increased tectonic activity, whether locally or globally, equates to more heat and chemically charged, heated fluid release from active geological features into our oceans, sub-glacial polar areas, and atmosphere.

This altered heat and fluid have acted to significantly influence, and in some cases, completely control climate and climate-related events.

To describe this new theory, the term “Plate Climatology” was coined in 2014 and published on Climate Change Dispatch.

Sections of the book that substantiate this theory include:

The building block principles of the theory were conceived by integrating Kamis’ observations and ideas with information from various scientific disciplines.

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better to know...?, climate and geology, climate-debate

Scientists Say A 6°C Warmer-Than-Today Arctic Is ‘Optimal’ For Thermophile Species

by K. Richard, Apr 6, 2023 in NoTricksZone

Back in the Early Holocene, when CO2 levels were said to be ~255 ppm, Arctic Svalbard was warm enough to accommodate abundant numbers of thermophiles, or warmth-demanding species. Only “remnants” of these species and their habitat exist in today’s much-colder Arctic.

With the exception of a few centuries in recent millennia, today’s Svalbard (Arctic) is the most glaciated it has been in the last 10,000 years (see the blue trend line in the below chart from Brožová et al., 2023).

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This region is today about 6°C colder than it was during the early Holocene (~10,000 to 8,000 years ago), a climatic period scientists characterize as an optimum, or “most favorable,” for a “rich species pool” of thermophiles.

The sea surface temperatures (SSTs) in the western Barents Sea were as warm as 13°C and “sea ice-free during most of the mid-Holocene” (Łącka et al., 2019). In contrast, today’s SST in this region are as cold as they were during the last glacial (2-4°C), when CO2 hovered near 200 ppm. Rapid double-digit SST fluctuations, varying from 3 to 13°C, have been ongoing throughout the Holocene.

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climate and geology

New Study: Roman And Medieval Warm Periods Were 2.8°C Warmer Than 1970-2000 In Central China

by K. Richard, Mar 13, 2023 in NoTricksZone

A series of paleoclimate lake reconstructions across China in recent years have failed to support the global-scale warming narrative.

Per a new lake temperature reconstruction (Li et al., 2023) from Central China, there were distinct “warm intervals during the RWP [Roman Warm Period] (403–413 CE), with a temperature 2.89°C higher than that of the mean for 1970–2000 CE, and during the MWP [Medieval Warm Period] (864–882 and 965–994 CE), when the temperature was 2.81°C higher.”

There are 8 other lake sediment reconstructions from the region (Qinghai, Gahai, Sugan, Kusai, Tiancai, Heiahi, Lugu, Cuoqia) documented in the study. None of the 8 are shown to have a modern temperature uptick that would support the claims of an unusually warm modern climate relative to past millennia.

climate and geology

Elegantly modeling Earth’s abrupt glacial transitions

by American Institute of Physics, Mar 7, 2023 in ScienceDaily

Proxy data — indirect records of the Earth’s climate found in unlikely places like coral, pollen, trees, and sediments — show interesting oscillations approximately every 100,000 years starting about 1 million years ago. Strong changes in global ice volume, sea level, carbon dioxide concentration, and surface temperature indicate cycles of a long, slow transition to a glacial period and an abrupt switch to a warm and short interglacial period.

Milutin Milankovitch hypothesized that the timing of these cycles was controlled by the orbital parameters of the Earth, including the shape of its path around the sun and the tilt of the planet. A slightly closer orbit or more tilted planet could create a small increase in solar radiation and a feedback loop that leads to massive changes in climate. This idea suggests that there may be some predictability in the climate, a notoriously complex system.

In Chaos, by AIP Publishing, Stefano Pierini of Parthenope University of Naples proposed a new paradigm to simplify the verification of the Milankovitch hypothesis.

“The main motivation behind this study was the wish to characterize and illustrate the Milankovitch hypothesis in a simple, elegant, and intuitive way,” Pierini said.

Many models suggest that Milankovitch is correct; however, such methods are often detailed and study specific. They incorporate climate feedback loops — for example, increased ice cover reflects more radiation back into space, leading to further cooling and more ice cover — as threshold crossing rules. This means that an abrupt jump in climate only occurs once a parameter reaches a given tipping point.

Pierini’s “deterministic excitation paradigm” combines the physics concepts of relaxation oscillation and excitability to link Earth’s orbital parameters and the glacial cycles in a more generic way. The relaxation oscillation component describes how the climate slowly returns to its original glacier state after it is disturbed. At that point, the excitability piece of the model captures the external orbital changes and triggers the next glacial cycle.

By using his own threshold crossing rules and adopting a classical energy-balance model, Pierini obtained correct and robust timing of the most recent glacial cycles.`

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climate and geology

Early Cretaceous shift in the global carbon cycle affected both land and sea

by University of Nebraska-Lincoln, Feb 22, 2023 in ScienceDaily

Geologists doing fieldwork in southeastern Utah’s Cedar Mountain Formation found carbon isotope evidence that the site, though on land, experienced the same early Cretaceous carbon-cycle change recorded in marine sedimentary rocks in Europe. This ancient carbon-cycle phenomenon, known as the ‘Weissert Event’ was driven by large, sustained volcanic eruptions in the Southern Hemisphere that greatly increased carbon dioxide levels in the atmosphere and produced significant greenhouse climate effects over a prolonged time.

Scientific research in recent decades has confirmed that major changes in the global carbon cycle caused significant changes in the Earth’s atmosphere and oceans 135 million years ago, during the early Cretaceous Period. A range of questions remain about the details of climate change dynamics in that era. This new research, involving wide-ranging chemical and radioactivity-based analyses of rock strata in Utah’s Cedar Mountain Formation, helps fill in that knowledge gap by confirming that such carbon-cycle shifts were recorded on land in ancient North America.

The carbon cycle is one of Earth’s fundamental environmental phenomena, involving the ongoing transfer of carbon among the atmosphere, oceans and living organisms, as well as soils, sediments and rocks in the solid Earth. The cycle is crucial to biological processes for living things on land and sea. When large-scale changes in the cycle occur, they can produce major shifts in climate and the oceans’ biological conditions.

“We’re studying how the global carbon cycle has functioned in the past, how changes are recorded in the sedimentary rocks around the world,” said Joeckel, a professor in the School of Natural Resources at Nebraska. The environmental phenomena he and his colleagues analyzed “are exactly the kind of things we’re talking about today, as people increase the input of carbon dioxide into the atmosphere at a much-accelerated rate by burning fossil fuels.”

Joeckel, the Nebraska state geologist, headed the Utah fieldwork and organized the study, published as a peer-reviewed paper in a special February issue of the journal Geosciences.

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climate and geology, climate-debate

Keeling Curve CO2 Measurements Halted By Mauna Loa Eruption

by BigIslandVideoNews, Nov 29, 2022

(BIVN) – The collection of data for use in the decades-long record of atmospheric carbon dioxide, known famously as the Keeling Curve, was cut off on Monday night, as lava from the latest Mauna Loa eruption flows down the mountain.

The lava crossed the Mauna Loa Weather Observatory Road at approximately 8 p.m. in the evening, cutting off power to observatory facilities and equipment.

Researchers at Scripps Institution of Oceanography at UC San Diego, which started collecting the Keeling Curve data at the site in 1958, say they “are exploring options regarding the relocation of measurement equipment.” From the Tuesday announcement:

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See also Mauna Loa eruption cuts access, power to Mauna Loa Observatory

Australia, climate and geology

An Inconvenient Tree: Is Climate Change Driving Worse Floods

by E. Worrall, Nov 27, 2022 in WUWT

Does evidence of past extreme floods invalidate claims that climate change is making floods worse?

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Could volcanic activity be a contributor to major floods in Australia? Australia is on the South Western edge of the Ring of Fire. While the Australian mainland is not very volcanically active, there have been some spectacular eruptions in our neighbourhood, such as the infamous Krakatoa eruption in 1883, or the 1815 Tambora Eruption, which is blamed for causing famine in the United States in 1816, “The Year Without a Summer”.

A notable volcanic eruption occurred at the start of 2022 – The Hunga Tonga eruption. JoNova published an intriguing comparison between the volcanic ash distribution from the Hunga Tonga eruption in January 2022, and 2022 rainfall anomalies across Australia. Hunga Tonga was light on sulphates, but the blast threw unprecedented amounts of water into the stratosphere. Where I live, on the Southern edge of the volcanic debris distribution, we’ve had some spectacular sunsets over the last year.

The apparent overlap between rainfall anomalies and volcanic debris could be a coincidence – but the comparison is visually intriguing.

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climate and geology

Earth can regulate its own temperature over millennia, new study finds

by Massachusetts Institute of Technology, Nov16, 2022 in ScienceDaily

The Earth’s climate has undergone some big changes, from global volcanism to planet-cooling ice ages and dramatic shifts in solar radiation. And yet life, for the last 3.7 billion years, has kept on beating.

Now, a study by MIT researchers in Science Advances confirms that the planet harbors a “stabilizing feedback” mechanism that acts over hundreds of thousands of years to pull the climate back from the brink, keeping global temperatures within a steady, habitable range.

Just how does it accomplish this? A likely mechanism is “silicate weathering” — a geological process by which the slow and steady weathering of silicate rocks involves chemical reactions that ultimately draw carbon dioxide out of the atmosphere and into ocean sediments, trapping the gas in rocks.

Scientists have long suspected that silicate weathering plays a major role in regulating the Earth’s carbon cycle. The mechanism of silicate weathering could provide a geologically constant force in keeping carbon dioxide — and global temperatures — in check. But there’s never been direct evidence for the continual operation of such a feedback, until now.

The new findings are based on a study of paleoclimate data that record changes in average global temperatures over the last 66 million years. The MIT team applied a mathematical analysis to see whether the data revealed any patterns characteristic of stabilizing phenomena that reined in global temperatures on a geologic timescale.

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Journal Reference:

  1. Constantin W. Arnscheidt, Daniel H. Rothman. Presence or absence of stabilizing Earth system feedbacks on different time scales. Science Advances, 2022; 8 (46) DOI: 10.1126/sciadv.adc9241
climate and geology, climate-debate

Nature Unbound I: The Glacial Cycle

by Javier, Oct 24, 2016 in ClimateEtc.

Insights into the debate on whether the Holocene will be long or short.

Summary: Milankovitch Theory on the effects of Earth’s orbital variations on insolation remains the most popular explanation for the glacial cycle since the early 1970’s. According to its defenders, the main determinant of a glacial period termination is high 65° N summer insolation, and a 100 kyr cycle in eccentricity induces a non-linear response that determines the pacing of interglacials. Based on this theory some authors propose that the current interglacial is going to be a very long one due to a favorable evolution of 65° N summer insolation. Available evidence, however, supports that the pacing of interglacials is determined by obliquity, that the 100 kyr spacing of interglacials is not real, and that the orbital configuration and thermal evolution of the Holocene does not significantly depart from the average interglacial of the past 800,000 years, so there is no orbital support for a long Holocene.

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climate and geology

Another Study Says Europe Was At Times Warmer During The Last Glacial When CO2 Levels Were 40% Lower

by K. Richard, Oct 24, 2022 in NoTricksZone

The Earth was still in ice age conditions 14,700 to 12,900 years ago, or during the “Bolling interstadial.” CO2 hovered near 230 ppm at that time, and yet “continental Europe was a few degrees warmer than present” (Toth et al., 2022).

In recent years there have been multiple studies detailing a European climate that was as warm or warmer than today during the late Pleistocene ice age.

The latest study, Toth et al., 2022, uses chironomid proxy evidence to reconstruct summer temperatures at a lake site in the Eastern Carpathians.

These authors report that “continental Europe was a few degrees warmer than present during the Bolling interstadial,” and there were slightly (0.5°C) warmer-than-today periods (e.g., ~16,300 years ago) at the study site. The warming events were both pronounced (5°C) and abrupt.

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better to know...?, climate and geology

Ultra-depleted hydrogen isotopes in hydrated glass record Late Cretaceous glaciation in Antarctica

by D.A. Nelson et al. , Sept 7, 2022 in NatureCommunications

Abstract

The Early Jurassic Butcher Ridge Igneous Complex (BRIC) in the Transantarctic Mountains contains abundant and variably hydrated silicic glass which has the potential to preserve a rich paleoclimate record. Here we present Fourier Transform Infrared Spectroscopic data that indicates BRIC glasses contain up to ~8 wt.% molecular water (H2Om), and low (<0.8 wt.%) hydroxyl (OH) component, interpreted as evidence for secondary hydration by meteoric water. BRIC glasses contain the most depleted hydrogen isotopes yet measured in terrestrial rocks, down to δD = −325 ‰. In situ 40Ar/39Ar geochronology of hydrated glasses with ultra-depleted δD values yield ages from 105 Ma to 72 Ma with a peak at c. 91.4 Ma. Combined, these data suggest hydration of BRIC glasses by polar glacial ice and melt water during the Late Cretaceous, contradicting paleoclimate reconstructions of this period that suggest Antarctica was ice-free and part of a global hot greenhouse.

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climate and geology

Successive climate crises in the deep past drove the early evolution and radiation of reptiles

by T. Simoes et al., Aug 19, 2022 in ScienceAdvance

Abstract

Climate change–induced mass extinctions provide unique opportunities to explore the impacts of global environmental disturbances on organismal evolution. However, their influence on terrestrial ecosystems remains poorly understood. Here, we provide a new time tree for the early evolution of reptiles and their closest relatives to reconstruct how the Permian-Triassic climatic crises shaped their long-term evolutionary trajectory. By combining rates of phenotypic evolution, mode of selection, body size, and global temperature data, we reveal an intimate association between reptile evolutionary dynamics and climate change in the deep past. We show that the origin and phenotypic radiation of reptiles was not solely driven by ecological opportunity following the end-Permian extinction as previously thought but also the result of multiple adaptive responses to climatic shifts spanning 57 million years.
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climate and geology

Iceland eruption may be the start of decades of volcanic activity

by G. Andrews, Aug 4, 2022 in NationalGeographic

Less than a year has passed since lava stopped sputtering from Iceland’s Reykjanes Peninsula following the first major volcanic outburst from this region in almost 800 years. But now the island is once again bleeding molten rock. The start of a new eruption so soon after unrest in 2021 seems to underscore that this once quiescent peninsula has awoken from its long slumber.

“This could herald the start of decades of occasional eruptions,” says Dave McGarvie, a volcanologist at Lancaster University.

The new eruption, which started at 1:18 p.m. local time on August 3, sent scarlet ribbons streaming from the base of a small mountain into the uninhabited Meradalir Valley. Located far from populations, the volcanic burbles likely pose little danger to the public, at least in the near term. And this relative safety allows scientists and tourists alike to marvel at the geologic majesty and get excited for a possible onslaught of new scientific knowledge.

After all, each volcanic eruption here provides a “window into the abyss,” McGarvie says. The 2021 event yielded revelations about the personality of the peninsula’s exuberant eruptions—from their physical behaviors to their quirky chemistries. This new eruption promises even more insights as the nascent volcano forges the world’s youngest land.

It’s still unclear how prolific or lengthy the eruption will be; this information will only come to light with more time and continued monitoring. But this week’s show of fireworks strongly hints the peninsula will become one of the most volcanically active parts of the planet for several generations.

“I am genuinely excited,” McGarvie says.

A volcanic double-bill

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climate and geology

Tonga Eruption Blasted Unprecedented Amount of Water Into Stratosphere

by C. Rotter, Aug 3, 2022 in WUWT

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This looping video shows an umbrella cloud generated by the underwater eruption of the Hunga Tonga-Hunga Ha’apai volcano on Jan. 15, 2022. The GOES-17 satellite captured the series of images that also show crescent-shaped shock waves and lightning strikes.
Credit: NASA Earth Observatory image by Joshua Stevens using GOES imagery courtesy of NOAA and NESDIS

The huge amount of water vapor hurled into the atmosphere, as detected by NASA’s Microwave Limb Sounder, could end up temporarily warming Earth’s surface.

When the Hunga Tonga-Hunga Ha’apai volcano erupted on Jan. 15, it sent a tsunami racing around the world and set off a sonic boom that circled the globe twice. The underwater eruption in the South Pacific Ocean also blasted an enormous plume of water vapor into Earth’s stratosphere – enough to fill more than 58,000 Olympic-size swimming pools. The sheer amount of water vapor could be enough to temporarily affect Earth’s global average temperature.

“We’ve never seen anything like it,” said Luis Millán, an atmospheric scientist at NASA’s Jet Propulsion Laboratory in Southern California. He led a new study examining the amount of water vapor that the Tonga volcano injected into the stratosphere, the layer of the atmosphere between about 8 and 33 miles (12 and 53 kilometers) above Earth’s surface.

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climate and geology

A Tropical Plant’s Warmth Threshold Affirms Mid-Holocene Temps Were ‘7.7°C Higher Than Today’

by K. Richard, July 25, 2022 in NoTricksZone

A warmth-demanding plant can provide us with solid evidence of a much warmer than today Mid-Holocene climate.

Growth of the tropical aquatic plant ceases when air temperatures fall below 10°C.

A new study says that from about 8000 to 5000 years ago it was warm enough in winter that could grow at the 40°N latitude in northern China. Today its warmth threshold growth limit is ~34°N.

Scientists can therefore deduce the Mid-Holocene winter temperatures needed to have been “7.7°C higher than today” at that time.

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climate and geology

Global-Scale Warming Events Of ‘Up To 15 °C Within A Few Decades’ Have Occurred Since The Jurassic

Boulila et al., 2022 in NoTricksZone

A new study (Boulila et al., 2022) suggests “abrupt and severe changes in Earth’s past climate” have been occurring at ~1,500-year periodicities since the iceless Jurassic period.

Warming events of degrees C per within decades or less were at one time thought to have occurred only at locations like Greenland and the North Atlantic during the last glacial period (70 to 12 thousand years ago).

But the evidence has been piling up from locations throughout the globe (e.g., on continents and tropical to high latitude oceans, lakes, and rivers) indicating these warming events have “a global interconnection between the two hemispheres.”

These “abrupt and severe” global warming events with ~1,500-year periodicities can even be traced back to the iceless Jurassic period when Antarctica was a rainforest and 38°C warmer than today. This suggests the driving force for these global warming periods were not dependent on ice sheet dynamics.

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Abstract

Earth’s past climate exhibits short-term (1500-year) pronounced fluctuations during the last glacial period, called Dansgaard–Oeschger (DO) glacial events, which have never been detected in pre-Quaternary times. The record of DO equivalent climate variability in Mesozoic strata can provide constraints on understanding these events. Here we highlight a prominent 1500-year cyclicity in a Jurassic (~ 155 Ma) ice-free sedimentary record from the Tethyan Basin. This Jurassic 1500-year cyclicity is encoded in high-resolution magnetic susceptibility (MS) proxy data reflecting detrital variations, and expressed as marl-limestone couplets. Additionally, MS data detect the modulation of these DO-scale couplets by supercouplet sets, reflecting the precession and its harmonics. We suggest that this Jurassic DO-like cyclicity may originate from paleo-monsoon-like system, analogous to the record of DO events in the Pleistocene East Asian monsoon archives. Paleogeographic reconstructions and atmosphere–ocean simulations further support the potential existence of strong, ancient monsoon circulations in the Tethyan Basin during the Jurassic.

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Australia, climate and geology

2021-2022 Tonga Volcanic Eruption and Record Rainfall in Eastern Australia and New Zealand

by A. Wong & W. Yims, Jul 4, 2022 in The SaltbushClub

Summary

During late 2021, the Hunga Tonga-Hunga Ha’apai submarine volcano erupted creating a new island which erupted sub-aerially on 15th January, 2022 sending a plume 58 km above sea level penetrating the mesosphere. The study of observation records including satellite data has revealed warming of the ocean-surface layer followed by atmospheric cooling caused by the release of geothermal heat and volcanic materials entering the atmosphere respectively. Environmental factors influencing weather include the development of a relatively ‘short’ life-span South Pacific Blob; the transfer of large quantities of water vapour from the ocean into the atmosphere; the low-pressure condition on the ocean surface; the formation of clouds; the reduction of solar radiation caused by volcanic materials in the atmosphere; the strengthening of trade winds; the meandering of jet streams; the development of atmospheric rivers, the additional cooling effect of torrential rainfall, and, the switch to La Niña conditions. The record rainfall in eastern Australia and New Zealand and Tropical Cyclone Dovi occurring in February 2022 were both outcomes of atmospheric cooling following the sub-aerial eruption.

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