by James E. Kamis, August 7, 2018 in ClimateChangeDispatch
In what amounts to dissension from National Aeronautics and Space Administration (NASA) climate change policy, a series of just-released studies by working-level scientists prove that geological and not atmospheric forces are responsible for melting of Earth’s polar ice sheets.
NASA Greenland Study August 1, 2018
The results of this research study illustrated in Figure 2 confirm the very high geothermal bedrock heat-flow from Greenland’s massive subglacial Mantle Plume, which was originally documented in four previous research studies (see here, here, here, and here).
A geothermal heat-flow cause for the melting of Greenland’s ice sheet has been the focus of numerous Climate Change Dispatch articles (see here, here, here, and here).
by David Middleton, June 6 , 2019 in WUWT
What is a highstand?
A highstand is one phase of the sea level cycle (AAPG Wiki)
The highstand is the maximum sea level achieved during the cycle.
The Holocene Epoch
The Holocene Epoch was recently formally subdivided into three stages:
- Greenlandian Stage = Lower or Early-Holocene. 11.70 ka to 8.33 ka
- Northgrippian Stage = Middle or Mid-Holocene. 8.33 ka to 4.25 ka
- Meghalayan Stage = Upper or Late-Holocene. 4.25 ka to present
The abbreviation “ka” refers to thousands of years ago. Lower, Middle and Upper are generally used when referring to rock-time units. Early, Mid and Late are generally used when referring to time units (Haile, 1987). Prior to the formal subdivision, Lower/Early, Middle/Mid and Upper/Late were commonly used; however there was no formal nomenclature. The fake word, “Anthropocene” is not used by real geologists.
There is also an informal climatological subdivision of the Holocene:
- Preboreal 10 ka–9
- Boreal 9 ka–8 ka
- Atlantic 8 ka–5 ka
- Subboreal 5 ka–2.5 ka
- Subatlantic 2.5 ka–present
Why would there have been a Mid- to Late-Holocene highstand?
Figure 1. Holocene sea level curves from Moore & Curray, 1974.
by Università Ca’ Foscari Venezia, June 5, 2019 in WUWT
Click here for project video.
On 1st June 2019 the European Beyond EPICA Oldest Ice Core project started with the aim of drilling for and recovering ice from up to 1.5 Million years ago in Antarctica. The previous EPICA project recovered ice from 800,000 years ago. The new project aims to go beyond that. The new core will give us information on the greenhouse gases present during the Middle Pleistocene Transition (MPT), which occurred between 900,000 and 1.2 Million years ago. During this period the climatic periodicity transitioned from 41,000 to 100,000 years between ice ages. Why this change happened is the mystery scientists want to resolve.
To do this, experts from 10 European Countries and 16 different Research Institutions have joined forces under the guidance of Carlo Barbante and his management team at the CNR and Ca’ Foscari University of Venice in Italy, funded by the European Horizon 2020-research programme.
For further information visit https://www.beyondepica.eu/
by A. Jacobs & A. Préat, May 20, 2019 in SSRN.Elsevier
The focus of this study is based on a detailed analysis of the hyperthermal events of the
Paleocene / Eocene limit of 56 Ma and the lower Eocene (for the 54-52 Ma interval, Figure 1).
This example will show that the Earth has experienced many times much higher temperatures
than today, with warmer, sometimes more acidic oceans and an atmosphere much richer in CO2
(or CH4) than the current one. Are these past events precursors of the current situation?
Keywords: global warming, climate change, Paleocene, Eocene, hyperthermal events
by David Middleton, May 18, 2019 in WUWT
Gingerich, 2019 is a recent paper reiterating the PETM Chicken Little of the Sea meme. In the comments section of a recent post, it was cited as evidence of imminent catastrophe and followed up by a comment featuring this image from Clean Tecnica:
I just had to track this back to the Clean Tecnica article… Their scientific prowess is almost always laughable… And I was not disappointed.
by William J. Davis, September 2017, in ResearchGate
Assessing human impacts on climate and biodiversity requires an understanding of the relationship between the concentration of carbon dioxide (CO2) in the Earth’s atmosphere and global temperature (T). Here I explore this relationship empirically using comprehensive, recently-compiled databases of stable-isotope proxies from the Phanerozoic Eon (~540 to 0 years before the present) and through complementary modeling using the atmospheric absorption/transmittance code MODTRAN. Atmospheric CO2 concentration is correlated weakly but negatively with linearly-detrended T proxies over the last 425 million years.
by A. Préat & A. Jacobs, 17 avril 2019 in ScienceClimatEnergie
Le but de cet article est de montrer combien la climatologie (actuelle et celle du passé) est complexe et que’ la science est loin d’être dite’. Pour ce qui est de la climatologie actuelle de très nombreux articles existent, dont une partie sur SCE. Pour la climatologie du passé les exemples géologiques ne manquent pas (également quelques articles généraux sur SCE, ici). Le propos de cet article est basé sur une analyse détaillée des événements hyperthermiques de la limite Paléocène/Eocène il y a 56 Ma et de l’Eocène inférieur (pour l’intervalle 54-52 Ma, Figure 1). Cet exemple montrera que la Terre a connu à de nombreuses reprises des températures bien plus élevées que celles d’aujourd’hui, avec des océans plus chauds, parfois plus acides et une atmosphère beaucoup plus riche en CO2 (ou en CH4) que l’actuelle. Cela n’a jamais empêché la vie de se développer, et ‘ironie du sort’ c’est au cours d’un de ces événements hyperthermiques du Tertiaire (ou PETM, voir plus loin), qui fut l’un des plus chauds qu’ait connu la Terre, que les mammifères ont poursuivi une radiation évolutive (= diversification des espèces) sans précédent entamée après l’extinction des dinosaures à la limite Crétacé/Tertiaire [1, 2].
by P. Homewood, April 7, 2019 in NotaLotofPeopleKnowThat
It is thought that the Northern Hemisphere experienced only ephemeral glaciations from the Late Eocene to the Early Pliocene epochs (about 38 to 4 million years ago), and that the onset of extensive glaciations did not occur until about 3 million years ago. Several hypotheses have been proposed to explain this increase in Northern Hemisphere glaciation during the Late Pliocene. Here we use a fully coupled atmosphere-ocean general circulation model and an ice-sheet model to assess the impact of the proposed driving mechanisms for glaciation and the influence of orbital variations on the development of the Greenland ice sheet in particular. We find that Greenland glaciation is mainly controlled by a decrease in atmospheric carbon dioxide during the Late Pliocene. By contrast, our model results suggest that climatic shifts associated with the tectonically driven closure of the Panama seaway, with the termination of a permanent El Niño state or with tectonic uplift are not large enough to contribute significantly to the growth of the Greenland ice sheet; moreover, we find that none of these processes acted as a priming mechanism for glacial inception triggered by variations in the Earth’s orbit.
by Anthony Watts, March 19, 2019 in WUWT
It is little wonder that kids are scared when grown-ups paint such a horrific picture of global warming.
For starters, leading politicians and much of the media have prioritized climate change over other issues facing the planet. Last September, United Nations Secretary-General António Guterres described climate change as a “direct existential threat” that may become a “runaway” problem. Just last month, The New York Times ran a front-page commentary on the issue with the headline “Time to Panic.” And some prominent politicians, as well as many activists, have taken the latest report from the United Nations Intergovernmental Panel on Climate Change (IPCC) to suggest the world will come to an end in just 12 years.
by Anthony Watts, March 15, 2019 in WUWT
Over the last 540 million years, the Earth has weathered three major ice ages — periods during which global temperatures plummeted, producing extensive ice sheets and glaciers that have stretched beyond the polar caps.
Now scientists at MIT, the University of California at Santa Barbara, and the University of California at Berkeley have identified the likely trigger for these ice ages.
In a study published in Science, the team reports that each of the last three major ice ages were preceded by tropical “arc-continent collisions” — tectonic pileups that occurred near the Earth’s equator, in which oceanic plates rode up over continental plates, exposing tens of thousands of kilometers of oceanic rock to a tropical environment.
The scientists say that the heat and humidity of the tropics likely triggered a chemical reaction between the rocks and the atmosphere. Specifically, the rocks’ calcium and magnesium reacted with atmospheric carbon dioxide, pulling the gas out of the atmosphere and permanently sequestering it in the form of carbonates such as limestone.
Over time, the researchers say, this weathering process, occurring over millions of square kilometers, could pull enough carbon dioxide out of the atmosphere to cool temperatures globally and ultimately set off an ice age.
by James Kennett et al., March 13, 2019 in CO2Coalition
When UC Santa Barbara geology professor emeritus James Kennett and colleagues set out years ago to examine signs of a major cosmic impact that occurred toward the end of the Pleistocene epoch, little did they know just how far-reaching the projected climatic effect would be.
“It’s much more extreme than I ever thought when I started this work,” Kennett noted. “The more work that has been done, the more extreme it seems.”
He’s talking about the Younger Dryas Impact Hypothesis, which postulates that a fragmented comet slammed into the Earth close to 12,800 years ago, causing rapid climatic changes, megafaunal extinctions, sudden human population decrease and cultural shifts and widespread wildfires (biomass burning). The hypothesis suggests a possible triggering mechanism for the abrupt changes in climate at that time, in particular a rapid cooling in the Northern Hemisphere, called the Younger Dryas, amid a general global trend of natural warming and ice sheet melting evidenced by changes in the fossil and sediment record.
by J.E. Kamis, February 25, 2019 in ClimateChangeDispatch
Research study after research study has now proven beyond any doubt that the 350,000-square-mile subglacial Marie Byrd Mantle Plume and its associated geological features that are emitting massive amounts of ice melting heat and heated fluid onto the base of the Pine Island Glacier and Thwaites Glaciers.
Failure of the media to include in their numerous articles this telling scientific evidence which substantiates the significant and likely dominant role of this subglacial geologically induced heat flow in melting of West Antarctic glaciers is difficult to reconcile with proper scientific methodology.
A methodology which states that new and relevant data should be used to review old supposedly 100% settled theories.
Most of these research studies have been released one by one during the last three years which has led to minimizing their collective importance. Numerous previous Climate Change Dispatch articles written by this author beginning in 2014 have inexplicably been ignored by mainstream media outlets.
It’s time for the media to inform the public that by tying all this information together that a clear picture emerges concerning the significant impact of Antarctic subglacial geologically induced heat flow.
by Univ. of California – Berkeley, February 21, 2019 in ScienceDaily
Based on new data published today in the journal Science, it seems increasingly likely that an asteroid or comet impact 66 million years ago reignited massive volcanic eruptions in India, half a world away from the impact site in the Caribbean Sea.
But it leaves unclear to what degree the two catastrophes contributed to the near-simultaneous mass extinction that killed off the dinosaurs and many other forms of life.
The research sheds light on huge lava flows that have erupted periodically over Earth’s history, and how they have affected the atmosphere and altered the course of life on the planet.
by Don J. Easterbrook, 2011 in ScienceDirect
The Medieval Warm Period (MWP) was a time of warm climate from about 900 A.D. to 1300 A.D. when global temperatures were apparently somewhat warmer than at present. Its effects were evident in Europe where grain crops flourished, alpine tree lines rose, many new cities arose, and the population more than doubled. The Vikings took advantage of the climatic amelioration to colonize Greenland, and wine grapes were grown as far north as England where growing grapes is now not feasible and about 500 km north of present vineyards in France and Germany. Grapes are presently grown in Germany up to elevations of about 560 m, but from about 1100 A.D. to 1300 A.D., vineyards extended up to 780 m, implying temperatures warmer by about 1.0–1.4 °C (Oliver, 1973).
by Penn State, February 2, 2019 in ScienceDaily
Paleoclimatic records indicate that most of Greenland was ice-free within the last 1.1 million years even though temperatures then were not much warmer than conditions today. To explain this, the researchers point to there being more heat beneath the ice sheet in the past than today.
Data show that when the Iceland hot spot — the heat source that feeds volcanoes on Iceland — passed under north-central Greenland 80 to 35 million years ago, it left molten rock deep underground but did not break through the upper mantle and crust to form volcanoes as it had in the west and east. The Earth’s climate then was too warm for Greenland to have an ice sheet, but once it cooled the ice sheet formed, growing and shrinking successive with ice ages.