But the results of
studying earth climate in the past, indicates we currently in an unusual cool period, and that human evolution coincided with global cooling period.
Not exact matches
«This points to the unexplored risks of changing
climate on aviation,» said
study co-author Radley Horton, a climatologist at Columbia University's Lamont - Doherty
Earth Observatory.
Scientific
study of the Ice Age Floods is contributing to the understanding of cyclical
climate change and of very large and destructive contemporary floods on
Earth.
Assuming a rotation rate similar to today, the planet could have had a habitable
climate until at least 715 million years ago (SN Online: 8/26/16), even if Venus got 70 percent more sunlight than
Earth does now, physicist Michael Way of NASA's Goddard Institute for Space
Studies in New York City and colleagues reported in 2016 in Geophysical Research Letters.
Studies suggest that using olivine to transform
Earth's
climate would require more mineral than can fit on its surface, so carbonation is unlikely to be solely responsible for changes on Mars.
And Gulick's seismic
studies have taken him from pole to pole, mapping faults and glaciers, and bringing up cores to reveal
Earth's ancient
climate.
In order to reconstruct
climate history, it is necessary to
study natural
climate archives since, in terms of
Earth's history, humankind has only very recently begun measuring the planet.
It helps lay a foundation that scientists can apply to make predictions about what would allow life to alter exoplanets» atmospheres, and may inspire deeper
studies, here on
Earth, of how oceanic - atmospheric chemistry drives
climate instability and influences the rise and fall of life through the ages.
Paleoclimatology is the
study of
climate change taken on the scale of the entire history of the
earth.
Already sluggish, the sun may be slipping into several decades of hibernation that could exert a cooling effect on
Earth's
climate, several new
studies suggest.
The
study, which was published in the Proceedings of the National Academy of Sciences, presents a historical view of how
climate change and the resulting habitat loss can affect
Earth's biodiversity.
This is the first time anyone has examined regional
climate change in the central United States by directly comparing the influence of greenhouse gas emissions to agriculture, says Nathan Mueller, an
earth systems scientist at the University of California (UC), Irvine, who was not involved with this
study.
Antarctica's vulnerability to
climate change has also become increasingly clear, said Robin Bell of Columbia University's Lamont - Doherty
Earth Observatory, who
studies how ice sheets change.
«The Amazon rainforest is one of the tipping elements in the
Earth system,» says lead - author Delphine Clara Zemp who conducted the
study at the Potsdam Institute for
Climate Impact Research, Germany.
In a recent
study, Mathias Trachsel (Dept. of Biology, University of Bergen) and Atle Nesje (Dept. of
Earth Science, University of Bergen and Uni Research
Climate) used simple statistical models to assess and quantify the relative importance of summer temperature and winter precipitation for annual mass balances of eight Scandinavian glaciers.
«That is very exciting because a lot of interesting things happened with
Earth's
climate prior to 800,000 years ago that we currently can not
study in the ice core record.»
It's an accusation that has often been lobbed at Keith's main area of
study: geoengineering
Earth's
climate to counteract warming by, for instance, injecting particles into the sky to reflect sunlight.
«One of the key principles of geology is that the past is the key to the present: records of past
climate inform us of how the
Earth system functions,» says Michael Hren, assistant professor of chemistry and geosciences at the University of Connecticut and the
study's lead author.
Scientists like Zeebe also
study the PETM to better understand long - term changes in
Earth's future
climate.
«Prior analyses have found that
climate models underestimate the observed rate of tropical widening, leading to questions on possible model deficiencies, possible errors in the observations, and lack of confidence in future projections,» said Robert J. Allen, an assistant professor of climatology in UC Riverside's Department of
Earth Sciences, who led the
study.
They dramatically accelerated the natural breakdown of exposed rocks, according to a new
study, drawing so much planet - warming carbon dioxide (CO2) from the atmosphere that they sent
Earth's
climate spiraling into a major ice age.
One of these trips happened in 2014 while Lee and Rice colleagues also were
studying how a flare - up of Cretaceous - era arc volcanoes along the U.S. Pacific rim had impacted
Earth's
climate through enhanced volcanic production of carbon dioxide.
«
Studying the PETM helps us understand the mechanisms that aid recovery from global warming, thereby helping researchers reduce the uncertainties surrounding the
Earth's response to global
climate change,» Ridgwell said.
Scientists are interested in
studying ancient warming events to understand how the
Earth behaves when the
climate system is dramatically perturbed.
Dust that blew into the North Pacific Ocean could help explain why the
Earth's
climate cooled 2.7 million years ago, according to a new
study published in the journal Science Advances.
James Hansen, director of NASA's Goddard Institute for Space
Studies in New York City and a vociferous advocate for lowering global greenhouse gas emissions, was chosen for his work modeling
Earth's
climate, predicting global warming, and warning the world about the consequences.
Co-author of the
study Professor Ian Hall, from the School of
Earth and Ocean Sciences, said: «Our results highlight the challenge of basing our understanding of the
climate system on generally short observational records.
The earlier
study — which used pre-industrial temperature proxies to analyze historical
climate patterns — ruled out, with more than 99 % certainty, the possibility that global warming in the industrial era is just a natural fluctuation in
Earth's
climate.
Muller launched his own
climate study at the University of California, Berkeley — the Berkeley
Earth Surface Temperature project — in order to better
study temperature measurements, taking into account much of the concerns expressed by skeptics.
Paul Dirmeyer, a professor in the department of atmospheric, oceanic and
earth sciences at George Mason University who was not involved in the
study, notes: «Green et al. put forward an intriguing and exciting new idea, expanding our measures of land - atmospheric feedbacks from mainly a phenomenon of the water and energy cycles to include the biosphere, both as a response to
climate forcing and a forcing to
climate response.»
Studies of the sediment cores obtained during the expedition will focus on understanding how
Earth's tectonic plates move and how the global
climate system works.
A new Columbia Engineering
study, led by Pierre Gentine, associate professor of
earth and environmental engineering, analyzes global satellite observations and shows that vegetation alters
climate and weather patterns by as much as 30 percent.
«For the first time we can quantify how oceans responded to slow, natural
climate warming as the world emerged from the last ice age,» says Prof. Eric Galbraith from McGill University's Department of
Earth and Oceanic Sciences, who led the
study.
From a quarter to half of
Earth's vegetated lands has shown significant greening over the last 35 years largely due to rising levels of atmospheric carbon dioxide, according to a new
study published in the journal Nature
Climate Change on April 25.
Using global
climate models and NASA satellite observations of
Earth's energy budget from the last 15 years, the
study finds that a warming
Earth is able to restore its temperature equilibrium through complex and seemingly paradoxical changes in the atmosphere and the way radiative heat is transported.
An analysis of temperature data since 1500 all but rules out the possibility that global warming in the industrial era is just a natural fluctuation in the
earth's
climate, according to a new
study by McGill University physics professor Shaun Lovejoy.
The results of this
study have been published in Scientific Reports and could provide important information for the chemistry of the atmosphere, evaluation of
earth climate and in bioremediation.
Because scientists who've looked to glaciers to
study the history of
climate on
Earth have found that the Northern and Southern hemispheres have not been moving in sync.
The sediment cores used in this
study cover a period when the planet went through many
climate cycles driven by variations in
Earth's orbit, from extreme glacial periods such as the Last Glacial Maximum about 20,000 years ago, when massive ice sheets covered the northern parts of Europe and North America, to relatively warm interglacial periods with
climates more like today's.
And for another, the previous
studies estimate that
Earth's
climate will rapidly respond to the changes.
Of course, our
study looks back in time and the future will be a very different place in terms of ice sheets and CO2 but it remains to be seen whether or not
Earth's
climate becomes more or less stable as we move forward from here.»
A team of UK scientists have
studied how a circulation changes in the stratosphere (above 10 km) can influence both weather and
climate conditions on the surface of
Earth.
Professor Michael Benton from the University of Bristol, another co-author of the
study, said: «This work illustrates a case of the impact of
climate change on the evolution of animal biodiversity, and shows that for crocodilians, warming phases of our
earth's history constitute ideal opportunities to colonise new environments.»
The work, published yesterday in Science, finds evidence that
Earth's
climate is more sensitive to the amount of carbon dioxide in the atmosphere than some earlier
studies had suggested.
Analysis of three major bleaching events on
Earth's best -
studied reef highlights impact of
climate change
«This is one of several recent
studies that provide sobering evidence that
earth's
climate sensitivity may lie in the upper end of the current uncertainty range,» Mann said in an email.
Researchers use computer model outputs, such as this image from the Community
Earth System Model, to
study climate dynamics.
The team
studied storm development from the Pliocene era, roughly three million years ago, and chose that time period because it was the last time the
Earth had as much carbon dioxide as it does now, and the changes in
climate from it can play a major role in storm formation and intensity.
«Most of the previous research of the past
climate in this region is based on detailed
studies of specific sites,» said the lead author Jessica Oster, assistant professor of
earth and environmental sciences at Vanderbilt University.
Researchers from the United States and China are now
studying the core — nearly as long as the Empire State Building is tall — to assemble one of the longest - ever records of
Earth's
climate history.