The Nature
Climate Change study estimates the Clean Power Plan accounts for about half of emissions cuts from the U.S.'s current and proposed policies.
Not exact matches
«Human - induced
climate change likely increased Harvey's total rainfall around Houston by at least 19 percent, with a best
estimate of 37 percent,» Michael Wehner, a co-author on an attribution
study recently published in Geophysical Research Letters, said at the American Geophysical Union conference in December.
A
study by Laura Carbognin at the Institute of Marine Sciences in Venice and colleagues provides the best
estimate yet of how the city will cope with the effects of
climate change.
When scientists use
climate models for attribution
studies, they first run simulations with
estimates of only «natural»
climate influences over the past 100 years, such as
changes in solar output and major volcanic eruptions.
«Our
study illustrates that the complexity of
climate change, adaptation, and flood damage can be disentangled by surprisingly simple mathematical functions to provide
estimates of the average annual costs of sea - level rise over a longer time period.»
A new
study attempts to
estimate the effects of
climate change on global agriculture — and outline ways to mitigate its most dire consequences
Until now, most
estimates of how many species are threatened by
climate change have been based on theoretical
studies that look at the climatic and environmental conditions that species need to survive, and overlay this with
estimates of how much suitable habitat will remain as the world warms.
Density
estimates provide significantly more information about species» response to
climate change than only
studying their ranges, which has been standard practice in these kinds of
studies until now.
While his new
study makes no use of the huge computer models commonly used by scientists to
estimate the magnitude of future
climate change, Lovejoy's findings effectively complement those of the International Panel on Climate Change (IPCC), h
climate change, Lovejoy's findings effectively complement those of the International Panel on Climate Change (IPCC), he
change, Lovejoy's findings effectively complement those of the International Panel on
Climate Change (IPCC), h
Climate Change (IPCC), he
Change (IPCC), he says.
A new
study from
climate scientists Robert DeConto at the University of Massachusetts Amherst and David Pollard at Pennsylvania State University suggests that the most recent estimates by the Intergovernmental Panel on Climate Change for future sea - level rise over the next 100 years could be too low by almost a factor
climate scientists Robert DeConto at the University of Massachusetts Amherst and David Pollard at Pennsylvania State University suggests that the most recent
estimates by the Intergovernmental Panel on
Climate Change for future sea - level rise over the next 100 years could be too low by almost a factor
Climate Change for future sea - level rise over the next 100 years could be too low by almost a factor of two.
The
study applied «medium to high» future emissions
estimates of heat - trapping gases, as assumed by the California state government, to models designed to assess what effect
climate change would have on national parks like Yosemite, Death Valley, Redwood, Joshua Tree and Sequoia.
Also, the new mortality
estimates, while dramatically higher than the approximately 150,000 annual deaths attributed to
climate change stress in WHO's last assessment in 2004, are not directly comparable to earlier
studies, which relied on different models and different underlying scenarios.
And for another, the previous
studies estimate that Earth's
climate will rapidly respond to the
changes.
That made the
study's approach unique in this branch of
climate change literature, which typically relies on weather
estimates over broad geographical areas.
The complex geology and high rates of biodiversity in the region — currently home to an
estimated 7,452 plant and animal species — make it a potential «natural stronghold» in the fight against
climate change, according to a new, multimillion - dollar
study by the Nature Conservancy.
A Nature
Climate Change study last year
estimated that emissions per mile from light - duty vehicles could fall by as much as 94 percent by 2030 in a «best - case scenario» of electric driverless taxis (ClimateWire, July 7, 2015).
«The
study provides more realistic modeling
estimates of how much vegetation
change will occur over the 21st century and will allow better predictions of future
climate change,» she said.
By
studying the relationship between CO2 levels and
climate change during a warmer period in Earth's history, the scientists have been able to
estimate how the
climate will respond to increasing levels of carbon dioxide, a parameter known as «
climate sensitivity».
Previous
studies have
estimated the effect of
climate change and population growth on wildfire patterns and the risk of damage to buildings and homes in California.
That
study addressed a puzzle, namely that recent
studies using the observed
changes in Earth's surface temperature suggested
climate sensitivity is likely towards the lower end of the
estimated range.
According to one
study that looked at eight fuel aridity metrics in the Western U.S. and modeled
climate change's effects on them, human - caused
climate change accounted for about 55 percent of the observed increases in fuel aridity between 1979 and 2015 (Figure 6), and added an
estimated 4.2 million hectares of forest fire area between 1984 and 2015.7 Based on all eight metrics, the Western U.S. experienced an average of 9 additional days per year of high fire potential due to
climate change between 2000 and 2015, a 50 percent increase from the baseline of 17 days per year when looking back to 1979.
James A. Edmonds • Member, IPCC Steering Committee on «New Integrated Scenarios» (2006 - present) • Lead Author, Working Group III, «Framing Issues,» IPCC Fourth Assessment Report (2007) • Lead Author, Working Group III, «Global, Regional, and National Costs and Ancillary Benefits of Mitigation,» IPCC Third Assessment Report (2001) • Lead Author, Working Group III, «Decision - Making Frameworks,» IPCC Third Assessment Report (2001) • Lead Author, Working Group III, Summary for Policy Makers, IPCC Third Assessment Report (2001) • Lead Author, Working Group II, «Energy Supply Mitigation Options,» IPCC Second Assessment Report (1996) • Lead Author, Working Group II, «Mitigation: Cross-Sectoral and Other Issues,» IPCC Second Assessment Report (1996) • Lead Author, Working Group III, «
Estimating the Costs of Mitigating Greenhouse Gases,» IPCC Second Assessment Report (1996) • Lead Author, Working Group III, «A Review of Mitigation Cost
Studies,» IPCC Second Assessment Report (1996) • Lead Author, Working Group III, «Integrated Assessment of
Climate Change: An Overview and Comparison of Approaches and Results,» IPCC Second Assessment Report (1996) • Lead Author, IPCC Special Report,
Climate Change 1994: Radiative Forcing of
Climate Change and An Evaluation of the IPCC IS92 Emission Scenarios (1994) • Lead Author, IPCC Special Report,
Climate Change 1992: The Supplementary Report to the IPCC Scientific Assessment (1992) • Major contributor, IPCC First Assessment Report, Working Group III, Response Strategies Working Group (1991).
It is important to regard the LGM
studies as just one set of points in the cloud yielded by other
climate sensitivity
estimates, but the LGM has been a frequent target because it was a period for which there is a lot of data from varied sources,
climate was significantly different from today, and we have considerable information about the important drivers — like CO2, CH4, ice sheet extent, vegetation
changes etc..
Therefore it is necessary to
study the magnitude of the methane emissions and
estimate their influence on
climate change.
Based on regional
studies, the Intergovernmental Panel on
Climate Change (IPCC) estimated that 20 — 30 % of the world's species are likely to be at increasingly high risk of extinction from climate change impacts within this century if global mean temperatures exceed 2 — 3 °C above pre-industrial levels [6], while Thomas et al. [5] predicted that 15 — 37 % of species could be «committed to extinction» due to climate change b
Climate Change (IPCC) estimated that 20 — 30 % of the world's species are likely to be at increasingly high risk of extinction from climate change impacts within this century if global mean temperatures exceed 2 — 3 °C above pre-industrial levels [6], while Thomas et al. [5] predicted that 15 — 37 % of species could be «committed to extinction» due to climate change by
Change (IPCC)
estimated that 20 — 30 % of the world's species are likely to be at increasingly high risk of extinction from
climate change impacts within this century if global mean temperatures exceed 2 — 3 °C above pre-industrial levels [6], while Thomas et al. [5] predicted that 15 — 37 % of species could be «committed to extinction» due to climate change b
climate change impacts within this century if global mean temperatures exceed 2 — 3 °C above pre-industrial levels [6], while Thomas et al. [5] predicted that 15 — 37 % of species could be «committed to extinction» due to climate change by
change impacts within this century if global mean temperatures exceed 2 — 3 °C above pre-industrial levels [6], while Thomas et al. [5] predicted that 15 — 37 % of species could be «committed to extinction» due to
climate change b
climate change by
change by 2050.
Oct. 3, 2017 - A recent
study by Lawrence Livermore National Laboratory (LLNL) scientists and collaborators is the first to use an ensemble of global chemistry
climate models to
estimate death rates from air pollution caused by the impact of
climate change on pollutant concentrations.
For this
study, the researchers wanted to
estimate how likely the disease is to become established in Europe as its
climate changes up to the end of the century.
This 2006
study found that the effect of amplifying feedbacks in the
climate system — where global warming boosts atmospheric CO2 levels — «will promote warming by an extra 15 percent to 78 percent on a century - scale» compared to typical estimates by the U.N.'s Intergovernmental Panel on Climate
climate system — where global warming boosts atmospheric CO2 levels — «will promote warming by an extra 15 percent to 78 percent on a century - scale» compared to typical
estimates by the U.N.'s Intergovernmental Panel on
Climate Climate Change.
Studies estimate that over 25 % of the population suffers from allergic disorders and
climate change theories suggest the problem is growing.
Now a new
study by V. Ramanathan of the University of California, San Diego, published online this week in Nature Geoscience, finds that soot may be more than twice as potent a warming influence as the Intergovernmental Panel on
Climate Change estimated last year.
Thanks Pete and Gavin for your response in # 116 that the
estimates for future temperature
change being discussed in the
climate sensitivity
studies (discussed in this thread) do not generally take into account the effect of increased temperature on initiating further natural carbon release.
That
study addressed a puzzle, namely that recent
studies using the observed
changes in Earth's surface temperature suggested
climate sensitivity is likely towards the lower end of the
estimated range.
The IPCC range, on the other hand, encompasses the overall uncertainty across a very large number of
studies, using different methods all with their own potential biases and problems (e.g., resulting from biases in proxy data used as constraints on past temperature
changes, etc.) There is a number of single
studies on
climate sensitivity that have statistical uncertainties as small as Cox et al., yet different best
estimates — some higher than the classic 3 °C, some lower.
For projections of maximum expected
climate change, we
estimate species - level extinction across species included in the
study to be 21â $ «32 % (range of the three methods) with universal dispersal, and 38â $ «52 % for no dispersal (Table 1).
But we are supposed to think that that's irrelevant because immediately after experimenters told them «97 % of scientists accept
climate change,» a group of
study subjects, while not
changing their own positions on whether
climate change is happening, increased by a very small amount their expressed
estimate of the percentage of scientists who believe in
climate change?
A new Nature
Climate Change study shows that the prevailing climate models produced estimates that overshot the temperature rise of the last 15 years by more than
Climate Change study shows that the prevailing
climate models produced estimates that overshot the temperature rise of the last 15 years by more than
climate models produced
estimates that overshot the temperature rise of the last 15 years by more than 300 %.
Despite satellite
estimates that more than doubled the population of known Emperor Penguins, the International Union for the Conservation of Nature (IUCN)
changed their ranking of Emperors from a species of Least Concern to a Near - Threatened species based on modeling
studies blaming the decline of DuDu's penguins on
climate change as presented in Jenouvrier and Caswell's
study.
The
study, published Monday in Nature
Climate Change, compiled data on 160 different countries to arrive at a global
estimate of the tourism industry's carbon footprint.
Climate Change:
Study estimates that nuclear energy leads to substantially fewer pollution - related deaths and greenhouse gas emissions compared with fossil - fuel sources
The
study, published in Nature
Climate Change,
estimates that global tourism — including transportation, accommodations, activities, food consumption, and all the energy and infrastructure required to accommodate visitors — produced about 4.5 billion tons of carbon dioxide equivalent in 2013.
In a Nature
Climate Change study, Hino and her coauthors
estimated around 1.3 million people had been relocated through managed retreat in response to natural hazards over the past three decades.
The new
study, published in the peer - reviewed journal Nature
Climate Change, used economic modelling to estimate the impact of unchecked climate
Climate Change, used economic modelling to estimate the impact of unchecked climate c
Change, used economic modelling to
estimate the impact of unchecked
climate climate changechange.
Many palaeoclimate
studies have quantified pre-anthropogenic
climate change to calculate
climate sensitivity (equilibrium temperature
change in response to radiative forcing
change), but a lack of consistent methodologies produces awide range of
estimates and hinders comparability of results.
The
study, published in the journal
Climate Dynamics last month, estimates that climate change will cause reduced rainfall alone to dessicate 12 percent of the Earth's land b
Climate Dynamics last month,
estimates that
climate change will cause reduced rainfall alone to dessicate 12 percent of the Earth's land b
climate change will cause reduced rainfall alone to dessicate 12 percent of the Earth's land by 2100.
Recent
studies showing the worldwide acceleration of glacier melting indicate that the Intergovernmental Panel on
Climate Change's
estimate for sea level rise this century — ranging from 0.1 meters to 0.9 meters — will need to be revised upwards.
Studies surveyed Millar, R. et al. (2017) Emission budgets and pathways consistent with limiting warming to 1.5 C, Nature Geophysics, doi: 10.1038 / ngeo3031 Matthews, H.D., et al. (2017)
Estimating Carbon Budgets for Ambitious
Climate Targets, Current Climate Change Reports, doi: 10.1007 / s40641 -017-0055-0 Goodwin, P., et al. (2018) Pathways to 1.5 C and 2C warming based on observational and geological constraints, Nature Geophysics, doi: 10.1038 / s41561 -017-0054-8 Schurer, A.P., et al. (2018) Interpretations of the Paris climate target, Nature Geophysics, doi: 10.1038 / s41561 -018-0086-8 Tokarska, K., and Gillett, N. (2018) Cumulative carbon emissions budgets consistent with 1.5 C global warming, Nature Climate Change, doi: 10.1038 / s41558 -018-0118-9 Millar, R., and Friedlingstein, P. (2018) The utility of the historical record for assessing the transient climate response to cumulative emissions, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0449 Lowe, J.A., and Bernie, D. (2018) The impact of Earth system feedbacks on carbon budgets and climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.20
Climate Targets, Current
Climate Change Reports, doi: 10.1007 / s40641 -017-0055-0 Goodwin, P., et al. (2018) Pathways to 1.5 C and 2C warming based on observational and geological constraints, Nature Geophysics, doi: 10.1038 / s41561 -017-0054-8 Schurer, A.P., et al. (2018) Interpretations of the Paris climate target, Nature Geophysics, doi: 10.1038 / s41561 -018-0086-8 Tokarska, K., and Gillett, N. (2018) Cumulative carbon emissions budgets consistent with 1.5 C global warming, Nature Climate Change, doi: 10.1038 / s41558 -018-0118-9 Millar, R., and Friedlingstein, P. (2018) The utility of the historical record for assessing the transient climate response to cumulative emissions, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0449 Lowe, J.A., and Bernie, D. (2018) The impact of Earth system feedbacks on carbon budgets and climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.20
Climate Change Reports, doi: 10.1007 / s40641 -017-0055-0 Goodwin, P., et al. (2018) Pathways to 1.5 C and 2C warming based on observational and geological constraints, Nature Geophysics, doi: 10.1038 / s41561 -017-0054-8 Schurer, A.P., et al. (2018) Interpretations of the Paris
climate target, Nature Geophysics, doi: 10.1038 / s41561 -018-0086-8 Tokarska, K., and Gillett, N. (2018) Cumulative carbon emissions budgets consistent with 1.5 C global warming, Nature Climate Change, doi: 10.1038 / s41558 -018-0118-9 Millar, R., and Friedlingstein, P. (2018) The utility of the historical record for assessing the transient climate response to cumulative emissions, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0449 Lowe, J.A., and Bernie, D. (2018) The impact of Earth system feedbacks on carbon budgets and climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.20
climate target, Nature Geophysics, doi: 10.1038 / s41561 -018-0086-8 Tokarska, K., and Gillett, N. (2018) Cumulative carbon emissions budgets consistent with 1.5 C global warming, Nature
Climate Change, doi: 10.1038 / s41558 -018-0118-9 Millar, R., and Friedlingstein, P. (2018) The utility of the historical record for assessing the transient climate response to cumulative emissions, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0449 Lowe, J.A., and Bernie, D. (2018) The impact of Earth system feedbacks on carbon budgets and climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.20
Climate Change, doi: 10.1038 / s41558 -018-0118-9 Millar, R., and Friedlingstein, P. (2018) The utility of the historical record for assessing the transient
climate response to cumulative emissions, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0449 Lowe, J.A., and Bernie, D. (2018) The impact of Earth system feedbacks on carbon budgets and climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.20
climate response to cumulative emissions, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0449 Lowe, J.A., and Bernie, D. (2018) The impact of Earth system feedbacks on carbon budgets and
climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.20
climate response, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2017.0263 Rogelj, J., et al. (2018) Scenarios towards limiting global mean temperature increase below 1.5 C, Nature
Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.20
Climate Change, doi: 10.1038 / s41558 -018-0091-3 Kriegler, E., et al. (2018) Pathways limiting warming to 1.5 °C: A tale of turning around in no time, Philosophical Transactions of the Royal Society A, doi: 10.1098 / rsta.2016.0457
But the downside of those opportunities is the risk that the current pace of
climate change could be sped up dramatically by the release of long - trapped methane gas in the region's permafrost — a risk to which a new
study has attached an eye - popping price tag of $ 60 trillion in the next several decades, on top of previous
estimates.
«Most experts that really
study CO2 amounts
estimate that we haven't seen that amount of CO2 in our atmosphere in about 3 million years,» said J. Marshall Shepherd,
climate change expert and professor at the University of Georgia.
The IPCC is
studying 250 (0.000027 %) of the 900 million years of
estimated temperature
change and ignoring major
climate change mechanisms and considerations, including our solar system's orbit in the Milky Way galaxy.
One more reason to discount the blame CO2 first dogma put forth by warmist
climate science»... «In our study [Beaulieua et al.], most streams were sources of N2O to the atmosphere and the highest emission rates were observed in streams draining urban basins... his estimate of stream and river N2O emissions is three times greater than estimated by the Intergovernmental Panel on Climate Change.
climate science»... «In our
study [Beaulieua et al.], most streams were sources of N2O to the atmosphere and the highest emission rates were observed in streams draining urban basins... his
estimate of stream and river N2O emissions is three times greater than
estimated by the Intergovernmental Panel on
Climate Change.
Climate Change.»