The new
climate scenario simulations were carried out on DKRZ's supercomputer and occupied one quarter of its total computing capacity over a period of two years.
Not exact matches
In the new study, McGuire and his colleagues used
simulations to study changes in permafrost and carbon storage in the northern permafrost region from 2010 to 2299 using two
climate change
scenarios: One with low carbon dioxide emissions and one with high carbon dioxide emissions.
To reach these conclusions, the researchers used
simulations from five state - of - the - art
climate models to investigate how the characteristics of ARs may change under future
climate change
scenarios.
Then they plugged that into
simulations that took into account
climate models and two different carbon emissions scenarios identified by the Intergovernmental Panel on Climate
climate models and two different carbon emissions
scenarios identified by the Intergovernmental Panel on
Climate Climate Change.
However, comparing the results of the
climate simulations for the most recent interglacial with
scenario calculations for the future reveals substantial differences: thanks to the more intense solar radiation, back then the air temperatures at higher latitudes were also a few degrees higher than at present.
The Review is a super refined weekly web publication curated by subject matter experts from Yale who summarize important research articles from leading natural and social science journals with the hope that people can make more informed decisions using latest research results.The Review launched this week and covers a wide range of topics, like this brief about
climate change and biodiversity («Biodiversity Left Behind in Climate Change Scenarios»): They find that simply using the traditional classification of a species in climate change simulations can underestimate the true scale of biodiversit
climate change and biodiversity («Biodiversity Left Behind in
Climate Change Scenarios»): They find that simply using the traditional classification of a species in climate change simulations can underestimate the true scale of biodiversit
Climate Change
Scenarios»): They find that simply using the traditional classification of a species in
climate change simulations can underestimate the true scale of biodiversit
climate change
simulations can underestimate the true scale of biodiversity loss.
«The burned
simulations are based on three different
climate and wildfire
scenarios, and we also used three different erosion models,» said Sankey.
The researchers» forecasts are based on the AWI's BRIOS (Bremerhaven Regional Ice - Ocean
Simulations) model, a coupled ice - ocean model that the team forced with atmospheric data from the SRES - A1B
climate scenario, created at Britain's Met Office Hadley Centre in Exeter.
Simulations of different
climate scenarios suggest that by midcentury some of the prime wine regions
To investigate cloud —
climate feedbacks in iRAM, the authors ran several global warming
scenarios with boundary conditions appropriate for late twenty - first - century conditions (specifically, warming signals based on IPCC AR4 SRES A1B
simulations).
Effects of
climate change on US crop production:
simulation results using two different GCM
scenarios.
It is also equipped with phytotrons and greenhouses that enable the
simulation of various
climate scenarios, which helps researchers and scientists examine and predict the impacts of
climate change on plant growth.
A large ensemble of Earth system model
simulations, constrained by geological and historical observations of past
climate change, demonstrates our self ‐ adjusting mitigation approach for a range of
climate stabilization targets ranging from 1.5 to 4.5 °C, and generates AMP
scenarios up to year 2300 for surface warming, carbon emissions, atmospheric CO2, global mean sea level, and surface ocean acidification.
[Response: I wasn't part of the group that made the decisions on what
scenarios to use, but it is indeed true that running
simulations of
scenarios is a great drag on the
climate science community, so there is every reason to try to focus on the ones that will be most informative.
Zhang, X. D., and J. E. Walsh (2006), Toward a seasonally ice - covered Arctic Ocean:
Scenarios from the IPCC AR4 model
simulations, J
Climate, 19 (9), 1730 - 1747.
In the particular
simulation shown above, the frequency of the strongest (category 5) hurricanes roughly triples in the anthropogenic
climate change
scenario relative to the control.
Projections for the these variables are given for different model
simulations of
climate scenarios.
Using the business - as - usual
scenario for GHG radiative forcing (RCP8.5) and their novel estimate of Earth's warm - phase
climate sensitivity the authors find that the resulting warming during the 21st century overlaps with the upper range of the Coupled Model Intercomparison Project Phase 5 (CMIP5)
climate simulations.
Also referred to as synthetic
scenarios (IPCC, 1994), they are commonly applied to study the sensitivity of an exposure unit to a wide range of variations in
climate, often according to a qualitative interpretation of projections of future regional
climate from
climate model
simulations (guided sensitivity analysis, see IPCC - TGCIA, 1999).
Close agreement of observed temperature change with
simulations for the most realistic
climate forcing (
scenario B) is accidental, given the large unforced variability in both model and real world.
C - ROADS C - ROADS is an award - winning computer
simulation that helps people understand the long - term
climate impacts of policy
scenarios to reduce greenhouse gas emissions.
A recent meta - analysis published in the journal Nature
Climate Change, by Challinor et al. (2014) examines 1,722 crop model simulations, run using global climate model output under several emissions scenarios, to evaluate the potential effects of climate change and adaptation on crop
Climate Change, by Challinor et al. (2014) examines 1,722 crop model
simulations, run using global
climate model output under several emissions scenarios, to evaluate the potential effects of climate change and adaptation on crop
climate model output under several emissions
scenarios, to evaluate the potential effects of
climate change and adaptation on crop
climate change and adaptation on crop yield.
Interestingly, though
climate models have differing values for u, it remains almost time - invariant for a wide range of twenty - first century
climate transient warming
scenarios, while varying in
simulations of the twentieth century.
In general, diversity shifts towards the coast and northwards, and the degree depends on the dispersal assumptions, emission
scenarios, and the sensitivity of
climate simulations.
2: Our Changing
Climate, Key Message 5).2 Regional climate models (RCMs) using the same emissions scenario also project increased spring precipitation (9 % in 2041 - 2062 relative to 1979 - 2000) and decreased summer precipitation (by an average of about 8 % in 2041 - 2062 relative to 1979 - 2000) particularly in the southern portions of the Midwest.12 Increases in the frequency and intensity of extreme precipitation are projected across the entire region in both GCM and RCM simulations (Figure 18.6), and these increases are generally larger than the projected changes in average precipitatio
Climate, Key Message 5).2 Regional
climate models (RCMs) using the same emissions scenario also project increased spring precipitation (9 % in 2041 - 2062 relative to 1979 - 2000) and decreased summer precipitation (by an average of about 8 % in 2041 - 2062 relative to 1979 - 2000) particularly in the southern portions of the Midwest.12 Increases in the frequency and intensity of extreme precipitation are projected across the entire region in both GCM and RCM simulations (Figure 18.6), and these increases are generally larger than the projected changes in average precipitatio
climate models (RCMs) using the same emissions
scenario also project increased spring precipitation (9 % in 2041 - 2062 relative to 1979 - 2000) and decreased summer precipitation (by an average of about 8 % in 2041 - 2062 relative to 1979 - 2000) particularly in the southern portions of the Midwest.12 Increases in the frequency and intensity of extreme precipitation are projected across the entire region in both GCM and RCM
simulations (Figure 18.6), and these increases are generally larger than the projected changes in average precipitation.12, 2
Before using
scenarios or
climate simulation results, it is important to make sure you have formulated specific questions you want to address, and to investigate whether you can do that using the results of existing analyses, rather than performing your own.
As reported by other flora wide studies [20]--[21], our projections of range size change vary greatly based on future
climate simulations, emission levels, and dispersal
scenarios.
As in these studies, model projections depend greatly on future
climate simulations, emission levels, and dispersal
scenarios.
The planning tool SUDPLAN makes information available for the period 1961 - 2100, from a number of
climate scenarios scaled down across Europe, complete with hydrological
simulations and results from an air pollution model.
A range of future SLR is estimated from a set of
climate simulations governed by lower (B1), middle — upper (A2), and higher (A1fi) GHG emission
scenarios.
The models used the Intergovernmental Panel on
Climate Change's «A1B» mid-range projected emission
scenarios for ozone and aerosol precursors, independently calculated the resulting composition change, and then performed transient
simulations to 2050 examining the response to projected changes in the short - lived species and to changes in both long - lived and short - lived species together.
«This paper presents
simulations of
climate change with an ensemble of GCMs driven by the A1FI
scenario, and also assesses the implications of carbon - cycle feedbacks for the
climate - change projections.
The projections can use several different
climate scenarios to run the same future
simulation.
For their future
climate projections, Gillett et al. use five - member ensembles of
scenario simulations from 2006 — 2100 with RCP 2.6, RCP 4.5, and RCP 8.5 emissions
scenarios.
The first
simulation is an 1860 pre-industrial conditions 500 - year control run and the second is the SRESA1B, which is a «business as usual»
scenario with CO2 levels stabilizing at 720 ppmv at the close of the 21st century [Intergovernmental Panel on
Climate Change, 2001].
Research report: Extreme Weather Events and Crop Price Spikes in a Changing
Climate: Illustrative global
simulation scenarios
Climate projection — A projection of the response of the climate system to emission or concentration scenarios of greenhouse gases and aerosols, or radiative forcing scenarios, often based upon simulations by climate
Climate projection — A projection of the response of the
climate system to emission or concentration scenarios of greenhouse gases and aerosols, or radiative forcing scenarios, often based upon simulations by climate
climate system to emission or concentration
scenarios of greenhouse gases and aerosols, or radiative forcing
scenarios, often based upon
simulations by
climate climate models.
Climate scenarios from the Half a degree Additional warming, Projections, Prognosis and Impacts project (HAPPI) are largely consistent with transient
scenarios extracted from RCP4.5
simulations of the Coupled Model Intercomparison Project phase 5 (CMIP5).
Estimates from proxy data1 (for example, based on sediment records) are shown in red (1800 - 1890, pink band shows uncertainty), tide gauge data in blue for 1880 - 2009,2 and satellite observations are shown in green from 1993 to 2012.3 The future
scenarios range from 0.66 feet to 6.6 feet in 2100.4 These
scenarios are not based on
climate model
simulations, but rather reflect the range of possible
scenarios based on other kinds of scientific studies.
In my experience this is certainly the case if you talk about the
simulations as predictions rather than projections — the
climate models are not predicting what the weather will be on the 5th of May 2051 — they are providing projections of the
climate based on emission
scenarios and initial conditions.
Climate simulations using the IS92a and A2 and B2 SRES
scenarios (Meier et al., 2004; Räisänen et al., 2004) reinforce existing trends in storminess.
Research addressing this question relies on global
climate model
simulations based on a range of anticipated greenhouse gas (GHG) emissions
scenarios.
We make use of a 40 - member ensemble of
climate change
simulations under historical and RCP8.5 radiative forcing
scenarios for the period 1920 — 2100 conducted with the Community Earth System Model Version 1 (CESM1; Hurrell et al. 2013).
He used
simulations that depict a middle - of - the - road
climate change
scenario, meaning the range of warming by the end of this century is 1.0 °C to 2.6 °C above a 1986 to 2005 baseline.
Virtually all studies use a hydrological model driven by
scenarios based on
climate model
simulations, with a number of them using SRES - based
scenarios (e.g., Hayhoe et al., 2004; Zierl and Bugmann, 2005; Kay et al., 2006a).
Put another way, these billion - dollar, taxpayer - funded super-computer model
simulations have performed atrociously, and are entirely worthless at predicting future
climate scenarios.
Solution: Until
climate models are verified as being capable of somewhat accurate forecasts (predictions,
scenarios, etc.), policymakers and taxpayers should completely ignore any
climate simulation output that is a result of today's computer models.
Baseline (i.e., mean 1971 — 1999) global varies between 461 Pg C and 998 Pg C, and increases with ΔMLT for all vegetation models under all 110
climate and CO2 increase
scenarios (Fig. 1)(see Materials and Methods and SI Text for details of
simulations).
Given the existence of many other
climate models, one of the most important tests was the comparison of C - ROADS output to the output of disaggregated
simulations from the SRES database (e.g., MAGICC) given a range of emissions input
scenarios.
Drew Jones of
Climate Interactive presents
scenarios from the C - ROADS
simulation and explores how far these contributions get us, and what more is needed to keep warming to within 2 ° Celsius (3.6 °F) of temperature change above pre-industrial levels.