E. J. Stone
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View article: Paleoecological History of Maplecrest Fen, Catskill Mountains (<scp>NY</scp>, <scp>USA</scp>) From Deglaciation to the Industrial Age
Paleoecological History of Maplecrest Fen, Catskill Mountains (<span>NY</span>, <span>USA</span>) From Deglaciation to the Industrial Age Open
Aim To develop the palaeoecological and palaeoclimatic history of Maplecrest Fen, Greene County, NY. Location Catskill Mountains, New York. Time Period 13,500 calendar years to present (ybp, present = 1950). Taxon Angiosperms, gymnosperms …
View article: Simulation of the mid-Pliocene Warm Period using HadGEM3:experimental design and results from model&#8211;model andmodel&#8211;data comparison
Simulation of the mid-Pliocene Warm Period using HadGEM3:experimental design and results from model–model andmodel–data comparison Open
<p>Here we present the experimental design and results from a new mid-Pliocene simulation using the latest version of the UK&#8217;s physical climate model, HadGEM3-GC31-LL, conducted under the auspices of CMIP6/PMIP4/PlioMIP2. &…
View article: Organising a collaborative online hackathon for cutting‐edge climate research
Organising a collaborative online hackathon for cutting‐edge climate research Open
The 2021 Met Office Climate Data Challenge hackathon series (Met Office, 2021b) provided a valuable opportunity to learn best practice from the experience of running online hackathons uniquely characterised by the challenges faced by clima…
View article: The Bristol <scp>CMIP6</scp> Data Hackathon
The Bristol <span>CMIP6</span> Data Hackathon Open
The Bristol CMIP6 Data Hackathon formed part of the Met Office Climate Data Challenge Hackathon series during 2021, bringing together around 100 UK early career researchers from a wide range of environmental disciplines. The purpose was to…
View article: Quantum Markov chain Monte Carlo with digital dissipative dynamics on quantum computers
Quantum Markov chain Monte Carlo with digital dissipative dynamics on quantum computers Open
Modeling the dynamics of a quantum system connected to the environment is critical for advancing our understanding of complex quantum processes, as most quantum processes in nature are affected by an environment. Modeling a macroscopic env…
View article: Simulation of the mid-Pliocene Warm Period using HadGEM3: experimental design and results from model–model and model–data comparison
Simulation of the mid-Pliocene Warm Period using HadGEM3: experimental design and results from model–model and model–data comparison Open
Here we present the experimental design and results from a new mid-Pliocene simulation using the latest version of the UK's physical climate model, HadGEM3-GC31-LL, conducted under the auspices of CMIP6/PMIP4/PlioMIP2. Although two other p…
View article: Comment on cp-2021-40
Comment on cp-2021-40 Open
Abstract. Here we present the experimental design and results from a new mid-Pliocene simulation using the latest version of the UK's physical climate model, HadGEM3-GC31-LL, conducted under the auspices of CMIP6/PMIP4/PlioMIP2. Although t…
View article: Supplementary material to "Simulation of the mid-Pliocene Warm Period using HadGEM3: Experimental design and results from model-model and model-data comparison"
Supplementary material to "Simulation of the mid-Pliocene Warm Period using HadGEM3: Experimental design and results from model-model and model-data comparison" Open
Model descriptionHadGEM2-
View article: Simulation of the mid-Pliocene Warm Period using HadGEM3: Experimental design and results from model-model and model-data comparison
Simulation of the mid-Pliocene Warm Period using HadGEM3: Experimental design and results from model-model and model-data comparison Open
Here we present the experimental design and results from a new mid-Pliocene simulation using the latest version of the UK’s physical climate model, HadGEM3-GC31-LL, conducted under the auspices of CMIP6/PMIP4/PlioMIP2. Although two other p…
View article: Simulation of the mid-Pliocene Warm Period using HadGEM3-GC31-LL: Pliocene climate relative to the pre-industrial era, previous model versions, other climate models and proxy data
Simulation of the mid-Pliocene Warm Period using HadGEM3-GC31-LL: Pliocene climate relative to the pre-industrial era, previous model versions, other climate models and proxy data Open
<p>To better understand the processes contributing to future climate change, palaeoclimate model simulations are an important tool because they allow testing of the models&#8217; ability to simulate very different climates than t…
View article: The BRIDGE HadCM3 family of climate models: HadCM3@Bristol v1.0
The BRIDGE HadCM3 family of climate models: HadCM3@Bristol v1.0 Open
Understanding natural and anthropogenic climate change processes involves using computational models that represent the main components of the Earth system: the atmosphere, ocean, sea ice, and land surface. These models have become increas…
View article: Sensitivity of the Greenland Ice Sheet to Interglacial Climate Forcing: MIS 5e Versus MIS 11
Sensitivity of the Greenland Ice Sheet to Interglacial Climate Forcing: MIS 5e Versus MIS 11 Open
The Greenland Ice Sheet (GrIS) is thought to have contributed substantially to high global sea levels during the interglacials of Marine Isotope Stage (MIS) 5e and 11. Geological evidence suggests that the mass loss of the GrIS was greater…
View article: Recent advances on the dynamical representation and our understanding of the warmer‑than‑present last interglacial climate
Recent advances on the dynamical representation and our understanding of the warmer‑than‑present last interglacial climate Open
The Last Interglacial (LIG, ~129-116 thousand years Before Present, hereafter ka) represents an ideal case study to understand the climate mechanisms at play under a warmer-than-present climate. However a spatio-temporal representation of …
View article: The BRIDGE HadCM3 family of climate models:HadCM3@Bristol v1.0
The BRIDGE HadCM3 family of climate models:HadCM3@Bristol v1.0 Open
Understanding natural and anthropogenic climate change processes involves using computational models that represent the main components of the Earth system: the atmosphere, ocean, sea-ice and land surface. These models have become increasi…
View article: Model output of the Greenland Ice Sheet to interglacial climate forcing: MIS 5e versus MIS 11
Model output of the Greenland Ice Sheet to interglacial climate forcing: MIS 5e versus MIS 11 Open
The Greenland Ice Sheet (GrIS) is thought to have contributed substantially to high global sea levels during the interglacials of Marine Isotope Stage (MIS) 5e and 11. Geological evidence suggests that the mass loss of the GrIS was greater…
View article: How warm was Greenland during the last interglacial period?
How warm was Greenland during the last interglacial period? Open
The last interglacial period (LIG, ∼ 129–116 thousand years ago) provides the most recent case study of multimillennial polar warming above the preindustrial level and a response of the Greenland and Antarctic ice sheets to this warming, a…
View article: Impact of meltwater on high-latitude early Last Interglacial climate
Impact of meltwater on high-latitude early Last Interglacial climate Open
Recent data compilations of the early Last Interglacial period have indicated a bipolar temperature response at 130 ka, with colder-than-present temperatures in the North Atlantic and warmer-than-present temperatures in the Southern Ocean …
View article: How warm was Greenland during the last interglacial period?
How warm was Greenland during the last interglacial period? Open
The last interglacial period (LIG, ~ 129–116 thousand years ago) provides the most recent case study for multi-millennial polar warming above pre-industrial level and a respective response of the Greenland and Antarctic ice sheets to this …
View article: Impact of melt water on high latitude early Last Interglacial climate
Impact of melt water on high latitude early Last Interglacial climate Open
Recent data compilations of the early Last Interglacial period have indicated a bipolar temperature response at 130 ka, with colder-than-present temperatures in the North Atlantic and warmer-than-present temperatures in the Southern Ocean …