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The Canadian Earth System Model version 5 (CanESM5.0.3)

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TLDR
The Canadian Earth System Model version 5 (CanESM5) as mentioned in this paper is a global model developed to simulate historical climate change and variability, to make centennial-scale projections of future climate, and to produce initialized seasonal and decadal predictions.
Abstract
. The Canadian Earth System Model version 5 (CanESM5) is a global model developed to simulate historical climate change and variability, to make centennial-scale projections of future climate, and to produce initialized seasonal and decadal predictions. This paper describes the model components and their coupling, as well as various aspects of model development, including tuning, optimization, and a reproducibility strategy. We also document the stability of the model using a long control simulation, quantify the model's ability to reproduce large-scale features of the historical climate, and evaluate the response of the model to external forcing. CanESM5 is comprised of three-dimensional atmosphere (T63 spectral resolution equivalent roughly to 2.8 ∘ ) and ocean (nominally 1 ∘ ) general circulation models, a sea-ice model, a land surface scheme, and explicit land and ocean carbon cycle models. The model features relatively coarse resolution and high throughput, which facilitates the production of large ensembles. CanESM5 has a notably higher equilibrium climate sensitivity (5.6 K) than its predecessor, CanESM2 (3.7 K), which we briefly discuss, along with simulated changes over the historical period. CanESM5 simulations contribute to the Coupled Model Intercomparison Project phase 6 (CMIP6) and will be employed for climate science and service applications in Canada.

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The Arctic has warmed nearly four times faster than the globe since 1979

TL;DR: This paper showed that during the last 43 years the Arctic has been warming nearly four times faster than the globe, which is a higher ratio than generally reported in literature, and compared the observed Arctic amplification ratio with the ratio simulated by state-of-the-art climate models, and found that the observed fourfold warming ratio over 1979-2021 is an extremely rare occasion in the climate model simulations.
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Projections of Precipitation and Temperature over the South Asian Countries in CMIP6

TL;DR: In this article, the authors analyzed the projected changes in temperature and precipitation over six South Asian countries during the twenty-first century, and showed that the CMIP6 models display higher sensitivity to greenhouse gas emissions over South Asia compared with the CMIA5 models.
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Carbon-concentration and carbon-climate feedbacks in CMIP6 models and their comparison to CMIP5 models

TL;DR: In this article, results from the fully and biogeochemically coupled simulations in which CO2 increases at a rate of 1% 1/1/yr −1 /1pct CO2 from its preindustrial value are analyzed to quantify the magnitude of carbon-concentration and carbon-climate feedback parameters which measure the response of ocean and terrestrial carbon pools to changes in atmospheric CO2 concentration and the resulting change in global climate, respectively.
References
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Journal ArticleDOI

Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century

TL;DR: HadISST1 as mentioned in this paper replaces the global sea ice and sea surface temperature (GISST) data sets and is a unique combination of monthly globally complete fields of SST and sea ice concentration on a 1° latitude-longitude grid from 1871.
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Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization

TL;DR: In this article, the authors present the background and rationale for the new structure of CMIP, provides a detailed description of the DECK and CMIP6 historical simulations, and includes a brief introduction to the 21-CMIP6-Endorsed MIPs.
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Isopycnal mixing in ocean circulation models

TL;DR: In this paper, a subgrid-scale form for mesoscale eddy mixing on isopycnal surfaces is proposed for use in non-eddy-resolving ocean circulation models.
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Fully multidimensional flux-corrected transport algorithms for fluids

TL;DR: In this paper, the critical flux limiting stage is implemented in multidimensions without resort to time splitting, which allows the use of flux-corrected transport (FCT) techniques in multi-dimensional fluid problems for which time splitting would produce unacceptable numerical results.
Journal ArticleDOI

Development and validation of a global database of lakes, reservoirs and wetlands

TL;DR: The Global Lakes and Wetlands Database (GLWD) as mentioned in this paper was created by combining the best available sources for lakes and wetlands on a global scale and the application of Geographic Information System (GIS) functionality enabled the generation of a database which focuses in three coordinated levels on (1) large lakes and reservoirs, (2) smaller water bodies, and (3) wetlands.
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