Robustness of CMIP6 Historical Global Mean Temperature Simulations: Trends, Long Term Persistence, Autocorrelation, and Distributional Shape
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F20%3A82292" target="_blank" >RIV/60460709:41330/20:82292 - isvavai.cz</a>
Výsledek na webu
<a href="https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020EF001667" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2020EF001667</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1029/2020EF001667" target="_blank" >10.1029/2020EF001667</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Robustness of CMIP6 Historical Global Mean Temperature Simulations: Trends, Long Term Persistence, Autocorrelation, and Distributional Shape
Popis výsledku v původním jazyce
Multi model climate experiments carried out as part of different phases of the Coupled Model Intercomparison Project (CMIP) are crucial to evaluate past and future climate change. The reliability of models simulations is often gauged by their ability to reproduce the historical climate across many time scales. This study compares the global mean surface air temperature from 29 CMIP6 models with observations from three datasets. We examine (1) warming and cooling rates in five subperiods from 1880 to 2014, (2) autocorrelation and long term persistence, (3) models performance based on probabilistic and entropy metrics, and (4) the distributional shape of temperature. All models simulate the observed long term warming trend from 1880 to 2014. The late twentieth century warming (1975 2014) and the hiatus (1942 1975) are replicated by most models. The post 1998 warming is overestimated in 90% of the simulations. Only six out of 29 models reproduce the observed long term persistence. All models show differ
Název v anglickém jazyce
Robustness of CMIP6 Historical Global Mean Temperature Simulations: Trends, Long Term Persistence, Autocorrelation, and Distributional Shape
Popis výsledku anglicky
Multi model climate experiments carried out as part of different phases of the Coupled Model Intercomparison Project (CMIP) are crucial to evaluate past and future climate change. The reliability of models simulations is often gauged by their ability to reproduce the historical climate across many time scales. This study compares the global mean surface air temperature from 29 CMIP6 models with observations from three datasets. We examine (1) warming and cooling rates in five subperiods from 1880 to 2014, (2) autocorrelation and long term persistence, (3) models performance based on probabilistic and entropy metrics, and (4) the distributional shape of temperature. All models simulate the observed long term warming trend from 1880 to 2014. The late twentieth century warming (1975 2014) and the hiatus (1942 1975) are replicated by most models. The post 1998 warming is overestimated in 90% of the simulations. Only six out of 29 models reproduce the observed long term persistence. All models show differ
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10510 - Climatic research
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach
Ostatní
Rok uplatnění
2020
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Earth Futures
ISSN
2328-4277
e-ISSN
2328-4277
Svazek periodika
8
Číslo periodika v rámci svazku
10
Stát vydavatele periodika
US - Spojené státy americké
Počet stran výsledku
14
Strana od-do
1-14
Kód UT WoS článku
000587316800017
EID výsledku v databázi Scopus
2-s2.0-85093916232