Links between Temperature Biases and Flow Anomalies in an Ensemble of CNRM-CM5.1 Global Climate Model Historical Simulations

The aim of this study was to evaluate temperature and sea-level pressure (SLP) fields and to analyse a related anomalous flow over midlatitudes simulated by the CNRM-CM5.1 global climate model (GCM). Simulated flow over midlatitudes of the Northern Hemisphere was assessed through flow indices, class...

Full description

Saved in:
Bibliographic Details
Main Authors: O. Lhotka, A. Farda
Format: Article
Language:English
Published: Wiley 2018-01-01
Series:Advances in Meteorology
Online Access:http://dx.doi.org/10.1155/2018/4984827
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1832563139377364992
author O. Lhotka
A. Farda
author_facet O. Lhotka
A. Farda
author_sort O. Lhotka
collection DOAJ
description The aim of this study was to evaluate temperature and sea-level pressure (SLP) fields and to analyse a related anomalous flow over midlatitudes simulated by the CNRM-CM5.1 global climate model (GCM). Simulated flow over midlatitudes of the Northern Hemisphere was assessed through flow indices, classified into 11 circulation types. Reference data were taken from the NOAA-CIRES 20th Century Reanalysis, version 2c. CNRM-CM5.1 exhibited analogous temperature biases to those reported for the mean of the CMIP5 GCMs’ ensemble. The most prominent features were an erroneous temperature dipole pattern in the Atlantic Ocean and a warm bias over regions of deep water upwelling (locally exceeding 5°C). The latter feature was associated with negative SLP biases in those regions. Too low pressure was found over midlatitudes of the Northern Hemisphere, and CNRM-CM5.1 simulated too frequent zonal flow in these latitudes. The usage of three ensemble members with different initial conditions did not improve model’s outputs because the bias is found to be considerably larger compared to the ensemble members’ spread. The study showed that temperature and SLP biases are connected in certain regions, suggesting that improvement of GCMs and development of bias correction methods should be carried out with a complex insight.
format Article
id doaj-art-31f57ec12d214e9eb6eb8e19b5159972
institution Kabale University
issn 1687-9309
1687-9317
language English
publishDate 2018-01-01
publisher Wiley
record_format Article
series Advances in Meteorology
spelling doaj-art-31f57ec12d214e9eb6eb8e19b51599722025-02-03T01:20:53ZengWileyAdvances in Meteorology1687-93091687-93172018-01-01201810.1155/2018/49848274984827Links between Temperature Biases and Flow Anomalies in an Ensemble of CNRM-CM5.1 Global Climate Model Historical SimulationsO. Lhotka0A. Farda1Global Change Research Institute, Czech Academy of Sciences, Brno, Czech RepublicGlobal Change Research Institute, Czech Academy of Sciences, Brno, Czech RepublicThe aim of this study was to evaluate temperature and sea-level pressure (SLP) fields and to analyse a related anomalous flow over midlatitudes simulated by the CNRM-CM5.1 global climate model (GCM). Simulated flow over midlatitudes of the Northern Hemisphere was assessed through flow indices, classified into 11 circulation types. Reference data were taken from the NOAA-CIRES 20th Century Reanalysis, version 2c. CNRM-CM5.1 exhibited analogous temperature biases to those reported for the mean of the CMIP5 GCMs’ ensemble. The most prominent features were an erroneous temperature dipole pattern in the Atlantic Ocean and a warm bias over regions of deep water upwelling (locally exceeding 5°C). The latter feature was associated with negative SLP biases in those regions. Too low pressure was found over midlatitudes of the Northern Hemisphere, and CNRM-CM5.1 simulated too frequent zonal flow in these latitudes. The usage of three ensemble members with different initial conditions did not improve model’s outputs because the bias is found to be considerably larger compared to the ensemble members’ spread. The study showed that temperature and SLP biases are connected in certain regions, suggesting that improvement of GCMs and development of bias correction methods should be carried out with a complex insight.http://dx.doi.org/10.1155/2018/4984827
spellingShingle O. Lhotka
A. Farda
Links between Temperature Biases and Flow Anomalies in an Ensemble of CNRM-CM5.1 Global Climate Model Historical Simulations
Advances in Meteorology
title Links between Temperature Biases and Flow Anomalies in an Ensemble of CNRM-CM5.1 Global Climate Model Historical Simulations
title_full Links between Temperature Biases and Flow Anomalies in an Ensemble of CNRM-CM5.1 Global Climate Model Historical Simulations
title_fullStr Links between Temperature Biases and Flow Anomalies in an Ensemble of CNRM-CM5.1 Global Climate Model Historical Simulations
title_full_unstemmed Links between Temperature Biases and Flow Anomalies in an Ensemble of CNRM-CM5.1 Global Climate Model Historical Simulations
title_short Links between Temperature Biases and Flow Anomalies in an Ensemble of CNRM-CM5.1 Global Climate Model Historical Simulations
title_sort links between temperature biases and flow anomalies in an ensemble of cnrm cm5 1 global climate model historical simulations
url http://dx.doi.org/10.1155/2018/4984827
work_keys_str_mv AT olhotka linksbetweentemperaturebiasesandflowanomaliesinanensembleofcnrmcm51globalclimatemodelhistoricalsimulations
AT afarda linksbetweentemperaturebiasesandflowanomaliesinanensembleofcnrmcm51globalclimatemodelhistoricalsimulations