BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model

BCC-CSM2-HR is a high-resolution version of the Beijing Climate Center (BCC) Climate System Model (T266 in the atmosphere and <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow&...

Full description

Bibliographic Details
Published in:Geoscientific Model Development
Main Authors: Wu, Tongwen, Yu, Rucong, Lu, Yixiong, Jie, Weihua, Fang, Yongjie, Zhang, Jie, Zhang, Li, Xin, Xiaoge, Li, Laurent, Wang, Zaizhi, Liu, Yiming, Zhang, Fang, Wu, Fanghua, Chu, Min, Li, Jianglong, Li, Weiping, Zhang, Yanwu, Shi, Xueli, Zhou, Wenyan, Yao, Junchen, Liu, Xiangwen, Zhao, He, Yan, Jinghui, Wei, Min, Xue, Wei, Huang, Anning, Zhang, Yaocun, Zhang, Yu, Shu, Qi, Hu, Aixue
Format: Text
Language:English
Published: 2021
Subjects:
Online Access:https://doi.org/10.5194/gmd-14-2977-2021
https://gmd.copernicus.org/articles/14/2977/2021/
id ftcopernicus:oai:publications.copernicus.org:gmd89062
record_format openpolar
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description BCC-CSM2-HR is a high-resolution version of the Beijing Climate Center (BCC) Climate System Model (T266 in the atmosphere and <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">4</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="f7b7a5d5bfd5c45cef6c295312dc1896"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gmd-14-2977-2021-ie00001.svg" width="20pt" height="14pt" src="gmd-14-2977-2021-ie00001.png"/></svg:svg> ∘ latitude × <math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">4</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="730b8b169cb37255af42cf31763b7866"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gmd-14-2977-2021-ie00002.svg" width="20pt" height="14pt" src="gmd-14-2977-2021-ie00002.png"/></svg:svg> ∘ longitude in the ocean). Its development is on the basis of the medium-resolution version BCC-CSM2-MR (T106 in the atmosphere and 1 ∘ latitude × 1 ∘ longitude in the ocean) which is the baseline for BCC participation in the Coupled Model Intercomparison Project Phase 6 (CMIP6). This study documents the high-resolution model, highlights major improvements in the representation of atmospheric dynamical core and physical processes. BCC-CSM2-HR is evaluated for historical climate simulations from 1950 to 2014, performed under CMIP6-prescribed historical forcing, in comparison with its previous medium-resolution version BCC-CSM2-MR. Observed global warming trends of surface air temperature from 1950 to 2014 are well captured by both BCC-CSM2-MR and BCC-CSM2-HR. Present-day basic atmospheric mean states during the period from 1995 to 2014 are then evaluated at global scale, followed by an assessment on climate variabilities in the tropics including the tropical cyclones (TCs), the El Niño–Southern Oscillation (ENSO), the Madden–Julian Oscillation (MJO), and the quasi-biennial oscillation (QBO) in the stratosphere. It is shown that BCC-CSM2-HR represents the global energy balance well and can realistically reproduce the main patterns of atmospheric temperature and wind, precipitation, land surface air temperature, and sea surface temperature (SST). It also improves the spatial patterns of sea ice and associated seasonal variations in both hemispheres. The bias of the double intertropical convergence zone (ITCZ), obvious in BCC-CSM2-MR, almost disappears in BCC-CSM2-HR. TC activity in the tropics is increased with resolution enhanced. The cycle of ENSO, the eastward propagative feature and convection intensity of MJO, and the downward propagation of QBO in BCC-CSM2-HR are all in a better agreement with observations than their counterparts in BCC-CSM2-MR. Some imperfections are, however, noted in BCC-CSM2-HR, such as the excessive cloudiness in the eastern basin of the tropical Pacific with cold SST biases and the insufficient number of tropical cyclones in the North Atlantic.
format Text
author Wu, Tongwen
Yu, Rucong
Lu, Yixiong
Jie, Weihua
Fang, Yongjie
Zhang, Jie
Zhang, Li
Xin, Xiaoge
Li, Laurent
Wang, Zaizhi
Liu, Yiming
Zhang, Fang
Wu, Fanghua
Chu, Min
Li, Jianglong
Li, Weiping
Zhang, Yanwu
Shi, Xueli
Zhou, Wenyan
Yao, Junchen
Liu, Xiangwen
Zhao, He
Yan, Jinghui
Wei, Min
Xue, Wei
Huang, Anning
Zhang, Yaocun
Zhang, Yu
Shu, Qi
Hu, Aixue
spellingShingle Wu, Tongwen
Yu, Rucong
Lu, Yixiong
Jie, Weihua
Fang, Yongjie
Zhang, Jie
Zhang, Li
Xin, Xiaoge
Li, Laurent
Wang, Zaizhi
Liu, Yiming
Zhang, Fang
Wu, Fanghua
Chu, Min
Li, Jianglong
Li, Weiping
Zhang, Yanwu
Shi, Xueli
Zhou, Wenyan
Yao, Junchen
Liu, Xiangwen
Zhao, He
Yan, Jinghui
Wei, Min
Xue, Wei
Huang, Anning
Zhang, Yaocun
Zhang, Yu
Shu, Qi
Hu, Aixue
BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model
author_facet Wu, Tongwen
Yu, Rucong
Lu, Yixiong
Jie, Weihua
Fang, Yongjie
Zhang, Jie
Zhang, Li
Xin, Xiaoge
Li, Laurent
Wang, Zaizhi
Liu, Yiming
Zhang, Fang
Wu, Fanghua
Chu, Min
Li, Jianglong
Li, Weiping
Zhang, Yanwu
Shi, Xueli
Zhou, Wenyan
Yao, Junchen
Liu, Xiangwen
Zhao, He
Yan, Jinghui
Wei, Min
Xue, Wei
Huang, Anning
Zhang, Yaocun
Zhang, Yu
Shu, Qi
Hu, Aixue
author_sort Wu, Tongwen
title BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model
title_short BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model
title_full BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model
title_fullStr BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model
title_full_unstemmed BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model
title_sort bcc-csm2-hr: a high-resolution version of the beijing climate center climate system model
publishDate 2021
url https://doi.org/10.5194/gmd-14-2977-2021
https://gmd.copernicus.org/articles/14/2977/2021/
geographic Pacific
geographic_facet Pacific
genre North Atlantic
Sea ice
genre_facet North Atlantic
Sea ice
op_source eISSN: 1991-9603
op_relation doi:10.5194/gmd-14-2977-2021
https://gmd.copernicus.org/articles/14/2977/2021/
op_doi https://doi.org/10.5194/gmd-14-2977-2021
container_title Geoscientific Model Development
container_volume 14
container_issue 5
container_start_page 2977
op_container_end_page 3006
_version_ 1766137293747257344
spelling ftcopernicus:oai:publications.copernicus.org:gmd89062 2023-05-15T17:37:23+02:00 BCC-CSM2-HR: a high-resolution version of the Beijing Climate Center Climate System Model Wu, Tongwen Yu, Rucong Lu, Yixiong Jie, Weihua Fang, Yongjie Zhang, Jie Zhang, Li Xin, Xiaoge Li, Laurent Wang, Zaizhi Liu, Yiming Zhang, Fang Wu, Fanghua Chu, Min Li, Jianglong Li, Weiping Zhang, Yanwu Shi, Xueli Zhou, Wenyan Yao, Junchen Liu, Xiangwen Zhao, He Yan, Jinghui Wei, Min Xue, Wei Huang, Anning Zhang, Yaocun Zhang, Yu Shu, Qi Hu, Aixue 2021-05-26 application/pdf https://doi.org/10.5194/gmd-14-2977-2021 https://gmd.copernicus.org/articles/14/2977/2021/ eng eng doi:10.5194/gmd-14-2977-2021 https://gmd.copernicus.org/articles/14/2977/2021/ eISSN: 1991-9603 Text 2021 ftcopernicus https://doi.org/10.5194/gmd-14-2977-2021 2021-05-31T16:22:13Z BCC-CSM2-HR is a high-resolution version of the Beijing Climate Center (BCC) Climate System Model (T266 in the atmosphere and <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">4</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="f7b7a5d5bfd5c45cef6c295312dc1896"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gmd-14-2977-2021-ie00001.svg" width="20pt" height="14pt" src="gmd-14-2977-2021-ie00001.png"/></svg:svg> ∘ latitude × <math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">4</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="730b8b169cb37255af42cf31763b7866"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="gmd-14-2977-2021-ie00002.svg" width="20pt" height="14pt" src="gmd-14-2977-2021-ie00002.png"/></svg:svg> ∘ longitude in the ocean). Its development is on the basis of the medium-resolution version BCC-CSM2-MR (T106 in the atmosphere and 1 ∘ latitude × 1 ∘ longitude in the ocean) which is the baseline for BCC participation in the Coupled Model Intercomparison Project Phase 6 (CMIP6). This study documents the high-resolution model, highlights major improvements in the representation of atmospheric dynamical core and physical processes. BCC-CSM2-HR is evaluated for historical climate simulations from 1950 to 2014, performed under CMIP6-prescribed historical forcing, in comparison with its previous medium-resolution version BCC-CSM2-MR. Observed global warming trends of surface air temperature from 1950 to 2014 are well captured by both BCC-CSM2-MR and BCC-CSM2-HR. Present-day basic atmospheric mean states during the period from 1995 to 2014 are then evaluated at global scale, followed by an assessment on climate variabilities in the tropics including the tropical cyclones (TCs), the El Niño–Southern Oscillation (ENSO), the Madden–Julian Oscillation (MJO), and the quasi-biennial oscillation (QBO) in the stratosphere. It is shown that BCC-CSM2-HR represents the global energy balance well and can realistically reproduce the main patterns of atmospheric temperature and wind, precipitation, land surface air temperature, and sea surface temperature (SST). It also improves the spatial patterns of sea ice and associated seasonal variations in both hemispheres. The bias of the double intertropical convergence zone (ITCZ), obvious in BCC-CSM2-MR, almost disappears in BCC-CSM2-HR. TC activity in the tropics is increased with resolution enhanced. The cycle of ENSO, the eastward propagative feature and convection intensity of MJO, and the downward propagation of QBO in BCC-CSM2-HR are all in a better agreement with observations than their counterparts in BCC-CSM2-MR. Some imperfections are, however, noted in BCC-CSM2-HR, such as the excessive cloudiness in the eastern basin of the tropical Pacific with cold SST biases and the insufficient number of tropical cyclones in the North Atlantic. Text North Atlantic Sea ice Copernicus Publications: E-Journals Pacific Geoscientific Model Development 14 5 2977 3006