The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model
The importance of using a general circulation model that includes a well-resolved stratosphere for climate simulations, and particularly the influence this has on surface climate, is investigated. High top model sim- ulations are run with the Met Office Unified Model for the Coupled Model Intercompa...
Published in: | Journal of Climate |
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2016
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Online Access: | https://doi.org/10.1175/JCLI-D-11-00579.1 https://ora.ox.ac.uk/objects/uuid:5dd966b1-042e-4a24-a3a6-03466a2fa3fb |
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ftuloxford:oai:ora.ox.ac.uk:uuid:5dd966b1-042e-4a24-a3a6-03466a2fa3fb 2024-09-30T14:43:10+00:00 The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model Hardiman, S Butchart, N Hinton, T Osprey, S Gray, L 2016-07-28 https://doi.org/10.1175/JCLI-D-11-00579.1 https://ora.ox.ac.uk/objects/uuid:5dd966b1-042e-4a24-a3a6-03466a2fa3fb unknown doi:10.1175/JCLI-D-11-00579.1 https://ora.ox.ac.uk/objects/uuid:5dd966b1-042e-4a24-a3a6-03466a2fa3fb https://doi.org/10.1175/JCLI-D-11-00579.1 info:eu-repo/semantics/embargoedAccess Journal article 2016 ftuloxford https://doi.org/10.1175/JCLI-D-11-00579.1 2024-09-06T07:47:34Z The importance of using a general circulation model that includes a well-resolved stratosphere for climate simulations, and particularly the influence this has on surface climate, is investigated. High top model sim- ulations are run with the Met Office Unified Model for the Coupled Model Intercomparison Project Phase 5 (CMIP5). These simulations are compared to equivalent simulations run using a low top model differing only in vertical extent and vertical resolution above 15 km. The period 1960-2002 is analyzed and compared to observations and the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis dataset. Long-term climatology, variability, and trends in surface temperature and sea ice, along with the variability of the annular mode index, are found to be insensitive to the addition of a well-resolved stratosphere. The inclusion of a well-resolved stratosphere, however, does improve the impact of atmospheric teleconnections on surface climate, in particular the response to El Niño-Southern Oscillation, the quasi-biennial oscillation, and midwinter stratospheric sudden warmings (i.e., zonal mean wind reversals in the middle stratosphere). Thus, including a well-represented stratosphere could improve climate simulation on intraseasonal to in- terannual time scales. © 2012 American Meteorological Society. Article in Journal/Newspaper Sea ice ORA - Oxford University Research Archive Midwinter ENVELOPE(139.931,139.931,-66.690,-66.690) Journal of Climate 25 20 7083 7099 |
institution |
Open Polar |
collection |
ORA - Oxford University Research Archive |
op_collection_id |
ftuloxford |
language |
unknown |
description |
The importance of using a general circulation model that includes a well-resolved stratosphere for climate simulations, and particularly the influence this has on surface climate, is investigated. High top model sim- ulations are run with the Met Office Unified Model for the Coupled Model Intercomparison Project Phase 5 (CMIP5). These simulations are compared to equivalent simulations run using a low top model differing only in vertical extent and vertical resolution above 15 km. The period 1960-2002 is analyzed and compared to observations and the European Centre for Medium-Range Weather Forecasts (ECMWF) reanalysis dataset. Long-term climatology, variability, and trends in surface temperature and sea ice, along with the variability of the annular mode index, are found to be insensitive to the addition of a well-resolved stratosphere. The inclusion of a well-resolved stratosphere, however, does improve the impact of atmospheric teleconnections on surface climate, in particular the response to El Niño-Southern Oscillation, the quasi-biennial oscillation, and midwinter stratospheric sudden warmings (i.e., zonal mean wind reversals in the middle stratosphere). Thus, including a well-represented stratosphere could improve climate simulation on intraseasonal to in- terannual time scales. © 2012 American Meteorological Society. |
format |
Article in Journal/Newspaper |
author |
Hardiman, S Butchart, N Hinton, T Osprey, S Gray, L |
spellingShingle |
Hardiman, S Butchart, N Hinton, T Osprey, S Gray, L The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model |
author_facet |
Hardiman, S Butchart, N Hinton, T Osprey, S Gray, L |
author_sort |
Hardiman, S |
title |
The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model |
title_short |
The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model |
title_full |
The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model |
title_fullStr |
The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model |
title_full_unstemmed |
The Effect of a Well-Resolved Stratosphere on Surface Climate: Differences between CMIP5 Simulations with High and Low Top Versions of the Met Office Climate Model |
title_sort |
effect of a well-resolved stratosphere on surface climate: differences between cmip5 simulations with high and low top versions of the met office climate model |
publishDate |
2016 |
url |
https://doi.org/10.1175/JCLI-D-11-00579.1 https://ora.ox.ac.uk/objects/uuid:5dd966b1-042e-4a24-a3a6-03466a2fa3fb |
long_lat |
ENVELOPE(139.931,139.931,-66.690,-66.690) |
geographic |
Midwinter |
geographic_facet |
Midwinter |
genre |
Sea ice |
genre_facet |
Sea ice |
op_relation |
doi:10.1175/JCLI-D-11-00579.1 https://ora.ox.ac.uk/objects/uuid:5dd966b1-042e-4a24-a3a6-03466a2fa3fb https://doi.org/10.1175/JCLI-D-11-00579.1 |
op_rights |
info:eu-repo/semantics/embargoedAccess |
op_doi |
https://doi.org/10.1175/JCLI-D-11-00579.1 |
container_title |
Journal of Climate |
container_volume |
25 |
container_issue |
20 |
container_start_page |
7083 |
op_container_end_page |
7099 |
_version_ |
1811645092877828096 |