A Strategy for Process-Oriented Validation of Coupled Chemistry–Climate ModelsSource: Bulletin of the American Meteorological Society:;2005:;volume( 086 ):;issue: 008::page 1117Author:Eyring, V.
,
Harris, N. R. P.
,
Rex, M.
,
Shepherd, T. G.
,
Fahey, D. W.
,
Amanatidis, G. T.
,
Austin, J.
,
Chipperfield, M. P.
,
Dameris, M.
,
Forster, P. M. De F.
,
Gettelman, A.
,
Graf, H. F.
,
Nagashima, T.
,
Newman, P. A.
,
Pawson, S.
,
Prather, M. J.
,
Pyle, J. A.
,
Salawitch, R. J.
,
Santer, B. D.
,
Waugh, D. W.
DOI: 10.1175/BAMS-86-8-1117Publisher: American Meteorological Society
Abstract: Accurate and reliable predictions and an understanding of future changes in the stratosphere are major aspects of the subject of climate change. Simulating the interaction between chemistry and climate is of particular importance, because continued increases in greenhouse gases and a slow decrease in halogen loading are expected. These both influence the abundance of stratospheric ozone. In recent years a number of coupled chemistry?climate models (CCMs) with different levels of complexity have been developed. They produce a wide range of results concerning the timing and extent of ozone-layer recovery. Interest in reducing this range has created a need to address how the main dynamical, chemical, and physical processes that determine the long-term behavior of ozone are represented in the models and to validate these model processes through comparisons with observations and other models. A set of core validation processes structured around four major topics (transport, dynamics, radiation, and stratospheric chemistry and microphysics) has been developed. Each process is associated with one or more model diagnostics and with relevant datasets that can be used for validation. This approach provides a coherent framework for validating CCMs and can be used as a basis for future assessments. Similar efforts may benefit other modeling communities with a focus on earth science research as their models increase in complexity.
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contributor author | Eyring, V. | |
contributor author | Harris, N. R. P. | |
contributor author | Rex, M. | |
contributor author | Shepherd, T. G. | |
contributor author | Fahey, D. W. | |
contributor author | Amanatidis, G. T. | |
contributor author | Austin, J. | |
contributor author | Chipperfield, M. P. | |
contributor author | Dameris, M. | |
contributor author | Forster, P. M. De F. | |
contributor author | Gettelman, A. | |
contributor author | Graf, H. F. | |
contributor author | Nagashima, T. | |
contributor author | Newman, P. A. | |
contributor author | Pawson, S. | |
contributor author | Prather, M. J. | |
contributor author | Pyle, J. A. | |
contributor author | Salawitch, R. J. | |
contributor author | Santer, B. D. | |
contributor author | Waugh, D. W. | |
date accessioned | 2017-06-09T16:42:53Z | |
date available | 2017-06-09T16:42:53Z | |
date copyright | 2005/08/01 | |
date issued | 2005 | |
identifier issn | 0003-0007 | |
identifier other | ams-72833.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4214880 | |
description abstract | Accurate and reliable predictions and an understanding of future changes in the stratosphere are major aspects of the subject of climate change. Simulating the interaction between chemistry and climate is of particular importance, because continued increases in greenhouse gases and a slow decrease in halogen loading are expected. These both influence the abundance of stratospheric ozone. In recent years a number of coupled chemistry?climate models (CCMs) with different levels of complexity have been developed. They produce a wide range of results concerning the timing and extent of ozone-layer recovery. Interest in reducing this range has created a need to address how the main dynamical, chemical, and physical processes that determine the long-term behavior of ozone are represented in the models and to validate these model processes through comparisons with observations and other models. A set of core validation processes structured around four major topics (transport, dynamics, radiation, and stratospheric chemistry and microphysics) has been developed. Each process is associated with one or more model diagnostics and with relevant datasets that can be used for validation. This approach provides a coherent framework for validating CCMs and can be used as a basis for future assessments. Similar efforts may benefit other modeling communities with a focus on earth science research as their models increase in complexity. | |
publisher | American Meteorological Society | |
title | A Strategy for Process-Oriented Validation of Coupled Chemistry–Climate Models | |
type | Journal Paper | |
journal volume | 86 | |
journal issue | 8 | |
journal title | Bulletin of the American Meteorological Society | |
identifier doi | 10.1175/BAMS-86-8-1117 | |
journal fristpage | 1117 | |
journal lastpage | 1133 | |
tree | Bulletin of the American Meteorological Society:;2005:;volume( 086 ):;issue: 008 | |
contenttype | Fulltext |