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contributor authorRoberts, M. J.
contributor authorVidale, P. L.
contributor authorSenior, C.
contributor authorHewitt, H. T.
contributor authorBates, C.
contributor authorBerthou, S.
contributor authorChang, P.
contributor authorChristensen, H. M.
contributor authorDanilov, S.
contributor authorDemory, M.-E.
contributor authorGriffies, S. M.
contributor authorHaarsma, R.
contributor authorJung, T.
contributor authorMartin, G.
contributor authorMinobe, S.
contributor authorRingler, T.
contributor authorSatoh, M.
contributor authorSchiemann, R.
contributor authorScoccimarro, E.
contributor authorStephens, G.
contributor authorWehner, M. F.
date accessioned2019-09-19T10:09:00Z
date available2019-09-19T10:09:00Z
date copyright6/14/2018 12:00:00 AM
date issued2018
identifier otherbams-d-15-00320.1.pdf
identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4262093
description abstractAbstractThe time scales of the Paris Climate Agreement indicate urgent action is required on climate policies over the next few decades, in order to avoid the worst risks posed by climate change. On these relatively short time scales the combined effect of climate variability and change are both key drivers of extreme events, with decadal time scales also important for infrastructure planning. Hence, in order to assess climate risk on such time scales, we require climate models to be able to represent key aspects of both internally driven climate variability and the response to changing forcings. In this paper we argue that we now have the modeling capability to address these requirements?specifically with global models having horizontal resolutions considerably enhanced from those typically used in previous Intergovernmental Panel on Climate Change (IPCC) and Coupled Model Intercomparison Project (CMIP) exercises. The improved representation of weather and climate processes in such models underpins our enhanced confidence in predictions and projections, as well as providing improved forcing to regional models, which are better able to represent local-scale extremes (such as convective precipitation). We choose the global water cycle as an illustrative example because it is governed by a chain of processes for which there is growing evidence of the benefits of higher resolution. At the same time it comprises key processes involved in many of the expected future climate extremes (e.g., flooding, drought, tropical and midlatitude storms).
publisherAmerican Meteorological Society
titleThe Benefits of Global High Resolution for Climate Simulation: Process Understanding and the Enabling of Stakeholder Decisions at the Regional Scale
typeJournal Paper
journal volume99
journal issue11
journal titleBulletin of the American Meteorological Society
identifier doi10.1175/BAMS-D-15-00320.1
journal fristpage2341
journal lastpage2359
treeBulletin of the American Meteorological Society:;2018:;volume 099:;issue 011
contenttypeFulltext


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