UntitledSource: Journal of Climate:;2017:;volume( 030 ):;issue: 014::page 5221DOI: 10.1175/JCLI-D-16-0488.1Publisher: American Meteorological Society
Abstract: AbstractA neural-network-based cluster technique, the so-called self-organizing map (SOM), was performed to extract distinct sea surface temperature (SST) anomaly patterns during boreal winter. The SOM technique has advantages in nonlinear feature extraction compared to the commonly used empirical orthogonal function analysis and is widely used in meteorology. The eight distinguishable SOM patterns so identified represent three La Niña?like patterns, two near-normal patterns, and three El Niño?like patterns. These patterns show the varied amplitude and location of the SST anomalies associated with El Niño and La Niña, such as the central Pacific (CP) and eastern Pacific (EP) El Niño. The impact of each distinctive SOM pattern on winter-mean surface temperature and precipitation changes over North America was examined. Based on composite maps with observational data, each SOM pattern corresponds to a distinguishable spatial structure of temperature and precipitation anomaly over North America, which seems to result from differing wave train patterns, extending from the tropics to mid?high latitudes induced by longitudinally shifted tropical heating. The corresponding teleconnection as represented by the National Center for Atmospheric Research Community Atmospheric Model, version 4 (CAM4), was compared with the observational results. It was found that the 16-member ensemble average of the CAM4 experiments with prescribed SST can reproduce the observed atmospheric circulation responses to the different SST SOM patterns, which suggests that the circulation differences are largely SST driven rather than due to internal atmospheric variability.
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| contributor author | Guo, Yuanyuan;Ting, Mingfang;Wen, Zhiping;Lee, Dong Eun | |
| date accessioned | 2018-01-03T11:00:44Z | |
| date available | 2018-01-03T11:00:44Z | |
| date copyright | 3/28/2017 12:00:00 AM | |
| date issued | 2017 | |
| identifier other | jcli-d-16-0488.1.pdf | |
| identifier uri | http://138.201.223.254:8080/yetl1/handle/yetl/4246012 | |
| description abstract | AbstractA neural-network-based cluster technique, the so-called self-organizing map (SOM), was performed to extract distinct sea surface temperature (SST) anomaly patterns during boreal winter. The SOM technique has advantages in nonlinear feature extraction compared to the commonly used empirical orthogonal function analysis and is widely used in meteorology. The eight distinguishable SOM patterns so identified represent three La Niña?like patterns, two near-normal patterns, and three El Niño?like patterns. These patterns show the varied amplitude and location of the SST anomalies associated with El Niño and La Niña, such as the central Pacific (CP) and eastern Pacific (EP) El Niño. The impact of each distinctive SOM pattern on winter-mean surface temperature and precipitation changes over North America was examined. Based on composite maps with observational data, each SOM pattern corresponds to a distinguishable spatial structure of temperature and precipitation anomaly over North America, which seems to result from differing wave train patterns, extending from the tropics to mid?high latitudes induced by longitudinally shifted tropical heating. The corresponding teleconnection as represented by the National Center for Atmospheric Research Community Atmospheric Model, version 4 (CAM4), was compared with the observational results. It was found that the 16-member ensemble average of the CAM4 experiments with prescribed SST can reproduce the observed atmospheric circulation responses to the different SST SOM patterns, which suggests that the circulation differences are largely SST driven rather than due to internal atmospheric variability. | |
| publisher | American Meteorological Society | |
| type | Journal Paper | |
| journal volume | 30 | |
| journal issue | 14 | |
| journal title | Journal of Climate | |
| identifier doi | 10.1175/JCLI-D-16-0488.1 | |
| journal fristpage | 5221 | |
| journal lastpage | 5241 | |
| tree | Journal of Climate:;2017:;volume( 030 ):;issue: 014 | |
| contenttype | Fulltext |