GloSea5 모형의 6개월 장기 기후 예측성 검증

This study explores the 6-month lead prediction skill of several climate indices that influence on East Asian climate in the GloSea5 hindcast experiment. Such indices include Nino3.4, Indian Ocean Diploe (IOD), Arctic Oscillation (AO), various summer and winter Asian monsoon indices. The models pred...

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Published in:Atmosphere
Main Authors: 정명일, 손석우, 최정, 강현석
Format: Article in Journal/Newspaper
Language:unknown
Published: 한국기상학회 2018
Subjects:
Online Access:https://hdl.handle.net/10371/207191
https://doi.org/10.14191/Atmos.2015.25.2.323
id ftseoulnuniv:oai:s-space.snu.ac.kr:10371/207191
record_format openpolar
spelling ftseoulnuniv:oai:s-space.snu.ac.kr:10371/207191 2024-09-09T19:23:48+00:00 GloSea5 모형의 6개월 장기 기후 예측성 검증 Assessment of 6-Month Lead Prediction Skill of the GloSea5 Hindcast Experiment 정명일 손석우 최정 강현석 손석우 2018-11-02 https://hdl.handle.net/10371/207191 https://doi.org/10.14191/Atmos.2015.25.2.323 한국어 unknown 한국기상학회 대기, Vol.25 No.2, pp.323-337 1598-3560 https://hdl.handle.net/10371/207191 doi:10.14191/Atmos.2015.25.2.323 000422581100011 65319 ART002011051 ARCTIC OSCILLATION SUMMER MONSOON INDIAN-OCEAN EAST-ASIA WINTER PREDICTABILITY PRECIPITATION ENSO TELECONNECTIONS CLIMATOLOGY GloSea5 seasonal prediction climate index Article ART 2018 ftseoulnuniv https://doi.org/10.14191/Atmos.2015.25.2.323 2024-08-13T23:46:33Z This study explores the 6-month lead prediction skill of several climate indices that influence on East Asian climate in the GloSea5 hindcast experiment. Such indices include Nino3.4, Indian Ocean Diploe (IOD), Arctic Oscillation (AO), various summer and winter Asian monsoon indices. The models prediction skill of these indices is evaluated by computing the anomaly correlation coefficient (ACC) and mean squared skill score (MSSS) for ensemble mean values over the period of 1996~2009. In general, climate indices that have low seasonal variability are predicted well. For example, in terms of ACC, Nino3.4 index is predicted well at least 6 months in advance. The IOD index is also well predicted in late summer and autumn. This contrasts with the prediction skill of AO index which shows essentially no skill beyond a few months except in February and August. Both summer and winter Asian monsoon indices are also poorly predicted. An exception is the Western North Pacific Monsoon (WNPM) index that exhibits a prediction skill up to 4- to 6-month lead time. However, when MSSS is considered, most climate indices, except Nino3.4 index, show a negligible prediction skill, indicating that conditional bias is significant in the model. These results are only weakly sensitive to the number of ensemble members. N 2 Article in Journal/Newspaper Arctic Seoul National University: S-Space Arctic Indian Pacific Atmosphere 25 2 323 337
institution Open Polar
collection Seoul National University: S-Space
op_collection_id ftseoulnuniv
language unknown
topic ARCTIC OSCILLATION
SUMMER MONSOON
INDIAN-OCEAN
EAST-ASIA
WINTER
PREDICTABILITY
PRECIPITATION
ENSO
TELECONNECTIONS
CLIMATOLOGY
GloSea5
seasonal prediction
climate index
spellingShingle ARCTIC OSCILLATION
SUMMER MONSOON
INDIAN-OCEAN
EAST-ASIA
WINTER
PREDICTABILITY
PRECIPITATION
ENSO
TELECONNECTIONS
CLIMATOLOGY
GloSea5
seasonal prediction
climate index
정명일
손석우
최정
강현석
GloSea5 모형의 6개월 장기 기후 예측성 검증
topic_facet ARCTIC OSCILLATION
SUMMER MONSOON
INDIAN-OCEAN
EAST-ASIA
WINTER
PREDICTABILITY
PRECIPITATION
ENSO
TELECONNECTIONS
CLIMATOLOGY
GloSea5
seasonal prediction
climate index
description This study explores the 6-month lead prediction skill of several climate indices that influence on East Asian climate in the GloSea5 hindcast experiment. Such indices include Nino3.4, Indian Ocean Diploe (IOD), Arctic Oscillation (AO), various summer and winter Asian monsoon indices. The models prediction skill of these indices is evaluated by computing the anomaly correlation coefficient (ACC) and mean squared skill score (MSSS) for ensemble mean values over the period of 1996~2009. In general, climate indices that have low seasonal variability are predicted well. For example, in terms of ACC, Nino3.4 index is predicted well at least 6 months in advance. The IOD index is also well predicted in late summer and autumn. This contrasts with the prediction skill of AO index which shows essentially no skill beyond a few months except in February and August. Both summer and winter Asian monsoon indices are also poorly predicted. An exception is the Western North Pacific Monsoon (WNPM) index that exhibits a prediction skill up to 4- to 6-month lead time. However, when MSSS is considered, most climate indices, except Nino3.4 index, show a negligible prediction skill, indicating that conditional bias is significant in the model. These results are only weakly sensitive to the number of ensemble members. N 2
author2 손석우
format Article in Journal/Newspaper
author 정명일
손석우
최정
강현석
author_facet 정명일
손석우
최정
강현석
author_sort 정명일
title GloSea5 모형의 6개월 장기 기후 예측성 검증
title_short GloSea5 모형의 6개월 장기 기후 예측성 검증
title_full GloSea5 모형의 6개월 장기 기후 예측성 검증
title_fullStr GloSea5 모형의 6개월 장기 기후 예측성 검증
title_full_unstemmed GloSea5 모형의 6개월 장기 기후 예측성 검증
title_sort glosea5 모형의 6개월 장기 기후 예측성 검증
publisher 한국기상학회
publishDate 2018
url https://hdl.handle.net/10371/207191
https://doi.org/10.14191/Atmos.2015.25.2.323
geographic Arctic
Indian
Pacific
geographic_facet Arctic
Indian
Pacific
genre Arctic
genre_facet Arctic
op_relation 대기, Vol.25 No.2, pp.323-337
1598-3560
https://hdl.handle.net/10371/207191
doi:10.14191/Atmos.2015.25.2.323
000422581100011
65319
ART002011051
op_doi https://doi.org/10.14191/Atmos.2015.25.2.323
container_title Atmosphere
container_volume 25
container_issue 2
container_start_page 323
op_container_end_page 337
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