ENSO hindcast skill of the IAP-DecPreS near-term climate prediction system: comparison of full-field and anomaly initialization
Model initialization is a key process of climate predictions using dynamical models. In this study, the authors evaluated the performances of two distinct initialization approaches-anomaly and full-field initializations-in ENSO predictions conducted using the IAP-DecPreS near-term climate prediction...
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Published in | Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao Vol. 11; no. 1; pp. 54 - 62 |
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Main Authors | , , , |
Format | Journal Article |
Language | English |
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Beijing
Taylor & Francis
02.01.2018
KeAi Publishing Communications Ltd Elsevier KeAi Communications Co., Ltd |
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Abstract | Model initialization is a key process of climate predictions using dynamical models. In this study, the authors evaluated the performances of two distinct initialization approaches-anomaly and full-field initializations-in ENSO predictions conducted using the IAP-DecPreS near-term climate prediction system developed by the Institute of Atmospheric Physics (IAP). IAP-DecPreS is composed of the FGOALS-s2 coupled general circulation model and a newly developed ocean data assimilation scheme called 'ensemble optimal interpolation-incremental analysis update' (EnOI-IAU). It was found that, for IAP-DecPreS, the hindcast runs using the anomaly initialization have higher predictive skills for both conventional ENSO and El Niño Modoki, as compared to using the full-field initialization. The anomaly hindcasts can predict super El Niño/La Nina 10 months in advance and have good skill for most moderate and weak ENSO events about 4-7 months in advance. The predictive skill of the anomaly hindcasts for El Niño Modoki is close to that for conventional ENSO. On the other hand, the anomaly hindcasts at 1- and 4-month lead time can reproduce the major features of large-scale patterns of sea surface temperature, precipitation and atmospheric circulation anomalies during conventional ENSO and El Niño Modoki winter. |
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AbstractList | Model initialization is a key process of climate predictions using dynamical models. In this study, the authors evaluated the performances of two distinct initialization approaches—anomaly and full-field initializations—in ENSO predictions conducted using the IAP-DecPreS near-term climate prediction system developed by the Institute of Atmospheric Physics (IAP). IAP-DecPreS is composed of the FGOALS-s2 coupled general circulation model and a newly developed ocean data assimilation scheme called ‘ensemble optimal interpolation-incremental analysis update’ (EnOI-IAU). It was found that, for IAP-DecPreS, the hindcast runs using the anomaly initialization have higher predictive skills for both conventional ENSO and El Niño Modoki, as compared to using the full-field initialization. The anomaly hindcasts can predict super El Niño/La Nina 10 months in advance and have good skill for most moderate and weak ENSO events about 4–7 months in advance. The predictive skill of the anomaly hindcasts for El Niño Modoki is close to that for conventional ENSO. On the other hand, the anomaly hindcasts at 1- and 4-month lead time can reproduce the major features of large-scale patterns of sea surface temperature, precipitation and atmospheric circulation anomalies during conventional ENSO and El Niño Modoki winter. Model initialization is a key process of climate predictions using dynamical models. In this study, the authors evaluated the performances of two distinct initialization approaches-anomaly and full-field initializations-in ENSO predictions conducted using the IAP-DecPreS near-term climate prediction system developed by the Institute of Atmospheric Physics (IAP). IAP-DecPreS is composed of the FGOALS-s2 coupled general circulation model and a newly developed ocean data assimilation scheme called 'ensemble optimal interpolation-incremental analysis update' (EnOI-IAU). It was found that, for IAP-DecPreS, the hindcast runs using the anomaly initialization have higher predictive skills for both conventional ENSO and El Niño Modoki, as compared to using the full-field initialization. The anomaly hindcasts can predict super El Niño/La Nina 10 months in advance and have good skill for most moderate and weak ENSO events about 4-7 months in advance. The predictive skill of the anomaly hindcasts for El Niño Modoki is close to that for conventional ENSO. On the other hand, the anomaly hindcasts at 1- and 4-month lead time can reproduce the major features of large-scale patterns of sea surface temperature, precipitation and atmospheric circulation anomalies during conventional ENSO and El Niño Modoki winter. |
Author | WU, Bo YAN, Zi-Xiang ZHOU, Tian-Jun SUN, Qian |
Author_xml | – sequence: 1 givenname: Qian surname: SUN fullname: SUN, Qian organization: Leshan Central Station of Environment Monitoring – sequence: 2 givenname: Bo surname: WU fullname: WU, Bo email: wubo@mail.iap.ac.cn organization: LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences – sequence: 3 givenname: Tian-Jun surname: ZHOU fullname: ZHOU, Tian-Jun organization: LASG, Institute of Atmospheric Physics, Chinese Academy of Sciences – sequence: 4 givenname: Zi-Xiang surname: YAN fullname: YAN, Zi-Xiang organization: College of Atmospheric Science, Nanjing University of Information Science and Technology |
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CitedBy_id | crossref_primary_10_1007_s13351_020_9164_0 crossref_primary_10_1038_s41598_019_57183_3 crossref_primary_10_1029_2020JC017075 crossref_primary_10_1007_s00376_023_2122_x crossref_primary_10_1016_j_aosl_2023_100441 crossref_primary_10_3389_fclim_2021_736759 crossref_primary_10_1002_joc_6481 crossref_primary_10_1002_qj_4290 crossref_primary_10_1007_s00704_020_03229_w |
Cites_doi | 10.1175/1525-7541(2003)004<1147:TVGPCP>2.0.CO;2 10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO;2 10.1038/321827a0 10.1175/1520-0442(2002)015<2205:TABTIO>2.0.CO;2 10.5194/os-11-187-2015 10.1175/1520-0477-73.4.483 10.1175/BAMS-D-11-00111.1 10.1016/S0079-6611(01)00029-5 10.1007/s00382-013-1683-2 10.1029/98RG00715 10.1029/2006GL026994 10.1175/2008JCLI2624.1 10.1126/science.1132588 10.1002/qj.v137.656 10.1007/s00376-001-0047-8 10.1038/srep35909 10.1175/JCLI3526.1 10.1007/978-3-642-41801-3 10.1175/1520-0493(1981)109<0784:TITGHF>2.0.CO;2 10.1175/1520-0442(2004)017<2399:NAAOE>2.0.CO;2 10.1029/2006JC003798 10.1175/JCLI-D-14-00006.1 10.1175/JCLI-D-12-00265.1 10.1029/97JC02719 10.1080/07055900.1997.9649597 10.1029/2012GL051826 10.1038/nature08316 10.1175/1520-0493(1983)111<0517:TRBEEP>2.0.CO;2 10.1007/s10236-010-0307-1 10.1007/s00382-007-0234-0 10.1007/s00382-008-0397-3 10.1007/s00376-012-2113-9 |
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SubjectTerms | Anomalies anomaly initialization Atmospheric circulation Atmospheric physics Climate prediction coupled general circulation model Data collection El Nino El Nino phenomena ENSO prediction ENSO预测 full-field initialization General circulation models La Nina Near-term climate prediction system Ocean currents Oceanic analysis Physics Sea surface Sea surface temperature Southern Oscillation 全场初始化 异常场初始化 耦合环流模式 近期气候预测系统 |
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Title | ENSO hindcast skill of the IAP-DecPreS near-term climate prediction system: comparison of full-field and anomaly initialization |
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