Browse > Article
http://dx.doi.org/10.14191/Atmos.2018.28.1.037

Prediction Skill of East Asian Precipitation and Temperature Associated with El Niño in GloSea5 Hindcast Data  

Lim, So-Min (Earth System Research Division, National Institute of Meteorological Sciences)
Hyun, Yu-Kyung (Earth System Research Division, National Institute of Meteorological Sciences)
Kang, Hyun-Suk (Earth System Research Division, National Institute of Meteorological Sciences)
Yeh, Sang-Wook (Department of Marine Sciences and Convergent Technology, Hanyang University)
Publication Information
Atmosphere / v.28, no.1, 2018 , pp. 37-51 More about this Journal
Abstract
In this study, we investigate the performance of Global Seasonal Forecasting System version 5 (GloSea5) in Korea Meteorological Administration on the relationship between El $Ni{\tilde{n}}o$ and East Asian climate for the period of 1991~2010. It is found that the GloSea5 has a great prediction skill of El $Ni{\tilde{n}}o$ whose anomaly correlation coefficients of $Ni{\tilde{n}}o$ indices are over 0.96 during winter. The eastern Pacific (EP) El $Ni{\tilde{n}}o$ and the central Pacific (CP) El $Ni{\tilde{n}}o$ are considered and we analyze for EP El $Ni{\tilde{n}}o$, which is well simulated in GloSea5. The analysis period is divided into the developing phase of El $Ni{\tilde{n}}o$ summer (JJA(0)), mature phase of El $Ni{\tilde{n}}o$ winter (D(0)JF(1)), and decaying phase of El $Ni{\tilde{n}}o$ summer (JJA(1)). The GloSea5 simulates the relationship between precipitation and temperature in East Asia and the prediction skill for the East Asian precipitation and temperature varies depending on the El $Ni{\tilde{n}}o$ phase. While the precipitation and temperature are simulated well over the equatorial western Pacific region, there are biases in mid-latitude region during the JJA(0) and JJA(1). Because the low level pressure, wind, and vertical stream function are simulated weakly toward mid-latitude region, though they are similar with observation in low-latitude region. During the D(0)JF(1), the precipitation and temperature patterns analogize with observation in most regions, but there is temperature bias in inland over East Asia. The reason is that the GloSea5 poorly predicts the weakening of Siberian high, even though the shift of Aleutian low is predicted. Overall, the predictability of precipitation and temperature related to El $Ni{\tilde{n}}o$ in the GloSea5 is considered to be better in D(0)JF(1) than JJA(0) and JJA(1) and better in ocean than in inland region.
Keywords
GloSea5; Seasonal Prediction; El $Ni{\tilde{n}}o$; East Asia; Teleconnection;
Citations & Related Records
Times Cited By KSCI : 7  (Citation Analysis)
연도 인용수 순위
1 Webster, P. J., and S. Yang, 1992: Monsoon and ENSO: Selectively interactive systems. Quart. J. Roy. Meteor. Soc., 118, 877-926, doi:10.1002/qj.49711850705.   DOI
2 Wang, L., V. O. Magana, T. N. Palmer, J. Shukla, R. A. Tomas, M. Yanai, and T. Yasunari, 1998: Monsoons: Processes, predictability, and prospects for prediction. J. Geophys. Res., 103, 14451-14510, doi:10.1029/97JC02719.   DOI
3 Weng, H., K. Ashok, S. K. Behera, S. A. Rao, and T. Yamagata, 2007: Impacts of recent El Nino Modoki on dry/wet conditions in the Pacific rim during boreal summer. Climate Dyn., 29, 113-129, doi:10.1007/s00382-007-0234-0.   DOI
4 Weng, H., S. K. Behera, and T. Yamagata, 2009: Anomalous winter climate conditions in the Pacific rim during recent El Nino Modoki and El Nino events. Climate Dyn., 32, 663-674, doi:10.1007/s00382-008-0394-6.   DOI
5 Wu, R., Z.-Z. Hu, and B. P. Kirtman, 2003: Evolution of ENSO-related rainfall anomalies in East Asia. J. Climate, 16, 3742-3758, doi:10.1175/1520-0442(2003)016<3742:EOERAI>2.0.CO;2.   DOI
6 Yeh, S.-W., J.-S. Kug, B. Dewitte, M.-H. Kwon, B. P. Kirtman, and F.-F. Jin, 2009: El Nino in a changing climate. Nature, 461, 511-514, doi:10.1038/nature08316.   DOI
7 Yeo, S.-R., S.-W. Yeh, Y. Kim, and S.-Y. Yim, 2017: Monthly climate variation over Korea in relation to the two types of ENSO evolution. Int. J. Climatol., 38, 811-824, doi:10.1002/joc.5212.
8 Yuan, Y., and S. Yang, 2012: Impacts of different types of El Nino on the East Asian climate: focus on ENSO cycles. J. Climate, 25, 7702-7722, doi:10.1175/JCLID-11-00576.1.   DOI
9 Zhang, R., A. Sumi, and M. Kimoto, 1996: Impact of El Nino on the East Asian monsoon: A diagnostic study of the '86/87 and '91/92 events. J. Meteor. Soc. Japan, 74, 49-62, doi:10.2151/jmsj1965.74.1_49.   DOI
10 Shen, S., and K.-M. Lau, 1995: Biennial oscillation associated with the East Asian summer monsoon and tropical sea surface temperatures. J. Meteor. Soc. Japan, 73, 105-124, doi:10.2151/jmsj1965.73.1_105.   DOI
11 Best, M. J., and Coauthors, 2011: The Joint UK Land Environment Simulator (JULES), model description - Part 1: Energy and water fluxes. Geosci. Model Dev., 4, 677-699, doi:10.5194/gmd-4-677-2011.   DOI
12 Adler, R. F., and Coathors, 2003: The version-2 Global Precipitation Climatology Project (GPCP) monthly precipitation analysis (1979-present). J. Hydrometeor., 4, 1147-1167, doi:10.1175/1525-7541(2003)004<1147:TVGPCP>2.0.CO;2.   DOI
13 Alexander, M. A., I. Blade, M. Newman, J. R. Lanzante, N.-C. Lau, and J. D. Scott, 2002: The atmospheric bridge: the influence of ENSO teleconnections on airsea interaction over the global oceans. J. Climate., 15, 2205-2231, doi:10.1175/1520-0442(2002)015<2205:TABTIO>2.0.CO;2.   DOI
14 Ashok, K., S. K. Behera, S. A. Rao, H. Weng, and T. Yamagata, 2007: El Nino Modoki and its possible teleconnection. J. Geophys. Res., 112, C11007, doi:10.1029/2006JC003798.   DOI
15 Brown, A., S. Milton, M. Cullen, B. Golding, J. Mitchell, and A. Shelly, 2012: Unified modeling and prediction of weather and climate: A 25-year journey. Bull. Amer. Meteor. Soc., 93, 1865-1877, doi:10.1175/BAMS-D-12-00018.1.   DOI
16 Dee, D. P., and Coauthors, 2011: The ERA-Interim reanalysis: configuration and performance of the data assimilation system. Quart. J. Roy. Meteor. Soc., 137, 553-597, doi:10.1002/qj.828.   DOI
17 Imada, Y., H. Tatebe, M. Ishii, Y. Chikamoto, M. Mori, M. Arai, M. Watanabe, and M. Kimoto, 2015: Predictability of two types of El Nino assessed using an extended seasonal prediction system by MIROC. Mon. Wea. Rev., 143, 4597-4617, doi:10.1175/MWRD-15-0007.1.   DOI
18 Ho, C.-H., W. Choi, J. Kim, M.-K. Kim, and H.-D. Yoo, 2016: Does El Nino-Southern Oscillation affect the precipitation in Korea on seasonal time scales? Asia-Pac. J. Amos. Sci., 52, 395-403, doi:10.1007/s13143-016-0016-x.   DOI
19 Horel, J. D., and J. M. Wallace, 1981: Planetary-scale atmospheric phenomena associated with the southern oscillation. Mon. Wea. Rev., 109, 813-829, doi:10. 1175/1520-0493(1981)109<0813:PSAPAW>2.0.CO;2.   DOI
20 Hunke, E. C., and W. H. Lipscomb, 2010: CICE: The Los Alamos sea ice model documentation and software user's manual, Version 4.1, LA-CC-06-012. Technical report, Los Alamos National Laboratory, N.M, 116 pp.
21 Jeong, H.-I., and Coauthors, 2012: Assessment of the APCC coupled MME suite in predicting the distinctive climate impacts of two flavors of ENSO during boreal winter. Climate Dyn., 39, 475-493, doi:10.1007/s00382-012-1359-3.   DOI
22 Jeong, J.-H., and Coauthors, 2017: The status and prospect of seasonal climate prediction of climate over Korea and East Asia: A review. Asia-Pac. J. Atmos. Sci., 53, 149-173, doi:10.1007/s13143-017-0008-5.   DOI
23 Jhun, J.-G., and E.-J. Lee, 2004: A new East Asian winter monsoon index and associated characteristics of the winter monsoon. J. Climate, 17, 711-726, doi:10.1175/1520-0442(2004)017<0711:ANEAWM>2.0.CO;2.   DOI
24 Jung, M.-I., S.-W. Son, J. Choi, and H.-S. Kang, 2015: Assessment of 6-month lead prediction skill of the GloSea5 hindcast experiment. Atmosphere, 25, 323-337, doi:10.14191/Atmos.2015.25.2.323 (in Korean with English abstract).   DOI
25 Kim, S., H.-S. Kim, S.-K. Min, H.-Y. Son, D.-J. Won, H.-S. Jung, and J.-S. Kug, 2015: Intra-winter atmospheric circulation changes over East Asia and North Pacific associated with ENSO in a seasonal prediction model. Asia-Pac. J. Atmos. Sci., 51, 49-60, doi:10.1007/s13143-014-0059-9.   DOI
26 Kang, I.-S., and Y.-K. Jeong, 1996: Association of interannual variations of temperature and precipitation in Seoul with principal modes of pacific SST. Asia-Pac. J. Atmos. Sci., 32, 339-345.
27 Kim, H.-M., P. J. Webster, and J. A. Curry, 2012: Seasonal prediction skill of ECMWF System 4 and NCEP CFSv2 retrospective forecast for the Northern Hemisphere Winter. Climate Dyn., 39, 2957-2973, doi:10.1007/s00382-012-1364-6.   DOI
28 Kim, J.-S., J.-S. Kug, S.-W. Yeh, H.-K. Kim, and E.-H. Park, 2014: Relation between climate variability in Korea and two types of El Nino, and their sensitivity to definition of two types of El Nino. Atmosphere, 24, 89-99, doi:10.14191/Atmos.2014.24.1.089.   DOI
29 Kug, J.-S., F.-F. Jin, and S.-I. An, 2009: Two types of El Nino events: Cold tongue El Nino and warm pool El Nino. J. Climate, 22, 1499-1515, doi:10.1175/2008JCLI2624.1.   DOI
30 Lee, J.-Y., and Coauthors, 2017: The long-term variability of Changma in the East Asian summer monsoon system: A review and revisit. Asia-Pac. J. Atmos. Sci., 53, 257-272, doi:10.1007/s13143-017-0032-5.   DOI
31 MacLachlan, C., and Coauthors, 2014: Global Seasonal Forecast System version 5 (GloSea5): A high-resolution seasonal forecast system. Quart. J. Roy. Meteor. Soc., 141, 1072-1084, doi:10.1002/qj.2396.
32 Madec, G., 2008: NEMO ocean engine. Note du Pole de modelisation. Institut Pierre-Simon Laplace (IPSL), France, 27.
33 Ren, H.-L., and F.-F. Jin, 2011: Nino indices for two types of ENSO. Geophys. Res. Lett., 38, L04704, doi:10.1029/2010GL046031.
34 Min, S.-K., and Coauthors, 2015: Changes in weather and climate extremes over Korea and possible causes: A review. Asia-Pac. J. Atmos. Sci., 51, 103-121, doi:10.1007/s13143-015-0066-5.   DOI
35 Rasmusson, E. M., and T. H. Carpenter, 1982: Variations in tropical sea surface temperature and surface wind fields associated with the Southern Oscillation/El Nino. Mon. Wea. Rev., 110, 354-384, doi:10.1175/1520-0493(1982)110<0354:VITSST>2.0.CO;2.   DOI
36 Rayner, N. A., D. E. Parker, E. B. Horton, C. K. Folland, L. V. Alexander, D. P. Rowell, E. C. Kent, and A. Kaplan, 2003: Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century. J. Geophys. Res., 108, 4407, doi:10.1029/2002JD002670.   DOI
37 Son, H.-Y., J.-Y. Park, and J.-S. Kug, 2016: Precipitation variability in September over the Korean Peninsula during ENSO developing phase. Climate. Dyn., 46, 3419-3430, doi:10.1007/s00382-015-2776-x.   DOI
38 Trenberth, K. E., and D. J. Shea, 2005: Relationships between precipitation and surface temperature. Geophys. Res. Lett., 32, L14703, doi:10.1029/2005GL022760.
39 Walters, D. N., and Coauthors, 2011: The Met Office Unified Model global atmosphere 3.0/3.1 and JULES global land 3.0/3.1 configurations. Geosci. Model Dev., 4, 919-941, doi:10.5194/gmd-4-919-2011.   DOI
40 Wang, B., R. Wu, and X. Fu, 2000: Pacific-East Asian teleconnection: how does ENSO affect East Asian climate?. J. Climate, 13, 1517-1536, doi:10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO;2.   DOI
41 Wang, L., and W. Chen, 2010: How well do existing indices measure the strength of the East Asian winter monsoon?. Adv. Atmos. Sci., 27, 855-870, doi:10.1007/s00376-009-9094-3.   DOI
42 Wang, B., R. Wu, and K.-M. Lau, 2001: Interannual Variability of Asian Summer Monsoon: Contrasts between the Indian and the Western North Pacific-East Asian Monsoons. J. Climate, 14, 4073-4090, doi:10.1175/1520-0442(2001)014<4073:IVOTAS>2.0.CO;2.   DOI
43 Wang, B., Z. Wu, J. Li, J. Liu, C.-P. Chang, Y. Ding, and G. Wu, 2008: How to measure the strength of the East Asian summer monsoon. J. Climate, 21, 4449-4463, doi:10.1175/2008JCLI2183.1.   DOI