Improving the Predictability of the US Seasonal Surface Temperature With Convolutional Neural Networks Trained on CESM2 LENS

被引:0
|
作者
An, Yujay [1 ,2 ]
Kim, Hyemi [3 ,4 ]
机构
[1] Ward Melville High Sch, InSTAR, East Setauket, NY USA
[2] Princeton Univ, Princeton, NJ USA
[3] Ewha Womans Univ, Dept Sci Educ, Seoul, South Korea
[4] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA
基金
新加坡国家研究基金会;
关键词
machine learning; seasonal predictability; ENSO; US temperature; TELECONNECTIONS; PRECIPITATION; PREDICTION; ENSEMBLE;
D O I
10.1029/2024JD040961
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
To better understand and improve the prediction of the seasonal surface temperature (TS) across the United States, we employed convolutional neural network (CNN) models trained on the Community Earth System Model Version 2 Large Ensemble (CESM2 LENS). We used lagged sea surface temperatures (SST) over the tropical Pacific region, containing the information of the El Ni & ntilde;o Southern Oscillation (ENSO), as input for the CNN models. ENSO is the principal driver of variability in seasonal US surface temperatures (TSUS) and employing CNN models allows for spatiotemporal aspects of ENSO to be analyzed to make seasonal TSUS predictions. For predicting TSUS, the CNN models exhibited significantly improved skill over standard statistical multilinear regression (MLR) models and dynamical forecasts across most regions in the US, for lead times ranging from 1 to 6 months. Furthermore, we employed the CNN models to predict seasonal TSUS during extreme ENSO events. For these events, the CNN models outperformed the MLR models in predicting the effects on seasonal TSUS, suggesting that the CNN models are able to capture the ENSO-TSUS teleconnection more effectively. Results from a heatmap analysis demonstrate that the CNN models utilize spatial features of ENSO rather than solely the magnitude of the ENSO events, indicating that the improved skill of seasonal TSUS is due to analyzing spatial variation in ENSO events. The proposed CNN model demonstrates a promising improvement in prediction skill compared to existing methods, suggesting a potential path forward for enhancing TSUS forecast skill from subseasonal to seasonal timescales. While seasonal temperature forecasting is crucial for decision makers, it is generally a difficult task. A major setback to statistical machine learning methods for forecasting is the limited observational record. In our study, to bypass this, we used simulated climate model data, not historical data, to train machine learning (ML) models for seasonal surface temperature forecasts. We applied this method to train convolutional neural networks (CNN), a type of ML model that can analyze spatial patterns in data. We found that using CNN models greatly improves seasonal temperature predictions compared to standard linear models and that the CNN models effectively analyze spatial patterns in ENSO to make more accurate predictions. We concluded that using ML models is a promising method to improve seasonal temperature forecasts over the US. Seasonal predictability of US temperature is compared between CNN, statistical, and dynamical models Training CNN models on CESM2 LENS improves the seasonal predictability of US temperature Considering the spatiotemporal variability of tropical Pacific SST contributes to seasonal predictability improvement
引用
收藏
页数:12
相关论文
共 42 条
  • [1] Oceanic Harbingers of Pacific Decadal Oscillation Predictability in CESM2 Detected by Neural Networks
    Gordon, Emily M.
    Barnes, Elizabeth A.
    Hurrell, James W.
    GEOPHYSICAL RESEARCH LETTERS, 2021, 48 (21)
  • [2] Incorporating Uncertainty Into a Regression Neural Network Enables Identification of Decadal State-Dependent Predictability in CESM2
    Gordon, Emily M.
    Barnes, Elizabeth A.
    GEOPHYSICAL RESEARCH LETTERS, 2022, 49 (15)
  • [3] Ocean Complexity Shapes Sea Surface Temperature Variability in a CESM2 Coupled Model Hierarchy
    Larson, Sarah M.
    Mcmonigal, Kay
    Okumura, Yuko
    Amaya, Dillon
    Capotondi, Antonietta
    Bellomo, Katinka
    Simpson, Isla R.
    Clement, Amy C.
    JOURNAL OF CLIMATE, 2024, 37 (18) : 4931 - 4948
  • [4] Radial Lens Distortion Correction Using Convolutional Neural Networks Trained with Synthesized Images
    Rong, Jiangpeng
    Huang, Shiyao
    Shang, Zeyu
    Ying, Xianghua
    COMPUTER VISION - ACCV 2016, PT III, 2017, 10113 : 35 - 49
  • [5] Dominant factors influencing the seasonal predictability of US precipitation and surface air temperature
    Higgins, RW
    Leetmaa, A
    Xue, Y
    Barnston, A
    JOURNAL OF CLIMATE, 2000, 13 (22) : 3994 - 4017
  • [6] Sensitivity of Arctic Surface Temperature to Including a Comprehensive Ocean Interior Reflectance to the Ocean Surface Albedo Within the Fully Coupled CESM2
    Wei, Jian
    Ren, Tong
    Yang, Ping
    DiMarco, Steven F.
    Huang, Xianglei
    JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, 2023, 15 (12)
  • [7] Improvements in Wintertime Surface Temperature Variability in the Community Earth System Model Version 2 (CESM2) Related to the Representation of Snow Density
    Simpson, Isla R.
    Lawrence, David M.
    Swenson, Sean C.
    Hannay, Cecile
    McKinnon, Karen A.
    Truesdale, John E.
    JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS, 2022, 14 (04)
  • [8] Improving Resolution of 3D Surface With Convolutional Neural Networks
    Li, Zhen
    Yang, Xiaomin
    Song, Jianwen
    Liu, Kai
    Wang, Zuping
    Wu, Wei
    SUSTAINABLE CITIES AND SOCIETY, 2018, 42 : 127 - 138
  • [9] Small Impact of Stratospheric Dynamics and Chemistry on the Surface Temperature of the Last Glacial Maximum in CESM2(WACCM6ma)
    Zhu, Jiang
    Otto-Bliesner, Bette L.
    Garcia, Rolando
    Brady, Esther C.
    Mills, Mike
    Kinnison, Douglas
    Lamarque, Jean-Francois
    GEOPHYSICAL RESEARCH LETTERS, 2022, 49 (20)
  • [10] Predictability of sea surface temperature anomalies in the Indian Ocean using artificial neural networks
    Tripathi, K. C.
    Das, I. M. L.
    Sahai, A. K.
    INDIAN JOURNAL OF MARINE SCIENCES, 2006, 35 (03): : 210 - 220