基于深度学习的西北太平洋叶绿素-a 对热带气旋响应的预报模型

IF 3.1 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES Ocean Modelling Pub Date : 2024-03-05 DOI:10.1016/j.ocemod.2024.102345
Haobin Cen , Guoqing Han , Xiayan Lin , Yu Liu , Han Zhang
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引用次数: 0

摘要

热带气旋会导致海面叶绿素-a 浓度增加,这对研究区域海洋环境的变化非常重要。精确预报热带气旋引起的海面叶绿素-a 浓度变化仍是一项挑战。本研究应用双向长短期记忆(BiLSTM)神经网络深度学习模型预测了北太平洋西部(WNP)台风诱发的海面叶绿素-a浓度变化。2011 年至 2020 年的台风作为训练案例,2021 年至 2022 年的台风作为预测和测试案例。深度学习模型的输入变量包括 10 米海面风速(U10 和 V10)、海面温度异常(SSTA)和海面叶绿素-a 浓度。输出变量是台风过后一天的叶绿素-a 浓度。使用前 7 天的数据预测台风过境后一天的叶绿素-a 浓度,并使用滚动预测法预测随后 7 天的叶绿素-a 浓度。为了评估输入变量对模型预报性能的影响,进行了消融实验。结果表明,当使用 U10、V10 和前七天的叶绿素-a 作为输入变量时,模型的整体预报性能最佳。以台风 "灿都"、"仁发 "和 "马鹿 "为例,预报结果的均方根误差(RMSE)分别为 0.0143 毫克-米-3、0.0087 毫克-米-3 和 0.空间异常相关系数(ACC)分别为 0.9968、0.9775 和 0.9721。结果表明,在中等强度台风 "梅花 "的中期阶段,预报性能最为准确,其 RMSE、MAE 和 ACC 值分别为 0.0040 mg - m-3、0.0032 mg - m-3 和 0.9894。BiLSTM 神经网络模型对中等强度台风和中期台风的预报效果最好。这是因为中等强度台风或任何台风的成熟阶段往往有相对稳定和更可预测的路径,从而能更好地预测叶绿素-a 的浓度。在今后的工作中,我们打算将我们的训练和预测扩展到不同强度的台风,旨在进一步完善和提高预测性能。
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Deep learning-based forecasting model for chlorophyll-a response to tropical cyclones in the Western North Pacific

Tropical cyclones cause increases in sea surface chlorophyll-a concentration, which is important for studying variations in the regional marine environment. Precisely forecasting the variations of sea surface chlorophyll-a concentration induced by tropical cyclones remains a challenge. In this research, a bidirectional long short-term memory (BiLSTM) neural network deep learning model was applied to predict the variations of sea surface chlorophyll-a concentration induced by typhoons in the Western North Pacific (WNP). Typhoons occurring between 2011 and 2020 were used as training cases and those from 2021 to 2022 as forecasting and testing cases. The input variables of the deep learning model include the sea surface wind at 10 meters (U10 and V10), sea surface temperature anomaly (SSTA), and sea surface chlorophyll-a concentration. The output variable was the chlorophyll-a concentration one day after the passage of the typhoon. Data from the previous 7 days were used to predict the chlorophyll-a concentration one day after the typhoon's passage, and the rolling forecast method was employed to predict chlorophyll-a concentration in the following 7 days. To assess the impact of input variables on the model's forecasting performance, ablation experiments were conducted. The results showed that when using U10, V10, and chlorophyll-a from the previous seven days as inputs, the model exhibited the best overall forecasting performance. Taking Typhoons Chanthu, In-fa, and Malou as examples, the root mean square error (RMSE) for the forecast results are 0.0143 mg · m−3, 0.0087 mg · m−3, and 0.0030 mg · m−3, the mean absolute errors (MAE) are 0.0072 mg · m−3, 0.0074 mg · m−3, and 0.0025 mg · m−3, and the spatial anomaly correlation coefficients (ACC) are 0.9968, 0.9775, and 0.9721, respectively. The results reveal that the most accurate forecasting performance was observed during the mid-phase of the moderate-intensity Typhoon Muifa, with RMSE, MAE, and ACC values of 0.0040 mg · m−3, 0.0032 mg · m−3, and 0.9894, respectively. The BiLSTM neural network model had the best forecasting performance for typhoons of moderate intensity and during the mid-term phase. This is because moderate-intensity typhoons or the mature phase of any typhoon tend to have relatively stable and more predictable paths, resulting in better predictions of chlorophyll-a concentrations. In future work, we intend to extend our training and forecasting to typhoons of various intensities, aiming to further refine and enhance predictive performance.

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来源期刊
Ocean Modelling
Ocean Modelling 地学-海洋学
CiteScore
5.50
自引率
9.40%
发文量
86
审稿时长
19.6 weeks
期刊介绍: The main objective of Ocean Modelling is to provide rapid communication between those interested in ocean modelling, whether through direct observation, or through analytical, numerical or laboratory models, and including interactions between physical and biogeochemical or biological phenomena. Because of the intimate links between ocean and atmosphere, involvement of scientists interested in influences of either medium on the other is welcome. The journal has a wide scope and includes ocean-atmosphere interaction in various forms as well as pure ocean results. In addition to primary peer-reviewed papers, the journal provides review papers, preliminary communications, and discussions.
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