| 秋季巴倫支海-喀拉海海冰面積異常對渤海、黃海冰情的影響 |
| 作者:劉鑫1 2 趙倩3 李大超4 陳海軍5 初宇峰4 聶曉文4 隋俊鵬3 |
單位:1. 中國華能集團(tuán)清潔能源技術(shù)研究院有限公司, 北京 102209; 2. 國家能源海上風(fēng)電工程與運行技術(shù)研發(fā)中心, 北京 102209; 3. 國家海洋環(huán)境預(yù)報中心, 北京 100081; 4. 華能遼寧清潔能源有限責(zé)任公司, 遼寧 沈陽 110015; 5. 遼寧省自然資源事務(wù)服務(wù)中心, 遼寧 沈陽 1 |
| 關(guān)鍵詞:海冰 渤海 黃海 巴倫支海-喀拉海 冰情預(yù)測 |
| 分類號:P73l.32 |
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| 出版年·卷·期(頁碼):2025·42·第一期(32-37) |
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摘要:
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| 利用美國國家冰雪數(shù)據(jù)中心海冰覆蓋面積月平均數(shù)據(jù)、美國氣象環(huán)境預(yù)報中心/美國國家大氣研究中心月平均再分析資料和渤海、黃海冰情等級數(shù)據(jù),研究了秋季巴倫支海-喀拉海海冰面積異常對渤海、黃海冰情的影響。結(jié)果表明:去趨勢的秋季巴倫支海-喀拉海海冰面積與渤海、黃海冰情等級呈顯著的負(fù)相關(guān),相關(guān)系數(shù)為-0.54;秋季巴倫支海-喀拉海海冰面積異常偏少,有利于高緯度冷空氣南下,冷空氣活動頻繁造成冬季我國北方地區(qū)氣溫偏低,導(dǎo)致渤海、黃海冰情偏重,反之亦然;若前期秋季巴倫支海-喀拉海海冰面積呈負(fù)異常,則冬季渤海、黃海發(fā)生嚴(yán)重冰情的概率較大,近42年冬季渤海、黃海冰情等級在3級以上的年份,前期秋季巴倫支海-喀拉海海冰面積均為負(fù)異常。因此,前期秋季巴倫支海-喀拉海海冰面積可以作為我國冬季渤海、黃海冰情的預(yù)測因子。 |
| The effect of autumn sea ice area anomaly in the Barents-Kara Seas on ice condition of the Bohai Sea and the Yellow Sea was analyzed based on the National Snow and Ice Data Center monthly sea ice area data, the National Center for Environmental Prediction/National Center for Atmospheric Research reanalysis data, and the ice grade data in the Bohai Sea and the Yellow Sea. The results show that the detrended autumn sea ice area anomaly in the Barents-Kara Seas is negatively correlated to the ice grade in the Bohai Sea and the Yellow Sea with a correlation of -0.54. During the low autumn sea ice year in the Barents-Kara Seas, the frequency of cold air activity increases and winter temperature in north China is below normal, leading to heavier ice condition in the Bohai Sea and the Yellow Sea, and vice versa. When autumn sea ice area is negative anomaly in the BarentsKara Seas, there is a high probability of heavier ice condition in the Bohai Sea and the Yellow Sea. Autumn sea ice area is negative anomaly in the Barents-Kara Seas when ice grade is above Grade 3 in the past 42 years. Therefore, the autumn sea ice area in the Barents-Kara Seas is a good predictor of ice condition in the Bohai Sea and the Yellow Sea. |
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