AdaBoost-based satellite detection of summer daytime sea fog and low clouds in ice floe fields of the Arctic

IF 4.5 2区 地球科学 Q1 METEOROLOGY & ATMOSPHERIC SCIENCES
Atmospheric Research Pub Date : 2026-05-01 Epub Date: 2026-01-13 DOI:10.1016/j.atmosres.2026.108775
Huiyun Ma , Jiedong Liu , Zengwei Liu , Huihui Feng , Guannan Li , Runxi Gu
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引用次数: 0

Abstract

Under the trend of global warming, the Arctic region has experienced increasing warming and accelerating melting of sea ice, resulting in the opening of Arctic shipping routes with significant navigational potential. However, intense water vapor releases and a cold underlying surface can lead to frequent occurrences of sea fog and low clouds over the Arctic ice surfaces. Conducting detection of sea fog and low clouds is therefore highly important for ensuring the safety of Arctic shipping routes. In this study, a satellite detection algorithm for summer daytime sea fog and low clouds in ice floe fields of the Arctic has been proposed using the time series remote sensing data from the Moderate-Resolution Imaging Spectroradiometer (MODIS) and the AdaBoost method. Methodologically, three spectral indices, the normalized difference sea-water index (NDSWI), the sea-ice recognition index (SIRI), and the mid-high-cloud recognition index (MHCRI), are first constructed by analyzing the variations in reflection spectra for sea fog and low clouds, sea ice, sea water, and mid-high clouds. Additionally, three texture features, namely, the homogeneity, contrast, and entropy, of the brightness temperature at 11.030 μm (BT11.030 μm) are calculated using the gray-level co-occurrence matrix (GLCM). Subsequently, a strong learner classification model of the AdaBoost ensemble learning algorithm was built by adopting the samples of the spectral indices and texture features above and the weak learner of the decision. Finally, the residual mid-high clouds are removed through the threshold at BT11.030 μm. Verification indicated that the probability of detection (POD), false alarm rate (FAR), and critical success index (CSI) values were 84.44%, 9.45%, and 77.52%, respectively. This research supports the accurate detection of sea fog and low clouds in the Arctic, thereby ensuring safe navigation of Arctic shipping routes.
基于adaboost的北极浮冰区夏季日间海雾和低云的卫星探测
在全球变暖趋势下,北极地区气候变暖加剧,海冰加速融化,开辟了具有巨大航行潜力的北极航线。然而,强烈的水蒸气释放和寒冷的下层表面会导致北极冰表面频繁出现海雾和低云。因此,监测海雾和低云对保障北极航道安全具有重要意义。本文利用中分辨率成像光谱仪(MODIS)的时间序列遥感数据和AdaBoost方法,提出了一种北极浮冰区夏季日间海雾和低云的卫星探测算法。在方法上,通过分析海雾和低云、海冰、海水和中高云的反射光谱变化,首先构建归一化差分海水指数(NDSWI)、海冰识别指数(SIRI)和中高云识别指数(MHCRI)三个光谱指数。利用灰度共生矩阵(GLCM)计算了11.030 μm (BT11.030 μm)亮度温度的均匀性、对比度和熵三个纹理特征。随后,采用上述光谱指标和纹理特征的样本和决策的弱学习者,构建AdaBoost集成学习算法的强学习者分类模型。最后,通过阈值BT11.030 μm去除残余中高云。验证表明,检测概率(POD)、虚警率(FAR)和临界成功指数(CSI)值分别为84.44%、9.45%和77.52%。本研究支持对北极海域雾和低云的准确探测,从而保障北极航道的安全航行。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Atmospheric Research
Atmospheric Research 地学-气象与大气科学
CiteScore
9.40
自引率
10.90%
发文量
460
审稿时长
47 days
期刊介绍: The journal publishes scientific papers (research papers, review articles, letters and notes) dealing with the part of the atmosphere where meteorological events occur. Attention is given to all processes extending from the earth surface to the tropopause, but special emphasis continues to be devoted to the physics of clouds, mesoscale meteorology and air pollution, i.e. atmospheric aerosols; microphysical processes; cloud dynamics and thermodynamics; numerical simulation, climatology, climate change and weather modification.
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