超干旱地区的非静止干旱模式:空间时间和多时间尺度干旱分析
Mohammad Reza Nikoo1, Erfan Zarei2, Malik Al-Wardy2
1Department of Civil and Architectural Engineering, Sultan Qaboos University, Muscat, Oman.
The Science of the total environment
|September 5, 2025
概括
气候变化影响了阿曼的干旱. 非静态模型比静态模型更好地捕捉干旱动态,揭示区域趋势并为水政策提供信息.
科学领域:
- 气候学
- 水文学
- 环境科学
背景情况:
- 干旱是严重的自然灾害,特别是在像阿曼这样的干旱地区.
- 由于气候变化,固定干旱评估可能不足.
- 之前的研究经常使用基于点的方法,缺少空间干旱变异性.
研究的目的:
- 使用高分辨率数据评估阿曼的静止和非静止干旱趋势.
- 在不同时间尺度上比较不同干旱模型的性能.
- 分析空间和时间干旱动态以改善监测.
主要方法:
- 使用ERA5-Land数据 (1950-2024) 进行标准化降水蒸发指数 (SPEI) 在3个月,6个月和12个月的尺度.
- 应用了基于像素的静态和非静态日志逻辑参数模型.
- 使用Akaike信息标准 (AIC) 进行详细干旱分析的最佳模型.
主要成果:
- 非静态模型的表现优于静态模型,特别是长期干旱 (SPEI-12).
- 短期干旱 (SPEI-3) 最好用非静止位置转移来描述;SPEI-12需要动态平均值和变化.
- 北部和中部的湿度趋势有所增加,而东部沿海地区则趋于干旱.
结论:
- 在干旱地区进行干旱评估的非静止模型提供了优越的方法.
- 在气候变化下需要动态干旱监测.
- 结果为阿曼制定适应气候变化的水资源政策和早期预警系统提供了关键的见解.
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