Сравнение методов
Просматривайте выбранные методы рядом; строки с различиями подсвечены.
| Оптическая толщина аэрозоля× | Стандартизированный индекс осадков× | |
|---|---|---|
| Область | Геофизика | Геофизика |
| Семейство | Process / pipeline | Process / pipeline |
| Год появления≠ | 1929 | 1993 |
| Автор метода≠ | Anders Ångström | Thomas McKee, Neil Doesken, and John Kleist |
| Тип≠ | Optical parameter for aerosol loading quantification | Probabilistic drought indicator |
| Основополагающий источник≠ | Ångström, A. (1929). On the atmospheric transmission of sun radiation and on dust in the air. Geografiska Annaler, 11(2), 156-166. DOI ↗ | McKee, T. B., Doesken, N. J., & Kleist, J. (1993). The relationship of drought frequency and duration to time scales. Proceedings of the Eighth Conference on Applied Climatology, 179-184. link ↗ |
| Другие названия≠ | AOD, Aerosol Optical Thickness | SPI |
| Связанные | 3 | 3 |
| Сводка≠ | Aerosol Optical Depth (AOD) is a dimensionless measure of aerosol light extinction in the atmosphere, quantifying how much sunlight is scattered and absorbed by particles suspended in air. Formalized by Ångström in 1929 and now routinely measured via satellite (MODIS, Sentinel-5P) and ground networks (AERONET), AOD is essential for air quality monitoring, climate forcing assessment, and visibility prediction. | The Standardized Precipitation Index (SPI) is a climate index that quantifies precipitation anomalies relative to historical norms, standardized to account for differences in precipitation climatology across regions. Introduced by McKee, Doesken, and Kleist in 1993, SPI has become a primary tool for drought detection and characterization, adopted by meteorological agencies worldwide for operational drought monitoring and early warning systems. |
| ScholarGateНабор данных ↗ |
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