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Krahasoni metodat

Shqyrtoni metodat e zgjedhura krah për krah; rreshtat që ndryshojnë janë të theksuar.

Thellimi Optik i Aerosoleve×Indeksi Standardizuar i Resë (SPI)×
FushaGjeofizikëGjeofizikë
FamiljaProcess / pipelineProcess / pipeline
Viti i origjinës19291993
KrijuesiAnders ÅngströmThomas McKee, Neil Doesken, and John Kleist
LlojiOptical parameter for aerosol loading quantificationProbabilistic drought indicator
Burimi themeluesÅngström, 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 ↗
Emërtime të tjeraAOD, Aerosol Optical ThicknessSPI
Të lidhura33
PërmbledhjaAerosol 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.
ScholarGateSeti i të dhënave
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ScholarGateKrahasoni metodat: Aerosol Optical Depth · Standardized Precipitation Index. Marrë më 2026-06-19 nga https://scholargate.app/sq/compare