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Modelo Acoplado Oceano-Atmosfera×Índice de Precipitação Padronizado×
ÁreaGeofísicaGeofísica
FamíliaProcess / pipelineProcess / pipeline
Ano de origem19751993
Autor originalSyukuro Manabe, Kirk Bryan, and othersThomas McKee, Neil Doesken, and John Kleist
TipoCoupled atmosphere-ocean climate system simulationProbabilistic drought indicator
Fonte seminalManabe, S., Bryan, K., & Spelman, M. J. (1975). A global ocean-atmosphere climate model with seasonal variation for future studies of climate sensitivity. Journal of Physical Oceanography, 5(1), 3-29. link ↗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 ↗
Outros nomesAOGCMSPI
Relacionados33
ResumoAn Ocean-Atmosphere Coupled Model (AOGCM) is a comprehensive climate simulation that couples dynamic general circulation models of the atmosphere and ocean with explicit exchange of heat, momentum, and moisture at the interface. Developed by Manabe, Bryan, and colleagues in the 1970s, coupled models are essential for simulating climate change, ocean circulation changes, and climate-ocean interactions over decadal to centennial timescales.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.
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ScholarGateComparar métodos: Ocean-Atmosphere Coupled Model · Standardized Precipitation Index. Recuperado em 2026-06-19 de https://scholargate.app/pt/compare