Comparar métodos
Examine os métodos selecionados lado a lado; as linhas que diferem ficam destacadas.
| NDVI× | Modelo Acoplado Oceano-Atmosfera× | |
|---|---|---|
| Área | Geofísica | Geofísica |
| Família | Process / pipeline | Process / pipeline |
| Ano de origem≠ | 1973 | 1975 |
| Autor original≠ | Rouse, Haas, Schell, and Deering | Syukuro Manabe, Kirk Bryan, and others |
| Tipo≠ | Spectral index for vegetation assessment | Coupled atmosphere-ocean climate system simulation |
| Fonte seminal≠ | Rouse, J. W., Haas, R. H., Schell, J. A., & Deering, D. W. (1973). Monitoring vegetation systems in the Great Plains with ERTS. Third Earth Resources Technology Satellite Symposium Proceedings, 1, 309-317. link ↗ | Manabe, 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 ↗ |
| Outros nomes | NDVI | AOGCM |
| Relacionados | 3 | 3 |
| Resumo≠ | The Normalized Difference Vegetation Index (NDVI) is a spectral index computed from satellite or aerial multispectral imagery that quantifies vegetation greenness and vigor. Introduced by Rouse and colleagues in 1973 using Landsat data, NDVI has become the most widely used remote sensing metric for vegetation monitoring, drought assessment, crop productivity forecasting, and land cover change detection. | An 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. |
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