Agro Meteorology
evapotranspirasi
Global warming CMC
Atmosphere Layers separated by temperature variations. 1. Troposphere: 0-12 km -- where we live -- gets colder as you go up. -- all weather occurs here.
D. W. Shin, S. Cocke, Y.-K. Lim, T. E. LaRow, G. A. Baigorria, and J. J. OBrien Center for Ocean-Atmospheric Prediction Studies Florida State University,
Dust uplift and transport observed during the GERBILS campaign John Marsham 1, Doug Parker 1, Christian Grams 2, Qian Huang 1,3, Sarah Jones 2, Jim Haywood.
Trends in Water Cycle meeting, Paris, November 2004 Cloud and water vapour variability: models, reanalyses and observations Richard P. Allan and Tony Slingo.
SYSTEMATIC BIASES 3-hourly comparisons of top of atmosphere radiation from GERB and the Met Office global forecast model Systematic biases in model fluxes.
Part II: Observed Multi-Time Scale Variability in the Tropical Atlantic Part I: Biases in the NCEP CFS in the Tropical Atlantic Diagnosing CGCM bias and.
Chapt35
U3L2 - The Atmosphere
