Võrdle meetodeid

	Barnes-Cressmani analüüs	Skew-T Log-P analüüs	WRF mudel
Valdkond	Meteoroloogia	Meteoroloogia	Meteoroloogia
Perekond	Process / pipeline	Process / pipeline	Process / pipeline
Tekkeaasta	1959	1960s	2000
Looja	Barnes, Cressman	Reitan, Skamarock	Skamarock and Klemp
Tüüp	Objective analysis method	Graphical thermodynamic tool	Atmospheric simulation system
Algallikas	Barnes, S. L. (1964). A Technique for Maximizing Details in Numerical Weather Map Analysis. Journal of Applied Meteorology, 3(4), 396-409.	Bluestein, H. B. (1992). Synoptic-dynamic meteorology in midlatitudes. Volume I: Principles of Kinematics and Dynamics. Oxford University Press.	Skamarock, W. C., Klemp, J. B., Dudhia, J., et al. (2008). A Description of the Advanced Research WRF Version 3. NCAR Technical Note NCAR/TN-475+STR.
Rööpnimetused	Barnes analysis, Cressman analysis, Objective analysis, Grid interpolation	Skew-T, Skew-T Log-P diagram, Tephigram, Stuve diagram	Weather Research and Forecasting, WRF, ARW, NMM
Seotud	2	3	4
Kokkuvõte	Barnes-Cressman analysis is an objective interpolation method that creates gridded meteorological fields from irregularly spaced observations (station data, radiosonde profiles, buoys). It is widely used for synoptic analysis, quality control, and initialization of numerical weather models.	The Skew-T Log-P diagram is a thermodynamic chart used extensively in meteorology to visualize atmospheric profiles of temperature, dew point, and pressure. Developed in its modern form by Reitan in the 1960s, it allows forecasters and researchers to quickly assess atmospheric stability, convective potential, wind shear, and other properties critical for weather diagnosis and prediction.	The Weather Research and Forecasting (WRF) model is a mesoscale atmospheric simulation system used for weather forecasting, research, and climate applications. Developed cooperatively by NCAR, NOAA, and academic institutions, WRF became operational in 2004 and has become one of the most widely used atmospheric models worldwide.