विधियों की तुलना करें
चुनी हुई विधियों की आमने-सामने समीक्षा करें; भिन्नता वाली पंक्तियाँ रेखांकित हैं।
| कोहलर सिद्धांत× | मेघ संघनन नाभिक विश्लेषण× | |
|---|---|---|
| क्षेत्र | मौसम विज्ञान | मौसम विज्ञान |
| परिवार | Process / pipeline | Process / pipeline |
| उद्भव वर्ष≠ | 1936 | 1959 |
| प्रवर्तक≠ | Hilding Kohler | Twomey, Woodard |
| प्रकार≠ | Thermodynamic equilibrium framework | Cloud microphysical measurement |
| मौलिक स्रोत≠ | Köhler, H. (1936). The nucleus in and the growth of hygroscopic droplets. Transactions of the Faraday Society, 32, 1152-1161. DOI ↗ | Dusek, U., Frank, G. P., Hildebrandt, L., et al. (2006). Size matters more than chemistry for cloud-nucleating ability of aerosol particles. Science, 312(5778), 1375-1378. DOI ↗ |
| उपनाम | Kohler theory, Kohler equilibrium, Cloud droplet nucleation | CCN analysis, Cloud condensation nuclei, CCN measurement |
| संबंधित | 3 | 3 |
| सारांश≠ | Köhler theory is a foundational framework in cloud microphysics that predicts the equilibrium supersaturation required for an aerosol particle of given size and composition to grow into a cloud droplet. Published in 1936 by Hilding Köhler, it combines the Kelvin effect (vapor pressure enhancement over curved surfaces) with the Raoult effect (vapor pressure depression from dissolved solute) to explain cloud droplet formation. | Cloud condensation nuclei (CCN) analysis examines the number and properties of aerosol particles capable of nucleating cloud droplets at various supersaturation levels. This field involves measuring CCN concentrations, characterizing their chemical composition and size, and relating aerosol properties to cloud microphysical processes. |
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