পদ্ধতির তুলনা করুন
নির্বাচিত পদ্ধতিগুলো পাশাপাশি পর্যালোচনা করুন; যে সারিগুলোয় পার্থক্য আছে সেগুলো চিহ্নিত করা হয়।
| ভূ-ঘূর্ণি বায়ু× | WRF মডেল× | |
|---|---|---|
| ক্ষেত্র | আবহবিজ্ঞান | আবহবিজ্ঞান |
| পরিবার | Process / pipeline | Process / pipeline |
| উদ্ভবের বছর≠ | 1857 | 2000 |
| প্রবর্তক≠ | Buys Ballot, Coriolis | Skamarock and Klemp |
| ধরন≠ | Wind balance principle | Atmospheric simulation system |
| মৌলিক উৎস≠ | Holton, J. R. (2004). An Introduction to Dynamic Meteorology (4th ed.). Academic Press. link ↗ | 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. link ↗ |
| অপর নাম≠ | Geostrophic wind, Geostrophic balance, Geostrophic approximation | Weather Research and Forecasting, WRF, ARW, NMM |
| সম্পর্কিত≠ | 3 | 4 |
| সারসংক্ষেপ≠ | Geostrophic wind balance is a fundamental concept in meteorology that describes the balance between the pressure gradient force and the Coriolis force in large-scale atmospheric flow. When this balance is achieved, wind blows parallel to isobars without acceleration—a condition observed in the free atmosphere away from the equator and surface boundary layer. | 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. |
| ScholarGateডেটাসেট ↗ |
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