{"type":"rich","version":"1.0","provider_name":"Transistor","provider_url":"https://transistor.fm","author_name":"Science Tech Brief By HackerNoon","title":"The Models We Used to Observed Interactions Between Near-Inertial Waves and Mesoscale Eddies","html":"<iframe width=\"100%\" height=\"180\" frameborder=\"no\" scrolling=\"no\" seamless src=\"https://share.transistor.fm/e/45ca15f0\"></iframe>","width":"100%","height":180,"duration":299,"description":"\n        This story was originally published on HackerNoon at: https://hackernoon.com/the-models-we-used-to-observed-interactions-between-near-inertial-waves-and-mesoscale-eddies.\n             The authors use the PM model and the YBJ model to simulate the wind stress.  \n            Check more stories related to science at: https://hackernoon.com/c/science.\n            You can also check exclusive content about #science, #oceanography, #studying-the-ocean, #near-inertial-waves, #near-inertial-waves-definition, #what-are-mesoscale-eddies, #the-ybj-model-explained, #what-is-the-ybj-model,  and more.\n            \n            \n            This story was written by: @oceanography. Learn more about this writer by checking @oceanography's about page,\n            and for more stories, please visit hackernoon.com.\n            \n                \n                \n                The authors use the PM model and the YBJ model to simulate the wind stress. They use a domain that is 400 km×400 km in the horizontal and 4 km deep. The stratification and the wind forcing are taken to be horizontally uniform, capturing the forcing at a scale much larger than the mesoscale.\n        \n        ","thumbnail_url":"https://img.transistorcdn.com/S66fL9skYMhlajDauLWqBH_bXds_u8JsPbvAZlh45OA/rs:fill:0:0:1/w:400/h:400/q:60/mb:500000/aHR0cHM6Ly9pbWct/dXBsb2FkLXByb2R1/Y3Rpb24udHJhbnNp/c3Rvci5mbS9zaG93/LzQxMjczLzE2ODM1/ODI0MjQtYXJ0d29y/ay5qcGc.webp","thumbnail_width":300,"thumbnail_height":300}