Bryan Zhang, Dhruv Rao, Adam Yang, Lawrence Zhang, Rodz Andrie Amor
{"title":"Super Resolution On Global Weather Forecasts","authors":"Bryan Zhang, Dhruv Rao, Adam Yang, Lawrence Zhang, Rodz Andrie Amor","doi":"arxiv-2409.11502","DOIUrl":null,"url":null,"abstract":"Weather forecasting is a vitally important tool for tasks ranging from\nplanning day to day activities to disaster response planning. However, modeling\nweather has proven to be challenging task due to its chaotic and unpredictable\nnature. Each variable, from temperature to precipitation to wind, all influence\nthe path the environment will take. As a result, all models tend to rapidly\nlose accuracy as the temporal range of their forecasts increase. Classical\nforecasting methods use a myriad of physics-based, numerical, and stochastic\ntechniques to predict the change in weather variables over time. However, such\nforecasts often require a very large amount of data and are extremely\ncomputationally expensive. Furthermore, as climate and global weather patterns\nchange, classical models are substantially more difficult and time-consuming to\nupdate for changing environments. Fortunately, with recent advances in deep\nlearning and publicly available high quality weather datasets, deploying\nlearning methods for estimating these complex systems has become feasible. The\ncurrent state-of-the-art deep learning models have comparable accuracy to the\nindustry standard numerical models and are becoming more ubiquitous in practice\ndue to their adaptability. Our group seeks to improve upon existing deep\nlearning based forecasting methods by increasing spatial resolutions of global\nweather predictions. Specifically, we are interested in performing super\nresolution (SR) on GraphCast temperature predictions by increasing the global\nprecision from 1 degree of accuracy to 0.5 degrees, which is approximately\n111km and 55km respectively.","PeriodicalId":501166,"journal":{"name":"arXiv - PHYS - Atmospheric and Oceanic Physics","volume":"41 1","pages":""},"PeriodicalIF":0.0000,"publicationDate":"2024-09-17","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - PHYS - Atmospheric and Oceanic Physics","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2409.11502","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
Weather forecasting is a vitally important tool for tasks ranging from
planning day to day activities to disaster response planning. However, modeling
weather has proven to be challenging task due to its chaotic and unpredictable
nature. Each variable, from temperature to precipitation to wind, all influence
the path the environment will take. As a result, all models tend to rapidly
lose accuracy as the temporal range of their forecasts increase. Classical
forecasting methods use a myriad of physics-based, numerical, and stochastic
techniques to predict the change in weather variables over time. However, such
forecasts often require a very large amount of data and are extremely
computationally expensive. Furthermore, as climate and global weather patterns
change, classical models are substantially more difficult and time-consuming to
update for changing environments. Fortunately, with recent advances in deep
learning and publicly available high quality weather datasets, deploying
learning methods for estimating these complex systems has become feasible. The
current state-of-the-art deep learning models have comparable accuracy to the
industry standard numerical models and are becoming more ubiquitous in practice
due to their adaptability. Our group seeks to improve upon existing deep
learning based forecasting methods by increasing spatial resolutions of global
weather predictions. Specifically, we are interested in performing super
resolution (SR) on GraphCast temperature predictions by increasing the global
precision from 1 degree of accuracy to 0.5 degrees, which is approximately
111km and 55km respectively.