{"title":"随机天气模型:加纳博诺地区案例","authors":"Bernard Gyamfi","doi":"arxiv-2409.06731","DOIUrl":null,"url":null,"abstract":"The paper sought to fit an Ornstein Uhlenbeck model with seasonal mean and\nvolatility, where the residuals are generated by a Brownian motion for Ghanian\ndaily average temperature. This paper employed the modified Ornstein Uhlenbeck\nmodel proposed by Bhowan which has a seasonal mean and stochastic volatility\nprocess. The findings revealed that, the Bono region experiences warm\ntemperatures and maximum precipitation up to 32.67 degree celsius and 126.51mm\nrespectively. It was observed that the Daily Average Temperature (DAT) of the\nregion reverts to a temperature of approximately 26 degree celsius at a rate of\n18.72% with maximum and minimum temperatures of 32.67degree celsius and\n19.75degree celsius respectively. Although the region is in the middle belt of\nGhana, it still experiences warm(hot) temperatures daily and experiences dry\nseasons relatively more than wet seasons in the number of years considered for\nour analysis. Our model explained approximately 50% of the variations in the\ndaily average temperature of the region which can be regarded as relatively a\ngood model. The findings of this paper are relevant in the pricing of weather\nderivatives with temperature as an underlying variable in the Ghanaian\nfinancial and agricultural sector. Furthermore, it would assist in the\ndevelopment and design of tailored agriculture/crop insurance models which\nwould incorporate temperature dynamics rather than extreme weather\nconditions/events such as floods, drought and wildfires.","PeriodicalId":501172,"journal":{"name":"arXiv - STAT - Applications","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2024-09-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"A Stochastic Weather Model: A Case of Bono Region of Ghana\",\"authors\":\"Bernard Gyamfi\",\"doi\":\"arxiv-2409.06731\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The paper sought to fit an Ornstein Uhlenbeck model with seasonal mean and\\nvolatility, where the residuals are generated by a Brownian motion for Ghanian\\ndaily average temperature. This paper employed the modified Ornstein Uhlenbeck\\nmodel proposed by Bhowan which has a seasonal mean and stochastic volatility\\nprocess. The findings revealed that, the Bono region experiences warm\\ntemperatures and maximum precipitation up to 32.67 degree celsius and 126.51mm\\nrespectively. It was observed that the Daily Average Temperature (DAT) of the\\nregion reverts to a temperature of approximately 26 degree celsius at a rate of\\n18.72% with maximum and minimum temperatures of 32.67degree celsius and\\n19.75degree celsius respectively. Although the region is in the middle belt of\\nGhana, it still experiences warm(hot) temperatures daily and experiences dry\\nseasons relatively more than wet seasons in the number of years considered for\\nour analysis. Our model explained approximately 50% of the variations in the\\ndaily average temperature of the region which can be regarded as relatively a\\ngood model. The findings of this paper are relevant in the pricing of weather\\nderivatives with temperature as an underlying variable in the Ghanaian\\nfinancial and agricultural sector. Furthermore, it would assist in the\\ndevelopment and design of tailored agriculture/crop insurance models which\\nwould incorporate temperature dynamics rather than extreme weather\\nconditions/events such as floods, drought and wildfires.\",\"PeriodicalId\":501172,\"journal\":{\"name\":\"arXiv - STAT - Applications\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2024-09-04\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"arXiv - STAT - Applications\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/arxiv-2409.06731\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"arXiv - STAT - Applications","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/arxiv-2409.06731","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
A Stochastic Weather Model: A Case of Bono Region of Ghana
The paper sought to fit an Ornstein Uhlenbeck model with seasonal mean and
volatility, where the residuals are generated by a Brownian motion for Ghanian
daily average temperature. This paper employed the modified Ornstein Uhlenbeck
model proposed by Bhowan which has a seasonal mean and stochastic volatility
process. The findings revealed that, the Bono region experiences warm
temperatures and maximum precipitation up to 32.67 degree celsius and 126.51mm
respectively. It was observed that the Daily Average Temperature (DAT) of the
region reverts to a temperature of approximately 26 degree celsius at a rate of
18.72% with maximum and minimum temperatures of 32.67degree celsius and
19.75degree celsius respectively. Although the region is in the middle belt of
Ghana, it still experiences warm(hot) temperatures daily and experiences dry
seasons relatively more than wet seasons in the number of years considered for
our analysis. Our model explained approximately 50% of the variations in the
daily average temperature of the region which can be regarded as relatively a
good model. The findings of this paper are relevant in the pricing of weather
derivatives with temperature as an underlying variable in the Ghanaian
financial and agricultural sector. Furthermore, it would assist in the
development and design of tailored agriculture/crop insurance models which
would incorporate temperature dynamics rather than extreme weather
conditions/events such as floods, drought and wildfires.