{"title":"维斯瓦河河口和格但斯克湾的热量机制","authors":"R. Graf, V. Vyshnevskyi","doi":"10.7163/gpol.0264","DOIUrl":null,"url":null,"abstract":"Surface water temperature characteristics of the Vistula River mouth and the Gdańsk Bay were determined on the basis of available observations, remote sensing and hydrodynamic models. The water temperature in the Vistula River and the Gdańsk Bay was found to be much higher than the air temperature. In recent decades, the water temperature in the Vistula River mouth and the Gdańsk Bay has increased significantly. It hasbeen determined that water temperature in the bay is affected not only by air temperature, but also by water discharge of the Vistula River and wind.","PeriodicalId":46250,"journal":{"name":"Geographia Polonica","volume":null,"pages":null},"PeriodicalIF":1.1000,"publicationDate":"2024-01-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Thermal regime of the Vistula River mouth and the Gdańsk Bay\",\"authors\":\"R. Graf, V. Vyshnevskyi\",\"doi\":\"10.7163/gpol.0264\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Surface water temperature characteristics of the Vistula River mouth and the Gdańsk Bay were determined on the basis of available observations, remote sensing and hydrodynamic models. The water temperature in the Vistula River and the Gdańsk Bay was found to be much higher than the air temperature. In recent decades, the water temperature in the Vistula River mouth and the Gdańsk Bay has increased significantly. It hasbeen determined that water temperature in the bay is affected not only by air temperature, but also by water discharge of the Vistula River and wind.\",\"PeriodicalId\":46250,\"journal\":{\"name\":\"Geographia Polonica\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":1.1000,\"publicationDate\":\"2024-01-12\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geographia Polonica\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.7163/gpol.0264\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOGRAPHY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geographia Polonica","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.7163/gpol.0264","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOGRAPHY","Score":null,"Total":0}
Thermal regime of the Vistula River mouth and the Gdańsk Bay
Surface water temperature characteristics of the Vistula River mouth and the Gdańsk Bay were determined on the basis of available observations, remote sensing and hydrodynamic models. The water temperature in the Vistula River and the Gdańsk Bay was found to be much higher than the air temperature. In recent decades, the water temperature in the Vistula River mouth and the Gdańsk Bay has increased significantly. It hasbeen determined that water temperature in the bay is affected not only by air temperature, but also by water discharge of the Vistula River and wind.