{"title":"Analysis of Year-to-Year and Seasonal Variability of Land Surface Albedo in the Russian Actinometric Network","authors":"O. M. Pokrovskiy, Ye. L. Makhotkina","doi":"10.2747/0749-3878.40.2.79","DOIUrl":null,"url":null,"abstract":"Data registered in the Russian actinometric network are used in analyzing time series of hourly albedo values for the period 1976-1995. The mean monthly midday albedos reveal a considerable year-to-year variability averaging 5-8%. The maximum variabilities are greater by a factor of two to three. Despite a definite diversity in behavior of albedo, most observation points exhibit stable trends in their long-term changes. During the cold season there is an albedo decrease, whereas in the warm season there is an albedo increase. The linear trends are about 0.5-1.0% per year. At individual stations during individual months during the cold season of the year there is a trend toward an albedo increase. Changes in the annual albedo variability are related to alternation of cold and warm winters.","PeriodicalId":405012,"journal":{"name":"Mapping Sciences and Remote Sensing","volume":"30 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2003-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Mapping Sciences and Remote Sensing","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2747/0749-3878.40.2.79","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
Data registered in the Russian actinometric network are used in analyzing time series of hourly albedo values for the period 1976-1995. The mean monthly midday albedos reveal a considerable year-to-year variability averaging 5-8%. The maximum variabilities are greater by a factor of two to three. Despite a definite diversity in behavior of albedo, most observation points exhibit stable trends in their long-term changes. During the cold season there is an albedo decrease, whereas in the warm season there is an albedo increase. The linear trends are about 0.5-1.0% per year. At individual stations during individual months during the cold season of the year there is a trend toward an albedo increase. Changes in the annual albedo variability are related to alternation of cold and warm winters.