{"title":"斯匹次卑尔根群岛西部伞形植物的温度状况","authors":"T. I. Litvinova, G. Kashulina","doi":"10.37614/2307-5252.2021.6.12.9.042","DOIUrl":null,"url":null,"abstract":"The air and profile of Umbrisols in the south-western part of Svalbard are characterized by negative average annual temperatures. The duration of the period with positive temperatures at the depth of the umbric horizon (8–10 cm) is 128 days; the sum of positive temperatures is about 500 оС. The distribution of average monthly temperatures in all horizons in the profile of 0–60 cm in the annual cycle reliably correlates with air temperature.","PeriodicalId":438304,"journal":{"name":"Transaction Kola Science Centre","volume":"62 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-12-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Temperature regime of umbrisols, Western Spitsbergen\",\"authors\":\"T. I. Litvinova, G. Kashulina\",\"doi\":\"10.37614/2307-5252.2021.6.12.9.042\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The air and profile of Umbrisols in the south-western part of Svalbard are characterized by negative average annual temperatures. The duration of the period with positive temperatures at the depth of the umbric horizon (8–10 cm) is 128 days; the sum of positive temperatures is about 500 оС. The distribution of average monthly temperatures in all horizons in the profile of 0–60 cm in the annual cycle reliably correlates with air temperature.\",\"PeriodicalId\":438304,\"journal\":{\"name\":\"Transaction Kola Science Centre\",\"volume\":\"62 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2021-12-31\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Transaction Kola Science Centre\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.37614/2307-5252.2021.6.12.9.042\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Transaction Kola Science Centre","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.37614/2307-5252.2021.6.12.9.042","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
Temperature regime of umbrisols, Western Spitsbergen
The air and profile of Umbrisols in the south-western part of Svalbard are characterized by negative average annual temperatures. The duration of the period with positive temperatures at the depth of the umbric horizon (8–10 cm) is 128 days; the sum of positive temperatures is about 500 оС. The distribution of average monthly temperatures in all horizons in the profile of 0–60 cm in the annual cycle reliably correlates with air temperature.
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