D. Kaverin, G. Malkova, D. Zamolodchikov, N. Shiklomanov, A. Pastukhov, A. Novakovskiy, M. Sadurtdinov, Andry Skvortsov, Andry Tsarev, A. Pochikalov, Sergei Malitsky, G. Kraev
{"title":"俄罗斯欧洲北部CALM站点的长期有源层监测","authors":"D. Kaverin, G. Malkova, D. Zamolodchikov, N. Shiklomanov, A. Pastukhov, A. Novakovskiy, M. Sadurtdinov, Andry Skvortsov, Andry Tsarev, A. Pochikalov, Sergei Malitsky, G. Kraev","doi":"10.1080/1088937X.2021.1981476","DOIUrl":null,"url":null,"abstract":"ABSTRACT This paper presents results from long-term active layer monitoring at four CALM sites in the Russian European North. Observational records range from 10 to 24 years in length (1996–2019). The impact of climatic and landscape parameters on active layer thickness has been assessed through linear regression. The temporal dynamics of climatic parameters, responsible for the thaw depth changes, were investigated. The long-term data indicate that the active-layer thickness has increased at all the monitoring sites, in response to changes in both summer and winter climatic parameters. The surface organic layer also serves as a major landscape factor influencing spatial patterns of thaw depth and climate-induced rates of permafrost thawing.","PeriodicalId":46164,"journal":{"name":"Polar Geography","volume":"13 1","pages":"203 - 216"},"PeriodicalIF":2.0000,"publicationDate":"2021-07-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"7","resultStr":"{\"title\":\"Long-term active layer monitoring at CALM sites in the Russian European North\",\"authors\":\"D. Kaverin, G. Malkova, D. Zamolodchikov, N. Shiklomanov, A. Pastukhov, A. Novakovskiy, M. Sadurtdinov, Andry Skvortsov, Andry Tsarev, A. Pochikalov, Sergei Malitsky, G. Kraev\",\"doi\":\"10.1080/1088937X.2021.1981476\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"ABSTRACT This paper presents results from long-term active layer monitoring at four CALM sites in the Russian European North. Observational records range from 10 to 24 years in length (1996–2019). The impact of climatic and landscape parameters on active layer thickness has been assessed through linear regression. The temporal dynamics of climatic parameters, responsible for the thaw depth changes, were investigated. The long-term data indicate that the active-layer thickness has increased at all the monitoring sites, in response to changes in both summer and winter climatic parameters. The surface organic layer also serves as a major landscape factor influencing spatial patterns of thaw depth and climate-induced rates of permafrost thawing.\",\"PeriodicalId\":46164,\"journal\":{\"name\":\"Polar Geography\",\"volume\":\"13 1\",\"pages\":\"203 - 216\"},\"PeriodicalIF\":2.0000,\"publicationDate\":\"2021-07-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"7\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Polar Geography\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.1080/1088937X.2021.1981476\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOGRAPHY, PHYSICAL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Polar Geography","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.1080/1088937X.2021.1981476","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
Long-term active layer monitoring at CALM sites in the Russian European North
ABSTRACT This paper presents results from long-term active layer monitoring at four CALM sites in the Russian European North. Observational records range from 10 to 24 years in length (1996–2019). The impact of climatic and landscape parameters on active layer thickness has been assessed through linear regression. The temporal dynamics of climatic parameters, responsible for the thaw depth changes, were investigated. The long-term data indicate that the active-layer thickness has increased at all the monitoring sites, in response to changes in both summer and winter climatic parameters. The surface organic layer also serves as a major landscape factor influencing spatial patterns of thaw depth and climate-induced rates of permafrost thawing.
期刊介绍:
Polar Geographyis a quarterly publication that offers a venue for scholarly research on the physical and human aspects of the Polar Regions. The journal seeks to address the component interplay of the natural systems, the complex historical, political, economic, cultural, diplomatic, and security issues, and the interchange amongst them. As such, the journal welcomes comparative approaches, critical scholarship, and alternative and disparate perspectives from around the globe. The journal offers scientists a venue for publishing longer papers such as might result from distillation of a thesis, or review papers that place in global context results from coordinated national and international efforts currently underway in both Polar Regions.