Please use this identifier to cite or link to this item: http://hdl.handle.net/10397/82143
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dc.contributorDepartment of Land Surveying and Geo-Informatics-
dc.creatorDai, X-
dc.creatorYang, X-
dc.creatorWang, M-
dc.creatorGao, Y-
dc.creatorLiu, S-
dc.creatorZhang, J-
dc.date.accessioned2020-05-05T05:58:50Z-
dc.date.available2020-05-05T05:58:50Z-
dc.identifier.issn2073-4441-
dc.identifier.urihttp://hdl.handle.net/10397/82143-
dc.language.isoenen_US
dc.publisherMolecular Diversity Preservation International (MDPI)en_US
dc.rights© 2019 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).en_US
dc.rightsThe following publication Dai X, Yang X, Wang M, Gao Y, Liu S, Zhang J. The Dynamic Change of Bosten Lake Area in Response to Climate in the Past 30 Years. Water. 2020; 12(1):4, is available at https://doi.org/10.3390/w12010004en_US
dc.subjectArea changeen_US
dc.subjectBosten lakeen_US
dc.subjectClimate responseen_US
dc.subjectWater body information extractionen_US
dc.titleThe dynamic change of bosten lake area in response to climate in the past 30 yearsen_US
dc.typeJournal/Magazine Articleen_US
dc.identifier.volume12-
dc.identifier.issue1-
dc.identifier.doi10.3390/w12010004-
dcterms.abstractThe widely distributed lakes, as one of the major components of the inland water system, are the primary available freshwater resources on the earth and are sensitive to accelerated climate change and extensive human activities. Lakes play an important role in the terrestrial water cycle and biogeochemical cycle and substantially influence the health of humans living in the surrounding areas. Given the importance of lakes in the ecosystem, long-term monitoring of dynamic changes has important theoretical and practical significance. Here, we extracted water body information and monitored the long-term dynamics of Bosten Lake, which is the largest inland lake in China. We quantified the meteorological factors of the study area from the observation data of meteorological stations between 1988 and 2018. The characteristics of climate change and its correlation with the change of area in the Bosten Lake Basin in the past 30 years were analyzed. The major contributions of this study are as follows: (1) The initial water body was segmented based on the water index model Normalized DifferenceWater Index (NDWI) and Modified Normalized DifferenceWater Index (MNDWI) with a pre-assigned threshold value. The results were evaluated with the area extracted through artificial visual interpretation. Then we conducted mathematical morphology operators, opening and closing operations, and median filter to eliminate noise to ensure the accuracy of water body information extraction from the Bosten Lake. A long-term water surface area database of the Bosten Lake was established from high-resolution remote sensing images during 1988-2018. (2) Due to the seasonal difference of snow, ice content, and other objects on images, the areadynamics of Bosten Lake in the recent 30 years were analyzed separately in dry season and rainy season. The water surface area of Bosten Lake showed large inter-annual variations between 1988-2018. (3) Based on the assumption that climatic change has more direct effects on lake than human activities, six meteorological factors were selected to analyze the impacts of climate change on the annual mean lake surface area. The result indicated that in the past 30 years, climate conditions in the Bosten Lake Basin fluctuated greatly. We conducted correlations analysis between the areal dynamics of the Bosten Lake and the meteorological factors. Here, the annual average evaporation had the highest correlation with the areal dynamics of Bosten Lake followed by air temperature, precipitation, sunshine hours, and relative humidity, while the annual average wind speed had the weakest correlation.-
dcterms.accessRightsopen accessen_US
dcterms.bibliographicCitationWater, 2020, v. 12, no. 1, 4-
dcterms.isPartOfWater-
dcterms.issued2020-
dc.identifier.isiWOS:000519847200004-
dc.identifier.scopus2-s2.0-85079492583-
dc.identifier.artn4-
dc.description.validate202006 bcma-
dc.description.oaVersion of Recorden_US
dc.identifier.FolderNumberOA_Scopus/WOSen_US
dc.description.pubStatusPublisheden_US
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