Spatial and seasonal dynamics of soil loss ratio in mountain rangelands of south-western Kyrgyzstan
Vegetation cover is the main factor of soil loss prevention. The C-factor of the RUSLE (Revised Universal Soil Loss Equation) was predicted with NDVI, ground data and exponential regression equation for mountain rangelands of Kyrgyzstan. Time series of C-factor, precipitation and temperature were de...
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Veröffentlicht in: | Journal of mountain science 2016-02, Vol.13 (2), p.316-329 |
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description | Vegetation cover is the main factor of soil loss prevention. The C-factor of the RUSLE (Revised Universal Soil Loss Equation) was predicted with NDVI, ground data and exponential regression equation for mountain rangelands of Kyrgyzstan. Time series of C-factor, precipitation and temperature were decomposed into seasonal and trend components with STL (seasonal decomposition by loess) to assess their interrelations. C-factor, precipitation and temperature trend components indicated significant lagged correlation, whereas seasonal components indicated more complex relations with climate factors which can be promoting as well as limiting factors for vegetation development, depending on the season. Rainy springs and hot summers may increase soil loss dramatically, whereas warm and dry springs with rainy summers can decrease it. Steep slopes indicated higher soil loss ratio, whereas flat areas were better protected by vegetation. |
doi_str_mv | 10.1007/s11629-014-3393-6 |
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The C-factor of the RUSLE (Revised Universal Soil Loss Equation) was predicted with NDVI, ground data and exponential regression equation for mountain rangelands of Kyrgyzstan. Time series of C-factor, precipitation and temperature were decomposed into seasonal and trend components with STL (seasonal decomposition by loess) to assess their interrelations. C-factor, precipitation and temperature trend components indicated significant lagged correlation, whereas seasonal components indicated more complex relations with climate factors which can be promoting as well as limiting factors for vegetation development, depending on the season. Rainy springs and hot summers may increase soil loss dramatically, whereas warm and dry springs with rainy summers can decrease it. 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Mt. Sci</addtitle><addtitle>Journal of Mountain Science</addtitle><description>Vegetation cover is the main factor of soil loss prevention. The C-factor of the RUSLE (Revised Universal Soil Loss Equation) was predicted with NDVI, ground data and exponential regression equation for mountain rangelands of Kyrgyzstan. Time series of C-factor, precipitation and temperature were decomposed into seasonal and trend components with STL (seasonal decomposition by loess) to assess their interrelations. C-factor, precipitation and temperature trend components indicated significant lagged correlation, whereas seasonal components indicated more complex relations with climate factors which can be promoting as well as limiting factors for vegetation development, depending on the season. Rainy springs and hot summers may increase soil loss dramatically, whereas warm and dry springs with rainy summers can decrease it. Steep slopes indicated higher soil loss ratio, whereas flat areas were better protected by vegetation.</description><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Ecology</subject><subject>Environment</subject><subject>Geography</subject><subject>Mountains</subject><subject>Precipitation</subject><subject>Rangelands</subject><subject>Soil dynamics</subject><subject>Soils</subject><subject>Temperature</subject><subject>Vegetation</subject><subject>Vegetation cover</subject><subject>动态空间</subject><subject>吉尔吉斯斯坦</subject><subject>季节性</subject><subject>流失率</subject><subject>牧场</subject><subject>西南部</subject><subject>通用土壤流失方程</subject><subject>高山</subject><issn>1672-6316</issn><issn>1993-0321</issn><issn>1008-2786</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2016</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kU1LAzEQhhdRsH78AG9BL15WM8lusjlK8QsLHtRzSNNsu2WbtMkuUn-9s7SIePCUCTzvzDvvZNkF0BugVN4mAMFUTqHIOVc8FwfZCBQWlDM4xFpIlgsO4jg7SWlJqZCqglFm39ama0xLjJ-R5EwKHj-zrTerxiYSapJC05I2pEQikoE0nqxC7zuDRTR-7lqU7sm-W-SfLnUuevKyjfPtV-qMP8uOatMmd75_T7OPh_v38VM-eX18Ht9NclsUrMutrNxUFKUpuLFM2WLqaiZKqHhNK1EzykAKK2nJQChGS1kLbpVUvJqyGVSKn2bXu77rGDY92tCrJlnXokEX-qRBSl4xpUAievUHXYY-4uoDJQoqFRMDBTvKRtw_ulqvY7MycauB6iF2vYtdY-x6iF0L1LCdJiGL6cRfnf8RXe4HLYKfb1D3M0ngoaSs0M03xn-QFA</recordid><startdate>20160201</startdate><enddate>20160201</enddate><creator>Kulikov, Maksim</creator><creator>Schickhoff, Udo</creator><creator>Borchardt, Peter</creator><general>Science Press</general><general>Springer Nature B.V</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7ST</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2P</scope><scope>PCBAR</scope><scope>PHGZM</scope><scope>PHGZT</scope><scope>PKEHL</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>Q9U</scope><scope>SOI</scope></search><sort><creationdate>20160201</creationdate><title>Spatial and seasonal dynamics of soil loss ratio in mountain rangelands of south-western Kyrgyzstan</title><author>Kulikov, Maksim ; Schickhoff, Udo ; Borchardt, Peter</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c442t-c78eb645a43ac29c4bef265183f086f202176c70521692057f63c97938b2d1893</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2016</creationdate><topic>Earth and Environmental Science</topic><topic>Earth Sciences</topic><topic>Ecology</topic><topic>Environment</topic><topic>Geography</topic><topic>Mountains</topic><topic>Precipitation</topic><topic>Rangelands</topic><topic>Soil dynamics</topic><topic>Soils</topic><topic>Temperature</topic><topic>Vegetation</topic><topic>Vegetation cover</topic><topic>动态空间</topic><topic>吉尔吉斯斯坦</topic><topic>季节性</topic><topic>流失率</topic><topic>牧场</topic><topic>西南部</topic><topic>通用土壤流失方程</topic><topic>高山</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Kulikov, Maksim</creatorcontrib><creatorcontrib>Schickhoff, Udo</creatorcontrib><creatorcontrib>Borchardt, Peter</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Environment Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Science Database (Alumni Edition)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Science Database</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>ProQuest Central (New)</collection><collection>ProQuest One Academic (New)</collection><collection>ProQuest One Academic Middle East (New)</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central Basic</collection><collection>Environment Abstracts</collection><jtitle>Journal of mountain science</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Kulikov, Maksim</au><au>Schickhoff, Udo</au><au>Borchardt, Peter</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Spatial and seasonal dynamics of soil loss ratio in mountain rangelands of south-western Kyrgyzstan</atitle><jtitle>Journal of mountain science</jtitle><stitle>J. Mt. Sci</stitle><addtitle>Journal of Mountain Science</addtitle><date>2016-02-01</date><risdate>2016</risdate><volume>13</volume><issue>2</issue><spage>316</spage><epage>329</epage><pages>316-329</pages><issn>1672-6316</issn><eissn>1993-0321</eissn><eissn>1008-2786</eissn><abstract>Vegetation cover is the main factor of soil loss prevention. The C-factor of the RUSLE (Revised Universal Soil Loss Equation) was predicted with NDVI, ground data and exponential regression equation for mountain rangelands of Kyrgyzstan. Time series of C-factor, precipitation and temperature were decomposed into seasonal and trend components with STL (seasonal decomposition by loess) to assess their interrelations. C-factor, precipitation and temperature trend components indicated significant lagged correlation, whereas seasonal components indicated more complex relations with climate factors which can be promoting as well as limiting factors for vegetation development, depending on the season. Rainy springs and hot summers may increase soil loss dramatically, whereas warm and dry springs with rainy summers can decrease it. Steep slopes indicated higher soil loss ratio, whereas flat areas were better protected by vegetation.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s11629-014-3393-6</doi><tpages>14</tpages></addata></record> |
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subjects | Earth and Environmental Science Earth Sciences Ecology Environment Geography Mountains Precipitation Rangelands Soil dynamics Soils Temperature Vegetation Vegetation cover 动态空间 吉尔吉斯斯坦 季节性 流失率 牧场 西南部 通用土壤流失方程 高山 |
title | Spatial and seasonal dynamics of soil loss ratio in mountain rangelands of south-western Kyrgyzstan |
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