{"id":"e5229003-b32f-4580-b085-ee8c57509fde","title":"末次冰盛期以来亚洲高山区冰川分布数据","title_en":"Glacier distribution over the High-mountain Asia since the last glacial maximum","serial":"","user_limit":"为尊重知识产权、保障数据作者的权益、扩展数据中心的服务、评估数据的应用潜力，请数据使用者在使用数据所产生的研究成果中（包括公开发表的论文、论著、数据产品和未公开发表的研究报告、数据产品等成果），明确注明数据来源和数据作者。对于转载（二次或多次发布）的数据，作者还须注明原始数据来源。","instructions":"冰川面积数据以excel格式存储，其中时间yyyyy代表年前（相对1950）.\n冰川分布以netcdf文件存储，可以采用cdo或ncl专业气象数据处理或绘图软件打开查看和分析．","description":"本数据为末次冰盛期以来亚洲高山区冰川分布的模拟数据，其中包括典型区域（亚洲高山区、天山、喜马拉雅山、帕米尔高原）年分辨率的冰川面积变化序列以及典型时期（LGM（20000~19000ka），HS1（17000~16000ka），BA（~14900~14350ka），YD（12900~12000ka），EH（9500~8500ka），MH（6500~5500ka），LH（3500~2500ka）和Modern（1951~1990））1km分辨率的亚洲高山区冰川分布。该数据以基于CCSM3气候模式的TRACE全强迫模拟试验数据为外强迫场，驱动1km分辨率的PISM冰盖模式，从而获取末次盛冰期以来亚洲高山区冰川的可能分布。该数据可以用于研究末次冰盛期以来亚洲高山区冰川分布的变化及其对湖泊水位、径流、地貌等环境和气候要素的影响。","doi":"10.11888/Cryos.tpdc.271928","projection":"","language":"zh","share_type":"online","east":108.0,"west":67.0,"south":25.0,"north":45.0,"scale":null,"crs":null,"filesize":293.0,"share_policy":"a","ts_created":"2021-12-20T14:34:09.632770+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-12-20T16:31:13.219193+08:00","time_description":"过去2万年以来","datas_group":3,"time_description_en":"Over the past 20000 years","data_format":null,"project":[11],"specials":[],"cite":null,"review_status":5,"review_invite":[{"user_name":"梁丽乔","username":"丽乔","email":"liangliqiao@itpcas.ac.cn","is_cancel_expert":false}],"review_editor":{"id":42421,"last_login":"2022-04-08T15:16:51.670544+08:00","username":"任慧霞","email":"510727846@qq.com","is_active":true,"is_staff":true,"user_name":"任慧霞"},"data_sources":null,"temporal_resolution":"Yearly","spatial_resolution":"1km - 10km","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[21],"subtopics":{"metadata":"e5229003-b32f-4580-b085-ee8c57509fde","three_pole":null,"third_pole":null},"username":"王茉","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":285}