{"id":"578df7ea-1b2f-4e3e-b59a-74854a3c8b55","title":"高亚洲地区雪水当量数据集（2002-2011）","title_en":"Snow water equivalent dataset for the High Asia Region (2002-2011)","serial":"地球大数据科学工程专项时空三极环境项目","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":"","description":"雪水当量（积雪深度与密度之积）是反映地表积雪量变化的重要因子，是地表水文模型和气候模式中的一个重要参数。青藏高原作为亚洲水塔，多条大江大河补给主要依靠高原上冰川或积雪的融化。基于被动微波对积雪监测的敏感性，本数据实现了长时间序列的高亚洲地区雪水当量的反演。数据集包含日雪水当量、月雪水当量以及每五日雪水当量，可服务于当地水文、畜牧业生产等方面。","doi":"10.11922/sciencedb.660.","projection":"","language":"zh","share_type":"online","east":107.0,"west":67.0,"south":25.0,"north":45.0,"scale":null,"crs":"","filesize":3399.0,"share_policy":"a","ts_created":"2018-02-17T03:56:31+08:00","doi_type":"","ts_updated":"2021-04-19T11:18:40.942673+08:00","time_description":"2002-2011","datas_group":3,"time_description_en":"","data_format":"bin","project":[10,11],"specials":["1832ecb3-70d0-4b5e-bdb5-2e9ff4ad1efe","f2a78cde-1c98-4241-94dc-7532eba32b80"],"cite":"邱玉宝.  高亚洲地区雪水当量数据集. 时空三极环境大数据平台. 2018","review_status":5,"review_invite":[],"review_editor":{"id":21057,"last_login":"2022-04-02T11:43:37.753860+08:00","username":"gecm","email":"gechm@lzb.ac.cn","is_active":true,"is_staff":true,"user_name":"盖春梅"},"data_sources":"","temporal_resolution":"Yearly","spatial_resolution":"","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[5],"subtopics":{"metadata":"578df7ea-1b2f-4e3e-b59a-74854a3c8b55","three_pole":"XDA19070201","third_pole":null},"username":"邱玉宝","review_time":null,"protected_duration":6,"protected_describe":null,"is_important":false,"hit_count":4103}