{"id":"a4a8a248-c2f8-48dd-92fa-a59dd43c15f5","title":"喜马拉雅山中部佩枯错湖水温度，水文气象和湖面蒸发（2015-2018）","title_en":"Lake water temperature, hydrometeorology and lake evaporation at Paiku Co in the central Himalayas (2015-2018)","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":"数据格式为excel\n南部湖中心42米深度处湖水温度文件名：water temperature profile-40m\n北部湖中心72米深度处湖水温度文件名：water temperature profile-70m\n湖面蒸发文件名：lake hydrometeorology","description":"1）数据内容：2015年6月-2018年5月高原南部佩枯错不同深度湖水温度变化，大气温度和湿度变化，佩枯错湖面蒸发。\n2）数据来源：不同深度湖水温度观测点分别位于佩枯错南部和北部湖中心，南部湖中心水深42米，观测间距为5米，北部湖中心水深为72米，观测间距为10m。湖水温度观测使用HOBO温度计进行，观测步长为每小时。然后求取日平均值。湖面蒸发采用能量平衡法计算得出。\n3）湖水温度测量误差为0.2度。\n4）湖面蒸发对进一步计算湖泊水量平衡具有重要意义。","doi":"10.11888/Hydro.tpdc.270287","projection":"","language":"zh","share_type":"online","east":86.0,"west":85.0,"south":28.0,"north":29.0,"scale":null,"crs":null,"filesize":1.0,"share_policy":"a","ts_created":"2019-11-14T23:21:42.285827+08:00","doi_type":"","ts_updated":"2021-04-19T22:02:54.918312+08:00","time_description":"","datas_group":3,"time_description_en":"","data_format":null,"project":[11],"specials":[],"cite":null,"review_status":5,"review_invite":[{"user_name":"王磊","username":"wangshenglei98","email":"wanglei@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":"Daily","spatial_resolution":"100m - 1km","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[6,21],"subtopics":{"metadata":"a4a8a248-c2f8-48dd-92fa-a59dd43c15f5","three_pole":null,"third_pole":"XDA20060201"},"username":"类延斌","review_time":"2019-11-15T00:10:36.126097+08:00","protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":2571}