{"id":"32542ad9-298c-4f97-8a4b-f292a5c2b312","title":"青藏高原冰川末端自动气象站数据（2019-2020）","title_en":"Data from automatic weather station at the end of glacier in Qinghai-Tibet Plateau (2019-2020)","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":"气象数据以excel格式存储，文件的名称为“xxx_yyyy.excel”，其中xxx代表冰川名称，yyyy代表年份，比如24K_2020.excel就描述2020年24K冰川区的气象数据。","description":"冰川表面微气象是观测冰川表面一定高度处风向风速、气温、湿度、气压、四分量辐射、冰温及降水等气象要素。冰川表面微气象监测是进行冰川监测的重要内容之一，是开展冰川表面能量-物质平衡、冰川运动、冰川融水径流、冰芯等研究及相关模型模拟研究的重要基础数据，为探究气候变化与冰川变化之间的相互关系奠定基础。主要通过在冰川表面架设高山气象站进行自动监测，也可使用便携式气象站进行短期的流动监测。近年来，在天山、西昆仑、祁连山、羌塘内陆、唐古拉山、念青唐古拉、藏东南、横断山和喜马拉雅山地区20多条冰川表面开展了相关的气象监测研究。该数据集为冰川区及冰川末端月值气象数据。","doi":"10.11888/Meteoro.tpdc.271394","projection":"","language":"zh","share_type":"offline","east":-2.0,"west":-1.0,"south":-1.0,"north":-1.0,"scale":null,"crs":null,"filesize":10.0,"share_policy":"c","ts_created":"2021-06-04T09:13:02.419257+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-06-10T12:07:09.516055+08:00","time_description":"","datas_group":0,"time_description_en":"","data_format":null,"project":[11],"specials":["b6500306-f60b-4aa1-b0b6-0324d94866df"],"cite":null,"review_status":5,"review_invite":[{"user_name":"陈莹莹","username":"陈莹莹","email":"chenyy@itpcas.ac.cn","is_cancel_expert":false}],"review_editor":{"id":66424,"last_login":"2021-08-31T17:09:37.293773+08:00","username":"YanHou","email":"ljz2hy@163.com","is_active":false,"is_staff":false,"user_name":"侯燕"},"data_sources":null,"temporal_resolution":"Monthly","spatial_resolution":"<= 1 m","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[21],"subtopics":{"metadata":"32542ad9-298c-4f97-8a4b-f292a5c2b312","three_pole":null,"third_pole":null},"username":"杨威","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":1160}