{"id":"cc9278ae-98bf-48eb-a24c-acb1220b5c3c","title":"基于卫星和台站的青藏高原大气热源数据集（1984-2015）","title_en":"The atmospheric heat source dataset of Tibetan Plateau based on satellites and stations (1984-2015)","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":"数据类型为NetCDF，采用**_NN_day.nc和**_NN_mon.nc的方式命名。**为LH，NR，SH，分别表示潜热，净辐射和感热通量，NN表示站点个数，day和mon分别表明逐日或逐月数据。","description":"青藏高原作为地球的第三极，春夏季作为热源对区域和全球的天气和气候有着重要的影响。为了探究高原多时间尺度热力强迫作用的时空变化特征，建立一套持续、可靠的长时间观测的观测数据为基础的高原热源（汇）数据是十分有必要的。利用中国气象局在青藏高原上80（32）个观测台站1979—2016（1960—2016）年的气象要素（地表温度、地表气温、10m 风速、 日累计降水量等）为基础计算得到感热（SH）和潜热（LH），同时利用卫星资料处理得到高原上1984—2015年的净辐射通量（RC），得到了一套通过质量控制的长期高原热源数据集。本数据集在计算地表感热通量时，考虑了总体热传输系数 的日变化特征。","doi":"10.11888/Meteoro.tpdc.270115","projection":null,"language":"zh","share_type":"online","east":110.0,"west":80.0,"south":25.0,"north":40.0,"scale":null,"crs":null,"filesize":12.5,"share_policy":"a","ts_created":"2019-06-17T10:25:21.126700+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-04-19T11:41:51.218301+08:00","time_description":"","datas_group":3,"time_description_en":"","data_format":null,"project":[10,11],"specials":["1832ecb3-70d0-4b5e-bdb5-2e9ff4ad1efe"],"cite":null,"review_status":5,"review_invite":[],"review_editor":{"id":21054,"last_login":"2022-04-10T10:49:12.540341+08:00","username":"tingting","email":"panxd@itpcas.ac.cn","is_active":true,"is_staff":true,"user_name":"潘小多"},"data_sources":"","temporal_resolution":"Daily","spatial_resolution":"","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[5],"subtopics":{"metadata":"cc9278ae-98bf-48eb-a24c-acb1220b5c3c","three_pole":null,"third_pole":null},"username":"胡文婷","review_time":"2019-06-17T10:50:49.136371+08:00","protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":2800}