{"id":"8b5495b9-7d52-41e8-ba62-8c06e7131950","title":"青藏高原降水稳定氧18同位素数据集（1991–2008）","title_en":"Data set of δ18O stable Isotopes in Precipitation from Tibetan Network for Isotopes(1991–2008)","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":"文件命名：数据以表格xlsx格式存储，文件名称：2011RG000380_TNIP data for the review paper publishing.xls\n数据读取方式：可用office、wps等办公软件打开读取","description":"降水中稳定的氧同位素比（δ18O）是全球大气过程的综合示踪剂。 自1990年代以来，一直致力于研究位于青藏高原TP上20多个站点的降水同位素组成，这些站点位于西风和季风之间的气团交汇处。\n 在本文中，我们建立了一个青藏高原月尺度降水δ18 O的数据库，并使用不同的模型来评估TP上降水δ18 O的气候控制。 降水δ18 O的时空格局及其与温度和降水的关系揭示了三个不同的域，分别与西风（北TP），印度季风（南TP）及其之间的过渡有关。","doi":"10.11888/Geogra.tpdc.270940","projection":"WGS84","language":"zh","share_type":"online","east":75.2666666666667,"west":97.3666666666667,"south":27.9833333333333,"north":37.7666666666667,"scale":null,"crs":null,"filesize":0.212,"share_policy":"a","ts_created":"2020-10-25T00:00:00+08:00","doi_type":"拥有自主知识产权","ts_updated":"2021-04-19T19:10:35.512437+08:00","time_description":"","datas_group":3,"time_description_en":"","data_format":null,"project":[11],"specials":[],"cite":null,"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":null,"temporal_resolution":"Monthly","spatial_resolution":"-","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[353,354,355],"subtopics":{"metadata":"8b5495b9-7d52-41e8-ba62-8c06e7131950","three_pole":null,"third_pole":null},"username":"赵爱斌","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":true,"hit_count":5284}