{"id":"02f66bb6-21ba-4ce9-b343-4e7c6ae2889a","title":"青藏高原及东中亚地区典型湖泊区域全新世有效水分连续模拟结果","title_en":"Continuous simulation of Holocene effective moisture change in typical lake regions of the Tibetan Plateau and East and Central Asia","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":"该数据集为.xls格式，可以直接使用Excel、WPS等程序直接打开。","description":"流域内的水量平衡可以通过单个湖泊的水位波动体现，而区域湖泊水位的一致性波动则可以反映区域有效水分的变化。以往的研究主要通过分析湖泊沉积物的多代用指标来重建过去的有效水分，缺少对区域有效水分变化的定量研究。青藏高原及东中亚地区典型湖泊区域全新世有效水分连续模拟结果数据集是基于湖泊能量平衡模型、湖泊水量平衡模型及瞬态气候演变模型，以构建的虚拟湖泊为载体，连续且定量地展示了青藏高原青海湖、沉错、班公错等以及东中亚地区青土湖、呼伦湖、岱海等湖泊区域全新世有效水分变化。模拟结果为探究千年尺度上湖泊演化过程提供了新的视角。","doi":"10.11888/Paleoenv.tpdc.272189","projection":"","language":"zh","share_type":"online","east":135.0,"west":60.0,"south":15.0,"north":60.0,"scale":null,"crs":null,"filesize":0.0195,"share_policy":"a","ts_created":"2022-02-22T16:59:28.455853+08:00","doi_type":"拥有自主知识产权","ts_updated":"2022-02-22T18:31:52.625358+08:00","time_description":"全新世以来","datas_group":3,"time_description_en":"","data_format":null,"project":[11],"specials":[],"cite":null,"review_status":5,"review_invite":[{"user_name":"昝金波","username":"昝金波","email":"zanjb@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":"10 year < x < 100 year","spatial_resolution":"--","license":"Attribution-NonCommercial-ShareAlike 4.0 International (CC BY-NC-SA 4.0)","fund":[21,461],"subtopics":{"metadata":"02f66bb6-21ba-4ce9-b343-4e7c6ae2889a","three_pole":null,"third_pole":null},"username":"陈嵘","review_time":null,"protected_duration":null,"protected_describe":null,"is_important":false,"hit_count":28}