本数据集针对慕士塔格地区，主要包括慕士塔格地区克拉牙依拉克冰川，冰下地形数据集包括控制点的序号、经度、纬度、厚度。数据集包含87条记录，主要利用GPR探地雷达，在冰川表面选取适当位置的横截面，通过实测获取的该横截面位置冰川厚度数据。数据集只针对2008年当年冰川厚度，故不进行补充和完善，采用协议共享。数据集包含控制点的序号、经度（单位：度(°)）、纬度（单位：度(°)）、高程（单位：米(m)，即当年冰川厚度）4个字段。数据集主要为当年实测资料，时间为2008年8月。空间基准为WGS84/EGM96，用探地雷达测量前，先进行雷达波速在冰川冰内传播速度的测量，并对探地雷达相关参数进行修改，确保获取对应冰川最精确的厚度数据。
", "ds_source": "本数据集主要为实测数据，数据主要来源为GPR探地雷达。
", "ds_process_way": "在数据实测中，利用GPR探地雷达，在冰川表面选取适当位置的横截面，通过实测，然后在软件中解算获取冰川厚度。
", "ds_quality": "用探地雷达测量前，先进行雷达波速在冰川冰内传播速度的测量，并对探地雷达相关参数进行修改，确保获取对应冰川最精确的厚度数据。
", "ds_acq_start_time": "2008-08-01 00:00:00", "ds_acq_end_time": "2008-08-31 00:00:00", "ds_acq_place": "慕士塔格", "ds_acq_lon_east": 75.26666666666667, "ds_acq_lat_south": 38.69, "ds_acq_lon_west": 75.24, "ds_acq_lat_north": 38.75, "ds_acq_alt_low": null, "ds_acq_alt_high": null, "ds_share_type": "apply-access", "ds_total_size": 18316, "ds_files_count": 3, "ds_format": "TXT", "ds_space_res": "", "ds_time_res": "", "ds_coordinate": "WGS84", "ds_projection": "", "ds_thumbnail": null, "ds_thumb_from": 2, "ds_ref_way": "2008年慕士塔格地区典型冰川冰下地形数据集来源于科技基础性工作专项“中国西部主要冰川作用中心冰量变化调查（2013FY111400）”。 引用方式建议采用如下方式：刘时银, 张震, 吴坤鹏， 等. 中科院寒区旱区环境与工程研究所. 2008年慕士塔格地区典型冰川冰下地形数据集. 2019。", "paper_ref_way": "", "ds_ref_instruction": "数据产权属于中科院寒区旱区环境与工程研究所。使用数据时需注明来源。", "ds_from_station": "中国西部主要冰川作用中心冰量变化调查", "organization_id": "75b2f6d5-c7ed-438c-b7be-98672c057ed5", "ds_serv_man": "李红星", "ds_serv_phone": "0931-4967592", "ds_serv_mail": "lihongxing@lzb.ac.cn", "doi_value": "", "subject_codes": null, "quality_level": 3, "publish_time": "2020-12-08 17:36:38", "last_updated": "2023-05-16 17:35:21", "protected": false, "protected_to": "2022-12-06 00:00:00", "lang": "zh", "cstr": "11738.11.ncdc.DIMaC.2020.141", "i18n": { "en": { "title": "Typical glacial subglacial topography dataset for the Mushtag region, 2008", "ds_format": "", "ds_source": "This data set is mainly measured data, and the main data source is GPR ground penetrating radar.
", "ds_quality": "Before using ground penetrating radar (GPR), the propagation velocity of radar wave velocity in glacier ice is measured, and the parameters of GPR are modified to ensure the most accurate thickness data of corresponding glacier.
", "ds_ref_way": "\nThe data set of typical glacier subglacial topography in mostag area in 2008 is derived from the \"survey of ice quantity change in major glaciation centers in Western China (2013fy111400)\". The following citation methods are recommended: Liu Shiyin, Zhang Zhen, Wu Kunpeng, etc.", "ds_abstract": "This data set is aimed at the Mostag area, mainly including the Krajayilak glacier in the MUZTAG area. The subglacial terrain data set includes the serial number, longitude, latitude and thickness of control points. The data set contains 87 records, mainly using GPR ground penetrating radar to select the appropriate cross-section on the surface of the glacier, and obtain the glacier thickness data of the cross-section position through the actual measurement. The data set is only for the glacier thickness in 2008, so it is not supplemented and improved, and the protocol is used for sharing. The data set contains four fields: serial number, longitude (unit: Degree (°)), latitude (unit: Degree (°)) and elevation (unit: meter (m), that is, glacier thickness of the current year). The data set is mainly the measured data in August 2008. The spatial datum is WGS84 / EGM96. Before using GPR, the propagation velocity of radar wave velocity in glacier ice is measured, and the relevant parameters of GPR are modified to ensure the most accurate thickness data of corresponding glacier.
", "ds_time_res": "", "ds_acq_place": "Mostag", "ds_space_res": "", "ds_projection": "", "ds_process_way": "In the data measurement, GPR ground penetrating radar is used to select the appropriate cross-section on the glacier surface, and then the glacier thickness is calculated in the software.
", "ds_ref_instruction": "Data are the property of the Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences. Use of data requires attribution." } }, "submit_center_id": "ncdc", "data_level": 0, "license_type": "CC BY 4.0", "doi_reg_from": "reg_local", "cstr_reg_from": "reg_local", "doi_not_reg_reason": null, "cstr_not_reg_reason": null, "is_paper_in_submitting": false, "ds_topic_tags": [ "冰厚", "GPR", "慕士塔格" ], "ds_subject_tags": [], "ds_class_tags": [], "ds_locus_tags": [ "慕士塔格" ], "ds_time_tags": [ 2008 ], "ds_contributors": [ { "true_name": "刘时银", "email": "liusy@lzb.ac.cn", "work_for": "云南大学国际河流与生态安全研究院", "country": "中国" }, { "true_name": "上官冬辉", "email": "dhguan@lzb.ac.cn", "work_for": "中国科学院西北生态环境资源研究院", "country": "" }, { "true_name": "蒋宗立", "email": "jiangzongli@lzb.ac.cn", "work_for": "中国科学院西北生态环境资源研究院", "country": "中国" }, { "true_name": "张盈松", "email": "", "work_for": "中国科学院西北生态环境资源研究院", "country": "" } ], "ds_meta_authors": [ { "true_name": "吴坤鹏", "email": "wukunpeng2008@lzb.ac.cn", "work_for": "云南大学国际河流与生态安全研究院", "country": "中国" } ], "ds_managers": [ { "true_name": "吴坤鹏", "email": "wukunpeng2008@lzb.ac.cn", "work_for": "云南大学国际河流与生态安全研究院", "country": "中国" }, { "true_name": "刘时银", "email": "liusy@lzb.ac.cn", "work_for": "云南大学国际河流与生态安全研究院", "country": "中国" } ], "category": "冰川" }