本数据集为2010年天山奎屯河51号冰川厚度测量结果，给出了相应海拔带的面积、平均厚度、平均坡度及其最大厚度。", "ds_source": "
自主产生。", "ds_process_way": "
探地雷达观测：围绕冰川物质平衡观测阵网，采用PulseEKKO PRO 型探地雷达围绕花杆点布设横、纵剖面开展观测，使用剖面法，以探地雷达的发射天线和接收天线用固定的间距（天线距）沿测线同步移动完成冰川厚度的探测。", "ds_quality": "
严格按照世界冰川监测中心（WGMS）和国内相关冰川学观测调查方法、规范执行。", "ds_acq_start_time": "2010-08-01 00:00:00", "ds_acq_end_time": "2010-08-01 00:00:00", "ds_acq_place": "天山奎屯河51号冰川", "ds_acq_lon_east": 84.5, "ds_acq_lat_south": 43.1, "ds_acq_lon_west": 84.0, "ds_acq_lat_north": 43.5, "ds_acq_alt_low": 3400.0, "ds_acq_alt_high": 4000.0, "ds_share_type": "apply-access", "ds_total_size": 9621, "ds_files_count": 2, "ds_format": "excle", "ds_space_res": "", "ds_time_res": "", "ds_coordinate": "WGS84", "ds_projection": "UTM", "ds_thumbnail": "098be93e-563c-4f96-94d9-4d4e1b5d4ae6.png", "ds_thumb_from": 2, "ds_ref_way": "", "paper_ref_way": "", "ds_ref_instruction": "", "ds_from_station": null, "organization_id": "76330c66-832b-46b3-b501-f5f6edb08dc2", "ds_serv_man": "敏玉芳", "ds_serv_phone": "0931-4967596", "ds_serv_mail": "ncdc@lzb.ac.cn", "doi_value": "", "subject_codes": [ "170" ], "quality_level": 3, "publish_time": "2026-02-05 15:43:02", "last_updated": "2026-02-05 15:43:02", "protected": false, "protected_to": null, "lang": "zh", "cstr": "11738.11.NCDC.TIANSHAN.DB7122.2026", "i18n": { "en": { "title": "Glacier thickness in different altitude zones of Kuitun River No. 51 in Tianshan Mountains (2010)", "ds_format": "excle", "ds_source": "
Independently generated.", "ds_quality": "
Strictly follow the World Glacier Monitoring Center (WGMS) and relevant domestic glacier observation and survey methods and standards.", "ds_ref_way": "", "ds_abstract": "
This dataset presents the measurement results of the thickness of Glacier No. 51 on Kuitun River in Tianshan Mountains in 2010, including the area, average thickness, average slope, and maximum thickness of the corresponding altitude zones.", "ds_time_res": "", "ds_acq_place": "No. 51 Glacier of Kuitun River in Tianshan Mountains", "ds_space_res": "", "ds_projection": "", "ds_process_way": "
Ground penetrating radar observation: Around the glacier material balance observation array network, PulseEKKO PRO type ground penetrating radar is used to set up horizontal and vertical profiles around the flower pole point for observation. The profile method is used to detect the thickness of the glacier by synchronously moving the transmitting antenna and receiving antenna of the ground penetrating radar along the measurement line with a fixed spacing (antenna distance).", "ds_ref_instruction": "" } }, "submit_center_id": "ncdc", "data_level": 0, "license_type": "https://creativecommons.org/licenses/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": [ "冰川", "厚度", "51号冰川" ], "ds_subject_tags": [ "地球科学" ], "ds_class_tags": [], "ds_locus_tags": [ "山、奎屯河51号冰川" ], "ds_time_tags": [ 2010 ], "ds_contributors": [ { "true_name": "李忠勤", "email": "lizq@lzb.ac.cn", "work_for": "中国科学院西北生态环境资源研究院", "country": "中国" } ], "ds_meta_authors": [ { "true_name": "岳晓英", "email": "yuexiaoying@lzb.ac.cn", "work_for": "中国科学院西北生态环境资源研究院", "country": "中国" } ], "ds_managers": [ { "true_name": "王飞腾", "email": "wangfeiteng@lzb.ac.cn", "work_for": "中国科学院西北生态环境资源研究院", "country": "中国" } ], "category": "冰川" }