{
    "created": "2016-09-28 10:56:52",
    "updated": "2026-05-08 15:02:16",
    "id": "ccca7daa-0d19-11e6-b319-5cc5d45ad3ae",
    "version": 3,
    "ds_topic": null,
    "title_cn": "1985-1999年乌鲁木齐河源1号冰川运动速度",
    "title_en": "Velocity of glacier movement at Urumqi River Source No. 1, 1985-1999",
    "ds_abstract": "<p>&emsp;&emsp;本数据集为天山乌鲁木齐河源1号冰川1985-1999年冰川运动速度。1号冰川表面运动速度是用精密光学经纬仪及全站仪进行测量的，前者，从冰川上的控制点对布设在冰内的花杆进行重复前方交会，以坐标法计算，求出花杆（冰体）在单位时间内的空间位移而得到的。每年消融开始5月和消融结束的8月底各观测一次，这样便可得到消融期及全年的流速资料。后者，对冰川表面运动速度的观测是使用全站仪进行测量的，从控制点K1、K2上对布设在冰川表面的测杆进行观测的，以座标法计算出冰体单位时间内的空间位移。该数据集主要是记录了冰川运动速度（夏季、冬季和年运动速度）。</p>",
    "ds_source": "<p>&emsp;&emsp;冰川运动速度，单位时间内冰川移动的距离。由于冰川运动速度很慢、单位常以厘米/昼夜或公里/年计。通过野外测量或用一些经验公式计算。</p>",
    "ds_process_way": "<p>&emsp;&emsp;以坐标法计算出冰体单位时间内的空间位移。</p>",
    "ds_quality": "<p>&emsp;&emsp;数据质量良好。</p>",
    "ds_acq_start_time": "1988-06-04 00:00:00",
    "ds_acq_end_time": "1996-09-05 00:00:00",
    "ds_acq_place": "天山冰川站",
    "ds_acq_lon_east": 86.80888888888889,
    "ds_acq_lat_south": 43.11083333333333,
    "ds_acq_lon_west": 86.80583333333333,
    "ds_acq_lat_north": 43.11944444444445,
    "ds_acq_alt_low": 3700.0,
    "ds_acq_alt_high": 4200.0,
    "ds_share_type": "login-access",
    "ds_total_size": 136175,
    "ds_files_count": 2,
    "ds_format": "csv",
    "ds_space_res": null,
    "ds_time_res": "日",
    "ds_coordinate": "WGS84",
    "ds_projection": "",
    "ds_thumbnail": "ccca7daa-0d19-11e6-b319-5cc5d45ad3ae.jpg",
    "ds_thumb_from": 2,
    "ds_ref_way": "",
    "paper_ref_way": "",
    "ds_ref_instruction": "",
    "ds_from_station": "天山冰川观测试验站",
    "organization_id": "a626f549-a49c-4431-8c3f-70cfdfd4784f",
    "ds_serv_man": "王飞腾",
    "ds_serv_phone": "0931-4967383",
    "ds_serv_mail": "wangfeiteng@lzb.ac.cn",
    "doi_value": "",
    "subject_codes": [
        "170.4510"
    ],
    "quality_level": 3,
    "publish_time": "2020-12-23 10:46:49",
    "last_updated": "2025-04-23 11:40:30",
    "protected": false,
    "protected_to": null,
    "lang": "zh",
    "cstr": "11738.11.ncdc.Tianshan.2020.61",
    "i18n": {
        "en": {
            "title": "Velocity of glacier movement at Urumqi River Source No. 1, 1985-1999",
            "ds_format": "csv",
            "ds_source": "<p>&emsp;Velocity of glacier movement, the distance traveled by a glacier per unit of time. Because glaciers move very slowly, the unit is often measured in centimeters per day and night or kilometers per year. It is calculated by field measurements or by some empirical formulas.</p>",
            "ds_quality": "<p>&emsp;Data quality is good.</p>",
            "ds_ref_way": "",
            "ds_abstract": "<p> This dataset is the glacier movement velocity of glacier No.1 in Urumqi River source, Tianshan Mountain, 1985-1999.The surface movement velocity of glacier No.1 is measured by precision optical latitude and longitude instrument and total station, the former, from the control point on the glacier to the flower pole laid inside the ice to repeat the forward rendezvous, to calculate by the coordinate method, and to find out the spatial displacement of the flower pole (the body of the ice) in a unit of time and obtain it. Observations are made once a year in May at the beginning of the ablation and once a year at the end of August at the end of the ablation, so that flow velocity information can be obtained for the ablation period and for the whole year. In the latter case, the observation of the speed of movement on the glacier surface is measured using a total station, and the spatial displacement of the ice body per unit of time is calculated by the coordinate method from the control points K1 and K2 on the measuring rods laid on the glacier surface. This dataset is primarily a record of glacier movement velocities (summer, winter and annual velocities).</p>",
            "ds_time_res": "日",
            "ds_acq_place": "Tianshan Glacier Station",
            "ds_space_res": "",
            "ds_projection": "",
            "ds_process_way": "<p>&emsp;The spatial displacement of the ice body per unit time is calculated by the coordinate method.</p>",
            "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": [
        "运动速度",
        "消融",
        "积累",
        "冰川变化"
    ],
    "ds_subject_tags": [
        "自然地理学"
    ],
    "ds_class_tags": [],
    "ds_locus_tags": [
        "新疆",
        "天山站"
    ],
    "ds_time_tags": [
        1985,
        1986,
        1987,
        1988,
        1989,
        1990,
        1991,
        1992,
        1993,
        1994,
        1995,
        1996,
        1997,
        1998,
        1999
    ],
    "ds_contributors": [
        {
            "true_name": "李忠勤",
            "email": "lzq@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": "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"
        }
    ],
    "ds_meta_authors": [
        {
            "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"
        }
    ],
    "ds_managers": [
        {
            "true_name": "李忠勤",
            "email": "lzq@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"
}