{
    "created": "2019-04-09 08:59:10",
    "updated": "2026-05-08 15:52:13",
    "id": "ab749580-03ac-4df1-a816-665e58b90818",
    "version": null,
    "ds_topic": null,
    "title_cn": "2017-2018年乌鲁木齐河源1号冰川末端变化",
    "title_en": "Changes in the end of Glacier No.1 at the source of Urumqi River, 2017-2018",
    "ds_abstract": "<p>本数据集为2017-2018年乌鲁木齐河源1号冰川末端变化数据，包括东支和西支；单位：米；每年消融季末至次年消融季末，采用重复丈量法。1号冰川东、西支冰舌的年进退变化量；年度的各流速点的空间坐标，中国天山乌鲁木齐河源1号冰川物质平衡项目的观测研究始于1959年夏季，当时的1号冰川面积为1.95 km2，冰川长度为2.41 km，冰川末端最低为海拔3736 m，是乌鲁木齐河流域发育规模最大的双冰斗冰川形态的现代冰川。随着冰舌萎缩，1993年，1条冰川蜕变为两条完全独立的冰川体系，即1号冰川西支和1号冰川东支。由此也表明一个区域冰川退缩意味着该区域冰川数量可能是增加的，而冰川面积及其储量是递减的。",
    "ds_source": "<p>天山一号冰川属双支冰斗山谷冰川、长2.2公里、平均宽度500米、面积1.828平方公里、最大厚度140米、最高点海拔4476米、年均运动速度约5米、冰舌末端海拔3734米、雪线平均高度为4055米、朝向东北、主流呈“S”型。               </p>",
    "ds_process_way": "<p>采用重复丈量法</p>",
    "ds_quality": "",
    "ds_acq_start_time": "2017-08-26 00:00:00",
    "ds_acq_end_time": "2018-08-28 00:00:00",
    "ds_acq_place": "乌鲁木齐河源1号冰川",
    "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": "apply-access",
    "ds_total_size": 12722402,
    "ds_files_count": 3,
    "ds_format": "docx",
    "ds_space_res": null,
    "ds_time_res": "年",
    "ds_coordinate": "WGS84",
    "ds_projection": "",
    "ds_thumbnail": "ab749580-03ac-4df1-a816-665e58b90818.jpg",
    "ds_thumb_from": 2,
    "ds_ref_way": "",
    "paper_ref_way": "",
    "ds_ref_instruction": " 为保障平台科技资源的权益、扩展平台中心的服务、提升科技资源的应用潜力，请资源使用者在使用资源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），明确注明资源来源和资源作者。",
    "ds_from_station": null,
    "organization_id": "a626f549-a49c-4431-8c3f-70cfdfd4784f",
    "ds_serv_man": "王璞玉",
    "ds_serv_phone": "13669368590",
    "ds_serv_mail": "wangpuyu@lzb.ac.cn",
    "doi_value": "",
    "subject_codes": null,
    "quality_level": 3,
    "publish_time": "2021-11-22 19:08:10",
    "last_updated": "2021-11-22 19:08:10",
    "protected": false,
    "protected_to": null,
    "lang": "zh",
    "cstr": "11738.11.ncdc.Tianshan.2020.93",
    "i18n": {
        "en": {
            "title": "Changes in the end of Glacier No.1 at the source of Urumqi River, 2017-2018",
            "ds_format": "",
            "ds_source": "<p>Tianshan No.1 glacier is a two branch ice bucket valley glacier, with a length of 2.2 km, an average width of 500 m, an area of 1.828 square kilometers, a maximum thickness of 140 meters, a maximum altitude of 4476 meters, an average annual velocity of about 5 meters, an altitude of 3734 meters at the end of the ice tongue, and an average snow line height of 4055 meters.</p>",
            "ds_quality": "",
            "ds_ref_way": "",
            "ds_abstract": "<p>This data set is the end change data of Glacier No.1 at the source of Urumqi River from 2017 to 2018, including the East branch and the West Branch; the unit: meter; the end of each ablation season to the end of the next year's ablation season; repeated measurement method is used. The annual advance and retreat of Glacier No.1 in the East and West branches of Glacier No.1; the spatial coordinates of annual velocity points; the observation and Study on the material balance project of Glacier No.1 at the source of Urumqi River in Tianshan, China started in the summer of 1959. At that time, the area of Glacier No.1 was 1.95 km2, the length of glacier was 2.41 km, and the lowest altitude at the end of glacier was 3736 m. It is the largest modern glacier in the form of double cirque glacier in Urumqi River Basin. In 1993, a glacier degenerated into two completely independent glacier systems, namely, the West Branch of Glacier No. 1 and the Eastern Branch of Glacier No. 1. It also indicates that the glacier retreat in a region means that the number of glaciers in the region may increase, while the area and reserves of glaciers are decreasing.</p>",
            "ds_time_res": "年",
            "ds_acq_place": "Glacier No.1 at the headwaters of Urumqi River",
            "ds_space_res": "",
            "ds_projection": "",
            "ds_process_way": "<p>Repeated measurement was used</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": [
        "乌鲁木齐河源1号冰川",
        "东支",
        "西支",
        "末端变化观测"
    ],
    "ds_subject_tags": [
        "自然地理学"
    ],
    "ds_class_tags": [],
    "ds_locus_tags": [
        "一号冰川东支",
        "木齐河源1号冰川",
        "一号冰川西支",
        "乌鲁一号冰川西支",
        "乌鲁木齐河源1号冰川"
    ],
    "ds_time_tags": [
        2017,
        2018
    ],
    "ds_contributors": [
        {
            "true_name": "王璞玉",
            "email": "wangpuyu@lzb.ac.cn",
            "work_for": "天山冰川观测实验站",
            "country": ""
        }
    ],
    "ds_meta_authors": [
        {
            "true_name": "王璞玉",
            "email": "wangpuyu@lzb.ac.cn",
            "work_for": "天山冰川观测实验站",
            "country": ""
        }
    ],
    "ds_managers": [
        {
            "true_name": "王璞玉",
            "email": "wangpuyu@lzb.ac.cn",
            "work_for": "天山冰川观测实验站",
            "country": ""
        }
    ],
    "category": "冰川"
}