{
    "created": "2016-09-28 10:56:54",
    "updated": "2026-06-15 22:30:34",
    "id": "23c3b1fe-128c-11e6-9640-5cc5d45ad3ae",
    "version": 2,
    "ds_topic": null,
    "title_cn": "2012年黑河上游葫芦沟流域人工蒸发皿和降水数据集",
    "title_en": "Data set of artificial evaporating dish and precipitation in hulugou basin in the upper reaches of Heihe River in 2012",
    "ds_abstract": "<p>此数据集是祁连站2012年1月1日2012年12月1日葫芦沟流域出口水文断面总控葫芦沟流域地表径流量（测量用重庆华正水文仪器公司生产的LS45A型旋杯式流速仪）。1.数据概述：此数据集是祁连站2012年1月1日2012年12月1日葫芦沟流域出口水文断面总控葫芦沟流域地表径流量。/2.数据内容：/葫芦沟出口水文断面流量数据每日08:00、14:00、20:00定时观测流域出口水文断面流速、水位变化（流速测量用重庆华正水文仪器公司生产的LS45A型旋杯式流速仪，并用Hobo压力式水位计实时监测水位变化），建立水位流量关系，计算流域出口流量。/3.时空范围：/地理坐标：经度：99°53ˊE；纬度：38°16ˊN；海拔：2962.5m。/水文断面流量：断面流量是指单位时间内流经某一过水断面的水量，通常用Q表示，单位是立方米/秒。</p>",
    "ds_source": "<p>（1）蒸发量的测定为每日20:00时用20专用量杯量测；一般是前一日20时以专用量杯量清水20毫米（原量）倒入器内，24小时后即当日20时，再量器内的水量（余量），其减小的量为蒸发量。即：蒸发量=原量—余量。若前一日20时到当日20时之间有降水，则计算式为：蒸发量=原量+降水量—余量。</p>\n\n<p>（2）降水量一般采用2段制进行观测，即每日8时及20时各观测一次，雨季增加观测段次，雨量大时还需加测。日雨量是以每天上午8时作为分界，将本日8时至次日8时的降水量作为本日的降水量。若为降雨，用20专用量杯量测，当降雪时，仅用外筒作为承雪器具，然后用电子天平（沈阳龙腾ES30K-12型号电子天平，最小感量为0.2g）称重测量。</p>",
    "ds_process_way": "<p>自动采集</p>",
    "ds_quality": "<p>数据质量高，数据基本没有缺失，对LS45A型旋杯式流速仪测量的数据进行了计算分析，结果显示，数据真实可信，可以根据此数据做进一步的分析。</p>",
    "ds_acq_start_time": "2012-01-01 00:00:00",
    "ds_acq_end_time": "2012-12-31 00:00:00",
    "ds_acq_place": "黑河上游葫芦沟",
    "ds_acq_lon_east": 99.94555555555556,
    "ds_acq_lat_south": 38.176944444444445,
    "ds_acq_lon_west": 99.84555555555555,
    "ds_acq_lat_north": 38.31055555555555,
    "ds_acq_alt_low": null,
    "ds_acq_alt_high": null,
    "ds_share_type": "apply-access",
    "ds_total_size": 17525,
    "ds_files_count": 2,
    "ds_format": "excel",
    "ds_space_res": null,
    "ds_time_res": "日",
    "ds_coordinate": "WGS84",
    "ds_projection": "",
    "ds_thumbnail": "23c3b1fe-128c-11e6-9640-5cc5d45ad3ae.png",
    "ds_thumb_from": 2,
    "ds_ref_way": "",
    "paper_ref_way": "",
    "ds_ref_instruction": "本数据由“黑河寒区水文过程小流域综合观测与模拟”项目产生，用户在使用数据时请在正文中明确声明数据的来源，并在参考文献部分引用本元数据提供的引用方式。",
    "ds_from_station": "平台服务中心",
    "organization_id": "52b7b79b-860c-49a5-9083-9a70cf8bed5a",
    "ds_serv_man": "韩春坛",
    "ds_serv_phone": "13919408816",
    "ds_serv_mail": "hancht@lzb.ac.cn",
    "doi_value": "",
    "subject_codes": [],
    "quality_level": 3,
    "publish_time": "2021-01-11 15:20:53",
    "last_updated": "2023-11-02 10:38:42",
    "protected": false,
    "protected_to": null,
    "lang": "zh",
    "cstr": "11738.11.ncdc.nieer.2020.1152",
    "i18n": {
        "en": {
            "title": "Data set of artificial evaporating dish and precipitation in hulugou basin in the upper reaches of Heihe River in 2012",
            "ds_format": "",
            "ds_source": "<p>(1) The evaporation capacity is measured by  20 special measuring cup at 20:00 every day; generally, the special measuring cup is used to measure the fresh water 20 mm (the original volume) and poured into the device at 20:00 the previous day, and the water volume (the margin) in the re measuring device 24 hours later, that is, at 20:00 the same day, the reduced volume is the evaporation capacity. That is: evaporation = original amount - allowance. If there is precipitation between 20:00 of the previous day and 20:00 of the current day, the calculation formula is: evaporation = original amount + precipitation - allowance. </p>\n<p>(2) The precipitation is generally observed in two-stage system, i.e. once at 8:00 and once at 20:00 every day. In rainy season, the number of observation sections is increased, and when the rainfall is large, additional measurement is required. The daily rainfall is defined by 8:00 a.m. of each day, and the precipitation from 8:00 a.m. to 8:00 a.m. of the next day is regarded as the precipitation of the day. In case of rainfall, use  20 special measuring cup to measure. When it snows, only use the outer cylinder as the snow bearing apparatus, and then use the electronic balance (Shenyang Longteng es30k-12 model electronic balance, the minimum sensitivity is 0.2g) to weigh and measure. </p>",
            "ds_quality": "<p>The data quality is high, and the data is basically not missing. The data measured by ls45a rotating cup flowmeter is calculated and analyzed. The results show that the data is authentic and can be further analyzed based on this data. </p>",
            "ds_ref_way": "",
            "ds_abstract": "<p>This data set is the total surface runoff of hulugou drainage basin controlled by the hydrological section at the outlet of Qilian station on January 1, 2012 and December 1, 2012 (ls45a rotating cup type current meter produced by Chongqing Huazheng Hydrological Instrument Co., Ltd. is used for measurement). 1. Data overview: this data set is the total surface runoff of hulugou drainage basin controlled by the hydrological section of hulugou drainage basin at Qilian station on January 1, 2012 and December 1, 2012. /2. Data content: / at 08:00, 14:00 and 20:00 every day, the flow rate and water level change of the outlet hydrological section of hulugou River Basin shall be regularly observed (the flow rate shall be measured by ls45a rotating cup type current meter produced by Chongqing Huazheng Hydrological Instrument Company, and the water level change shall be monitored in real time by hobo pressure type water level meter), the water level flow relationship shall be established, and the outlet flow of the river basin shall be calculated. /3. Time and space range: / geographic coordinate: longitude: 99 ° 53 ˊ E; latitude: 38 ° 16 ˊ n; altitude: 2962.5m. /Hydrological section flow: the section flow refers to the water flow through a certain section in unit time, usually expressed in Q, and the unit is cubic meter / second. </p>",
            "ds_time_res": "日",
            "ds_acq_place": "Hulugou in the upper reaches of Heihe River",
            "ds_space_res": "",
            "ds_projection": "",
            "ds_process_way": "<p>Automatic acquisition</p>",
            "ds_ref_instruction": "This data is generated by the project of \"comprehensive observation and Simulation of hydrological process in small watershed in Heihe cold region\". When using the data, users should clearly state the source of the data in the text, and quote the reference provided by this metadata in the reference part."
        }
    },
    "submit_center_id": "ncdc",
    "data_level": 0,
    "recommendation_value": 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,
    "belong_to_nieer": false,
    "ds_topic_tags": [
        "降水量",
        "蒸发量",
        "气象水文"
    ],
    "ds_subject_tags": [],
    "ds_class_tags": [],
    "ds_locus_tags": [
        "黑河上游站",
        "祁连县",
        "葫芦沟流域",
        "青海省"
    ],
    "ds_time_tags": [
        2012
    ],
    "ds_contributors": [
        {
            "true_name": "韩春坛",
            "email": "hancht@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": "韩春坛",
            "email": "hancht@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": "韩春坛",
            "email": "hancht@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": "气象"
}