洪水等级是用来定量刻画洪水强弱及其潜在破坏力等级的物理量。本数据集为新疆天山北坡玛纳斯河流域 1957-2012年不同洪水强弱等级时间序列数据及洪水等级专题图。参考许武成(2004)提出的洪水等级划分方法，以新疆天山北坡玛纳斯河流域出山口肯斯瓦特水文站1957-2012年实测逐日径流数据为评估水文要素，进行等级划分和时间序列数据制图生成。专题图以0 ~12不同数值表示洪水强弱等级。本专题图可用来定量刻画洪水强弱及其潜在破坏力等级，采用完全开放共享。", "ds_source": "
逐日平均径流数据来自玛纳斯河流域出山口肯斯瓦特水文站（85°57′E，43°58′N）逐日实测径流量数据，时段为1957-2012，其中2006年数据缺失。", "ds_process_way": "
基于出山口肯斯瓦特水文站逐日平均径流数据进行等级划分（见公式1）。", "ds_quality": "
以新疆天山北坡玛纳斯河流域出山口肯斯瓦特水文站1957-2012年实测逐日径流数据为评估水文要素，参考许武成(2004)提出的洪水等级划分方法，以新疆天山北坡玛纳斯河流域出山口肯斯瓦特水文站1957-2012年实测逐日径流数据为评估水文要素，进行等级划分和时间序列数据制图生成。", "ds_acq_start_time": "1957-01-01 00:00:00", "ds_acq_end_time": "2012-12-31 00:00:00", "ds_acq_place": "天山北坡玛纳斯河流域出山口肯斯瓦特水文站", "ds_acq_lon_east": 45.75, "ds_acq_lat_south": 43.24166666666667, "ds_acq_lon_west": 83.95833333333334, "ds_acq_lat_north": 86.97500000000001, "ds_acq_alt_low": null, "ds_acq_alt_high": null, "ds_share_type": "apply-access", "ds_total_size": 13957071, "ds_files_count": 2, "ds_format": "xls.Excel.tif", "ds_space_res": null, "ds_time_res": "", "ds_coordinate": "无", "ds_projection": "", "ds_thumbnail": "71b900c9-e86f-4c2f-8e6d-1cc4bac757ac.jpg", "ds_thumb_from": 2, "ds_ref_way": "刘艳，1957-2012年新疆天山北坡玛纳斯河流域融雪型洪水强弱等级数据，国家冰川冻土沙漠科学数据中心(www.ncdc.ac.cn)，2023，doi：10.12072/ncdc.isnow.db2719.2023", "paper_ref_way": "", "ds_ref_instruction": "刘艳，卢新玉，火红，中国气象局乌鲁木齐沙漠气象研究所.1957-2012新疆天山北坡玛纳斯河流域融雪型洪水强弱等级专题图，2020。", "ds_from_station": null, "organization_id": "aba68fe5-65d3-41b1-b036-bc274a834b5e", "ds_serv_man": "李红星", "ds_serv_phone": "0931-4967592", "ds_serv_mail": "ncdc@lzb.ac.cn", "doi_value": "10.12072/ncdc.isnow.db2719.2023", "subject_codes": [ "170.15", "170.45", "170.55" ], "quality_level": 3, "publish_time": "2023-01-25 16:53:18", "last_updated": "2023-02-16 08:50:14", "protected": false, "protected_to": null, "lang": "zh", "cstr": "11738.11.ncdc.isnow.db2719.2023", "i18n": { "en": { "title": "Intensity grade data of snowmelt flood in Manas River basin on the northern slope of Tianshan Mountains in Xinjiang from 1957 to 2012", "ds_format": "", "ds_source": "
\nThe daily average runoff data is from the daily measured runoff data of Kenswat Hydrological Station (85 ° 57 ′ E, 43 ° 58 ′ N) at the mountain outlet of the Manas River basin. The period is 1957-2012, and the data in 2006 is missing.", "ds_quality": "
\nBased on the measured daily runoff data from 1957 to 2012 at the Kenswat Hydrological Station at the outlet of the Manas River Basin on the northern slope of the Tianshan Mountains in Xinjiang, and referring to the flood grade classification method proposed by Xu Wucheng (2004), the measured daily runoff data from 1957 to 2012 at the Kenswat Hydrological Station at the outlet of the Manas River Basin on the northern slope of the Tianshan Mountains in Xinjiang are used as the evaluation hydrological elements for grade classification and time series data mapping.", "ds_ref_way": "", "ds_abstract": "
\nFlood grade is a physical quantity used to quantitatively describe the flood intensity and its potential destructive power. This data set is the time series data of different flood intensity levels and flood level thematic map of the Manas River basin on the northern slope of Tianshan Mountains in Xinjiang from 1957 to 2012. With reference to the flood classification method proposed by Xu Wucheng (2004), the measured daily runoff data of the Kenswat Hydrological Station at the outlet of the Manas River Basin on the northern slope of the Tianshan Mountains in Xinjiang from 1957 to 2012 are taken as the evaluation hydrological elements to carry out the classification and time series data mapping generation. The thematic map shows the flood intensity level with 0~12 different values. This thematic map can be used to quantitatively describe the flood intensity and its potential destructive power level, and is fully open and shared.
", "ds_time_res": "", "ds_acq_place": "Kenswat Hydrological Station at the outlet of Manas River Basin on the north slope of Tianshan Mountains", "ds_space_res": "", "ds_projection": "", "ds_process_way": "\nGrading is based on the daily average runoff data of Kenswat Hydrological Station at the mountain pass (see Formula 1).", "ds_ref_instruction": " Liu Yan, Lu Xinyu, Huo Hong, Urumqi Desert Meteorological Research Institute of the China Meteorological Administration. 1957-2012 Special Map of Intensity and Intensity of Snow Melting Flood in Manas River Basin on the North Slope of Tianshan Mountains, Xinjiang, 2020." } }, "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": [ "融雪型洪水灾害" ], "ds_subject_tags": [ "大气科学", "地理学", "水文学" ], "ds_class_tags": [], "ds_locus_tags": [ "玛纳斯河流域" ], "ds_time_tags": [ 1957, 1958, 1959, 1960, 1961, 1962, 1963, 1964, 1965, 1966, 1967, 1968, 1969, 1970, 1971, 1972, 1973, 1974, 1975, 1976, 1977, 1978, 1979, 1980, 1981, 1982, 1983, 1984, 1985, 1986, 1987, 1988, 1989, 1990, 1991, 1992, 1993, 1994, 1995, 1996, 1997, 1998, 1999, 2000, 2001, 2002, 2003, 2004, 2005, 2006, 2007, 2008, 2009, 2010, 2011, 2012 ], "ds_contributors": [ { "true_name": "刘艳", "email": "liuyan@idm.cn", "work_for": "中国气象局乌鲁木齐沙漠气象研究所", "country": "中国" } ], "ds_meta_authors": [ { "true_name": "刘艳", "email": "liuyan@idm.cn", "work_for": "中国气象局乌鲁木齐沙漠气象研究所", "country": "中国" } ], "ds_managers": [ { "true_name": "刘艳", "email": "liuyan@idm.cn", "work_for": "中国气象局乌鲁木齐沙漠气象研究所", "country": "中国" } ], "category": "积雪" }