• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

青藏高原网格化降水强度-历时-频率曲线数据集。

A dataset of gridded precipitation intensity-duration-frequency curves in Qinghai-Tibet Plateau.

作者信息

Ren Zhihui, Sang Yan-Fang, Cui Peng, Chen Fei, Chen Deliang

机构信息

Key Laboratory of Water Cycle & Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing, 100101, China.

University of Chinese Academy of Sciences, Beijing, 100049, China.

出版信息

Sci Data. 2025 Jan 2;12(1):3. doi: 10.1038/s41597-024-04362-1.

DOI:10.1038/s41597-024-04362-1
PMID:39747886
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11695680/
Abstract

The Qinghai-Tibet Plateau (QTP), a high mountain area prone to destructive rainstorm hazards and inducing natural disasters, underscores the importance of developing precipitation intensity-duration-frequency (IDF) curves for estimating extreme precipitation characteristics. Here we introduce the Qinghai-Tibet Plateau Precipitation Intensity-Duration-Frequency Curves (QTPPIDFC) dataset, the first gridded dataset tailored for estimating extreme precipitation characteristics in QTP. The generalized extreme value distribution is chosen to fit the annual maximum precipitation samples at 203 weather stations, based on which the at-site IDF curves are estimated; then, principal component analysis is done to identify the southeast-northwest spatial pattern of at-site IDF curves, and its first principal component gives a 96% explained variance; finally, spatial interpolation is done to estimate gridded IDF curves by using the random forest model with geographical and climatic variables as predictors. The dataset provides precipitation information within 1, 2, 3, 6, 12, 24 hours and 5, 10, 20, 50,100 return years, with a 1/30° spatial resolution. The QTPPIDFC dataset can solidly serve for hydrometeorological-related risk management and hydraulic/hydrologic engineering design in QTP.

摘要

青藏高原是一个容易遭受破坏性暴雨灾害并引发自然灾害的高山地区,这凸显了开发降水强度-历时-频率(IDF)曲线以估算极端降水特征的重要性。在此,我们介绍青藏高原降水强度-历时-频率曲线(QTPPIDFC)数据集,这是首个专门用于估算青藏高原极端降水特征的网格化数据集。选择广义极值分布来拟合203个气象站的年最大降水样本,并据此估算站点IDF曲线;然后,进行主成分分析以识别站点IDF曲线的东南-西北空间模式,其第一主成分的解释方差为96%;最后,以地理和气候变量作为预测因子,利用随机森林模型进行空间插值以估算网格化IDF曲线。该数据集提供了1、2、3、6、12、24小时以及5、10、20、50、100重现期的降水信息,空间分辨率为1/30°。QTPPIDFC数据集可为青藏高原与水文气象相关的风险管理以及水利/水文工程设计提供有力支持。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/9f93144f7281/41597_2024_4362_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/0b4bfcc798e4/41597_2024_4362_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/4f2bad724d7d/41597_2024_4362_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/02d1b6e5668c/41597_2024_4362_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/46808f51fc87/41597_2024_4362_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/5e548ccc0a2c/41597_2024_4362_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/149dd89236c4/41597_2024_4362_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/9efc60b9ed6f/41597_2024_4362_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/381863296841/41597_2024_4362_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/01be6973f406/41597_2024_4362_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/1b4565cedce9/41597_2024_4362_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/9f93144f7281/41597_2024_4362_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/0b4bfcc798e4/41597_2024_4362_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/4f2bad724d7d/41597_2024_4362_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/02d1b6e5668c/41597_2024_4362_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/46808f51fc87/41597_2024_4362_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/5e548ccc0a2c/41597_2024_4362_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/149dd89236c4/41597_2024_4362_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/9efc60b9ed6f/41597_2024_4362_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/381863296841/41597_2024_4362_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/01be6973f406/41597_2024_4362_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/1b4565cedce9/41597_2024_4362_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5270/11695680/9f93144f7281/41597_2024_4362_Fig11_HTML.jpg

相似文献

1
A dataset of gridded precipitation intensity-duration-frequency curves in Qinghai-Tibet Plateau.青藏高原网格化降水强度-历时-频率曲线数据集。
Sci Data. 2025 Jan 2;12(1):3. doi: 10.1038/s41597-024-04362-1.
2
Temporal and spatial variations in the sub-daily precipitation structure over the Qinghai-Tibet Plateau (QTP).青藏高原(QTP)次日降水结构的时空变化。
Sci Total Environ. 2024 Mar 10;915:170153. doi: 10.1016/j.scitotenv.2024.170153. Epub 2024 Jan 15.
3
Dataset of trend-preserving bias-corrected daily temperature, precipitation and wind from NEX-GDDP and CMIP5 over the Qinghai-Tibet Plateau.来自NEX - GDDP和CMIP5的青藏高原趋势保持偏差校正后的每日温度、降水和风数据集。
Data Brief. 2020 May 21;31:105733. doi: 10.1016/j.dib.2020.105733. eCollection 2020 Aug.
4
Spatial-Temporal Evolution and Driving Forces of Drying Trends on the Qinghai-Tibet Plateau Based on Geomorphological Division.基于地貌划分的青藏高原干燥趋势的时空演变及驱动因素。
Int J Environ Res Public Health. 2022 Jun 28;19(13):7909. doi: 10.3390/ijerph19137909.
5
[Spatial-temporal variation of vegetation water use efficiency and its relationship with climate factors over the Qinghai-Tibet Plateau, China].[中国青藏高原植被水分利用效率的时空变化及其与气候因子的关系]
Ying Yong Sheng Tai Xue Bao. 2022 Jun;33(6):1525-1532. doi: 10.13287/j.1001-9332.202206.024.
6
Distribution Patterns of Gymnosperm Species along Elevations on the Qinghai-Tibet Plateau: Effects of Climatic Seasonality, Energy-Water, and Physical Tolerance Variables.青藏高原裸子植物物种沿海拔梯度的分布格局:气候季节性、能量-水分及物理耐受性变量的影响
Plants (Basel). 2023 Dec 4;12(23):4066. doi: 10.3390/plants12234066.
7
Zoning of precipitation regimes on the Qinghai-Tibet Plateau and its surrounding areas responded by the vegetation distribution.青藏高原及其周边地区降水格局分区受植被分布的影响。
Sci Total Environ. 2022 Sep 10;838(Pt 2):155844. doi: 10.1016/j.scitotenv.2022.155844. Epub 2022 May 10.
8
A high-resolution gridded grazing dataset of grassland ecosystem on the Qinghai-Tibet Plateau in 1982-2015.1982-2015 年青藏高原草地生态系统高分辨率格网化 grazing 数据集。
Sci Data. 2023 Feb 2;10(1):68. doi: 10.1038/s41597-023-01970-1.
9
Study on Spatiotemporal Variation Pattern of Vegetation Coverage on Qinghai-Tibet Plateau and the Analysis of Its Climate Driving Factors.青藏高原植被覆盖时空变化格局研究及其气候驱动因子分析。
Int J Environ Res Public Health. 2022 Jul 21;19(14):8836. doi: 10.3390/ijerph19148836.
10
Climatic factors and human disturbance influence ungulate species distribution on the Qinghai-Tibet Plateau.气候因素和人为干扰影响青藏高原有蹄类物种的分布。
Sci Total Environ. 2023 Apr 15;869:161681. doi: 10.1016/j.scitotenv.2023.161681. Epub 2023 Jan 19.

本文引用的文献

1
Global systematical and comprehensive overview of mountainous flood risk under climate change and human activities.气候变化和人类活动影响下山区洪水风险的全球系统性综合概述
Sci Total Environ. 2024 Sep 1;941:173672. doi: 10.1016/j.scitotenv.2024.173672. Epub 2024 May 31.
2
Estimation of the Qinghai-Tibetan Plateau runoff and its contribution to large Asian rivers.青藏高原径流量估算及其对亚洲大河的贡献。
Sci Total Environ. 2020 Dec 20;749:141570. doi: 10.1016/j.scitotenv.2020.141570. Epub 2020 Aug 12.
3
Importance and vulnerability of the world's water towers.
世界水塔的重要性和脆弱性。
Nature. 2020 Jan;577(7790):364-369. doi: 10.1038/s41586-019-1822-y. Epub 2019 Dec 9.
4
Rainfall extremes: Toward reconciliation after the battle of distributions.极端降雨:分布之争后的和解之路。
Water Resour Res. 2014 Jan;50(1):336-352. doi: 10.1002/2013WR014211. Epub 2014 Jan 15.