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青藏高原七大河流源区径流深、蒸散发数据集（TPRED）

news 来源：原创 2025/5/11 7:42:03

时间分辨率月
空间分辨率 1km - 10km
共享方式开放获取
数据大小 83.27 MB
数据时间范围 1998-07-01 — 2017-12-31
元数据更新时间 2024-07-22

数据集摘要

通过构建耦合积雪、冻土、冰川等冰冻圈水文物理过程的WEB-DHM模型（Water and Energy Budget-based Distributed Hydrological Model），定量解析了青藏高原七大主要河流（黄河、长江、湄公河、怒江、雅鲁藏布江、恒河和印度河）源区的水资源时空动态与驱动机制，模拟生成了各流域1998~2017年逐月、5km水资源数据产品（包括径流、蒸发）（简称为TPRED）。

数据文件命名方式和使用方法

数据集为tif格式。每个流域一个文件夹，每个文件夹内包含该流域的runoff与ET等变量的数据集。

本数据要求的引用方式数据引用必读

数据的引用

王磊, 刘虎, 汪远伟, 齐嘉, 宋蕾, 柴晨好, 刘瑞顺, 范新凤, 李秀萍. (2024). 青藏高原七大河流源区径流深、蒸散发数据集（TPRED）. 国家青藏高原数据中心. https://doi.org/10.1038/s41597-024-03623-3.

Wang, L., Liu, H., Wang, Y., Qi, J., Song, L., Chai, C., Liu, R., Fan, X., Li, X. (2024). Tibetan Plateau runoff and evapotranspiration dataset by an observation-constrained cryosphere-hydrology model. National Tibetan Plateau / Third Pole Environment Data Center. https://doi.org/10.1038/s41597-024-03623-3.

(下载引用： RIS格式 RIS英文格式 Bibtex格式 Bibtex英文格式 )

文章的引用

1、Fan, X., Wang, L., Liu, H., et al. (2024). Tibetan Plateau Runoff and Evapotranspiration Dataset by an observation-constrained cryosphere-hydrology model. Sci Data 11, 773 (2024). https://doi.org/10.1038/s41597-024-03623-3 ( 查看下载 Bibtex格式 )

使用本数据时必须引用“文章的引用”中列出的文献，并进行数据的引用

参考文献

1、Wang, L., Zhou, J., Qi, J., Sun, L., Yang, K., & Tian, L., et al. (2017). Development of a land surface model with coupled snow and frozen soil physics. Water Resources Research, 53(6), 5085-5103. (查看| 下载)

2、Wang, L., Koike, T., Yang, K., et al. (2009). Development of a distributed biosphere hydrological model and its evaluation with the Southern Great Plains Experiments (SGP97 and SGP99). Journal of Geophysical Research: Atmospheres, 114(D8). (查看| 下载)

3、Shrestha, M., Koike, T., Hirabayashi, Y., et al. (2015). Integrated simulation of snow and glacier melt in water and energy balance‐based, distributed hydrological modeling framework at Hunza River Basin of Pakistan Karakoram region. Journal of Geophysical Research: Atmospheres, 120(10), 4889-4919. (查看| 下载)

4、Wang, Y.W., Wang, L., Zhou, J., Yao, T.D., Yang, W., Zhong, X.Y., Liu, R.S., Hu, Z.D., Luo, L., Ye, Q.H., Chen, N.S., & Ding, H.T. (2021). Vanishing Glaciers at Southeast Tibetan Plateau Have Not Offset the Declining Runoff at Yarlung Zangbo, Geophysical Research Letters, 48, e2021GL094651 (查看| 下载)

5、Liu, H., et al. (2023). Energy-balance modeling of heterogeneous glacio-hydrological regimes at upper Indus. J. Hydrol. Reg. Stud. 49, 101515. (查看| 下载)

6、Qi, J., et al. (2019). Coupled Snow and Frozen Ground Physics Improves Cold Region Hydrological Simulations: An Evaluation at the upper Yangtze River Basin (Tibetan Plateau). J. Geophys. Res. Atmos. 124, 12985–13004. (查看| 下载)

7、Song, L., et al. (2020). Improving Permafrost Physics in a Distributed Cryosphere-Hydrology Model and Its Evaluations at the Upper Yellow River Basin. J. Geophys. Res. Atmos. 125, 1–22. (查看| 下载)

8、Chai, C., Wang, L., Chen, D., Zhou, J., Liu, H., Zhang, J., Wang, Y., Chen, T., & Liu, R. (2022). Future snow changes and their impact on the upstream runoff in Salween. Hydrol. Earth Syst. Sci. 26(18), 4657–4683. https://doi.org/10.5194/hess-26-4657-2022 (查看| 下载)

请问runoff和Et的单位是多少呢？

可以参考文章的引用处提供的论文：https://doi.org/10.1038/s41597-024-03623-3