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Going from the virtual to the real world - using alternative data sources to tackle real-world challenges in hydrology

Going from the virtual to the real world - using alternative data sources to tackle real-world challenges in hydrology
从虚拟世界到现实世界 - 使用替代数据源应对现实世界的水文学挑战
批准号:
RGPIN-2014-04292
负责人:
Brissette, Francois
金额:
$1.6万
依托单位国家:
加拿大
项目类别:
Discovery Grants Program - Individual
财政年份:
2014
资助国家:
加拿大
项目状态:
已结题
起止时间:
2014-01-01 至 2015-12-31

项目摘要

项目成果

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中文摘要
翻译
应用水文学在很大程度上依赖于水文气象信息。水文模型(随机和确定性)的性能在很大程度上取决于输入数据的质量。气象站观测(通常测量温度和降水数据)为水文和其他模拟模式提供关键信息。然而,它们受到诸如时间视界短、数据丢失、错误、仪器偏差和设备更换或站点位移引入的偏差等问题的困扰。加拿大北部的一个更显著的缺点是站的空间密度低,具有长期观测记录的站几乎不存在。所有这些问题都严重限制了在流域尺度上充分反映水文过程时空变化的能力。也许更重要的是,这些问题会一直存在,因为北美的气象站数量正在减少,因为更多的气象站正在退役,而不是增加到现有的网络中。考虑到环境监测在气候变化中的重要性,这些网络的状态变得更加关键。面对这一令人担忧的现实,本研究计划旨在评估半虚拟和虚拟数据集作为传统站点数据(降水,温度,流量)的代理的使用。该计划将特别关注观察结果的再分析(半虚拟数据集)和高分辨率,有限区域动态生成的数据(来自区域气候模型的虚拟数据集)。再分析是由海洋-大气耦合模式通过同化来自不同来源的几个观测变量而产生的网格化数据。动态生成的数据来自各种复杂的动态模型(气候模型),这些模型与用于再分析的模型类似,但没有数据同化过程。当通过再分析在其边界处驱动时,区域气候模式将遵循驱动模式(再分析)中存在的大尺度环流,并有能力再现数据的历史序列,尽管比纯粹的数据再分析具有更多的自由度。在水文学中使用这些数据集既令人兴奋又有争议:令人兴奋的是,它们在现实世界中的应用构成了水文研究的新范式,但也存在争议,因为与观测数据集相比,它们显示出空间和时间偏差。具体而言,本研究计划将利用几个再分析和高分辨率区域气候模式数据集,为以下两个突出的水文问题提供替代解决方案:降水和温度历史时间序列缺失数据的填充。轴2。未测量流域的流量预报。在这两种情况下,在比较传统方法与本项目开发的方法时,将使用几个水文模型的输出作为主要的性能基准。我们有很高的期望,这些半虚拟和虚拟数据集的使用将为这些问题提供有效的替代解决方案,并且该研究计划将在为现实世界的应用建立这些数据集方面发挥先锋作用。
英文摘要
Applied hydrological science strongly relies on hydrometeorological information. The performance of hydrology models (stochastic and deterministic) is strongly dependent on the quality of input data. Weather station observations (typically measuring temperature and precipitation data) provide critical information to hydrology and other simulation models. They are however plagued with problems such as short temporal horizons, missing data, errors, instrument’s biases and biases introduced through equipment change or station displacement. A more significant drawback in Northern Canada is the low spatial density of stations and the quasi absence of stations with long observational records. All of these problems severely limit the ability to adequately represent the spatial and temporal variability of the hydrological processes at the basin scale. Perhaps more importantly, these problems are here to stay since the number of weather stations is decreasing in North America, as more stations are being decommissioned than added to the existing networks. The state of these networks is made even more critical considering the importance of environmental monitoring in a changing climate. In face of this alarming reality, this research programs aims at evaluating the use of semi-virtual and virtual datasets as proxies for traditional station data (precipitation, temperature, streamflow). This program will specifically look at reanalysis of observations (semi-virtual datasets) and high-resolution, limited-area dynamically generated data (virtual datasets from regional climate models). Reanalysis are gridded data generated from coupled ocean-atmosphere models through the assimilation of several observed variables from different sources. Dynamically generated data come from dynamical models of various complexities (climate models) which are similar to the ones used for reanalyses, however without the data assimilation process. When driven at their boundaries by reanalysis, regional climate models will follow the large-scale circulation present in the driving model (the reanalysis) and have the ability to reproduce the historical sequences of data, albeit with more degrees of freedom than a pure reanalysis of data. The use of these datasets in hydrology is both exciting and controversial: Exciting because their use in real-world applications constitutes a new paradigm in hydrological research, but controversial because they display spatial and temporal biases when compared against observation-derived datasets. Specifically, this research program will make use of several reanalysis and high-resolution regional climate model datasets to provide alternatives solutions to the following two outstanding hydrologic problems: Axis 1. Infilling of missing data in historical time series’ of precipitation and temperature. Axis 2. Streamflow forecasting in ungauged watersheds. In both cases, the outputs of several hydrology models will be used as the main performance benchmarks when comparing traditional approaches against the ones developed in this project. We have high hopes that the use of these semi-virtual and virtual datasets will offer efficient alternative solutions to these problems, and that this research program will play a pioneer role in the establishment of these datasets for real-world applications.
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