Collaborative Research: SGER--Dynamical Origins of Statistical Scaling in Floods on Real Networks-An Exploratory Diagnostic Analysis
Collaborative Research: SGER--Dynamical Origins of Statistical Scaling in Floods on Real Networks-An Exploratory Diagnostic Analysis
批准号:
0713714
负责人:
Vijay Gupta
金额:
$0.0万
依托单位国家:
美国
项目类别:
Standard Grant
财政年份:
2007
资助国家:
美国
项目状态:
已结题
起止时间:
2007-04-01 至 2008-09-30
中文摘要
一种新的洪水非线性地球物理理论,从此被称为标度理论,已经发展了近十年。它的明确目标是在划分自然地形的山坡-渠道联系的尺度上,从守恒方程和相关物理过程中预测洪水的空间统计幂律。在许多区域洪水频率的实证研究中,已经观察到年峰值流量统计与流域面积之间的幂律关系,最近在个别降雨径流事件中也观察到幂律关系。初步分析表明,基于事件的标度指数与年洪水分位数标度指数密切相关。这两组指数之间的密切关系提出了一个非常重要的假设,即不仅可以从单个RF-RO事件的物理过程中预测洪水尺度参数,而且可以通过考虑一年中的多个事件来预测年度洪水。智力优势:对理想化确定性自相似网络的研究表明,随着排水面积趋于无穷大,统计幂律逐渐出现。它们并不存在于控制洪水的物理方程中。这导致了一个关键的科学假设,即洪水中的幂律在通道网络的自相似性(自亲和性)中有其物理根源,这也是广泛观察到的网络分形结构及其霍顿关系的基础。目前的挑战是将理论推广到实际网络中。为了实现这一重要目标,我们建议使用两个农业研究服务盆地(亚利桑那州的核桃谷和密西西比州的古德温溪)的现有数据来测试诊断框架。关键思想是在一组分布参数假设下预测物理过程的幂定律。然后将这些预测与观察到的幂定律进行比较,以诊断我们的物理假设的有效性,并提出一组新的假设。为了预测洪水的标度规律,求解了一个质量守恒方程,该方程在自然地形中参数化了山坡-河道连接尺度上的物理过程,并计算了网络中每个连接的水流曲线。为了求解质量守恒方程,我们将使用我们的研究小组在过去五年中开发的基于gis的数字流域建模框架。这些目标本质上是探索性的,旨在建立“概念证明”。更广泛的影响:科学界一致认为,全球变暖是真实存在的,而且在很大程度上是由人类活动造成的。这种对行星水文气候的人为扰动正在引起一种非平稳变化,这使得无法根据长期历史降雨和河流流量数据进行统计洪水预测。历史水文数据通常用于统计水文模型,用于美国和世界其他国家的水资源管理。因此,非平稳气候下的水文预测对未来的水资源管理提出了一个巨大的问题。洪水的标度理论正在发展新的科学基础,特别适合在全球变暖引起的水文气候变化不稳定的新问题背景下进行洪水预测。洪水标度理论的科学基础可以概括为包括与水耦合的生态和生物地球化学过程,例如河岸蒸散,并在变化的水文气候中进行预测。
英文摘要
A new nonlinear geophysical theory of floods, henceforth called the scaling theory, has been developing for nearly a decade. It has the explicit goal to predict spatial statistical power laws in floods from conservations equations and related physical processes at the scale of hillslope-channel links that partition a natural terrain. In many empirical studies of regional flood frequencies, power law relationships have been observed between annual peak discharge statistics and drainage areas, and recently in individual rainfall-runoff events. Preliminary analyses show that event-based scaling exponents and the annual flood quantile scaling exponents are closely related. A close relationship between these two sets of exponents suggests a very important hypothesis, namely that it is possible to predict flood-scaling parameters from physical processes not only for individual RF-RO events, but also for annual floods by considering multiple events in a year.Intellectual Merit: Research in idealized deterministic self-similar networks has shown that statistical power laws emerge asymptotically as drainage area goes to infinity. They are not built into the physical equations governing floods. It has led to a key scientific hypothesis that power laws in floods have their physical origins in the self-similarity (self-affinity) of channel networks, which is also the basis for the widely observed fractal structure of networks and their Horton relations. The current challenge is to generalize the theory to real networks. To achieve this important goal, we propose to test a diagnostic framework using existing data from two Agricultural Research Service basins, Walnut Gulch, Arizona and Goodwin Creek, Mississippi. The key idea is to predict power laws from physical processes under a set of distributed parametric assumptions. Then compare the predictions with observed power laws for diagnosing the validity of our physical assumptions, and proposing a new set of assumptions. For predicting scaling laws in floods, a mass conservation equation, which parameterizes physical processes at the scale of hillslope-channel links in a natural terrain, is solved and flow hydrographs are computed for every link in a network. For solving the mass conservation equation, we will use a GIS-based digital watershed-modeling framework that our research group has developed in last five years. The objectives are exploratory in nature and are designed to establish a "proof of concept".Broader Impacts: Scientific consensus has grown that global warming is real and in substantial part is caused by human activities. This anthropogenic perturbation to the planetary hydro-climate is causing a non-stationary change, which precludes making statistical flood predictions from long-term historic rainfall and stream flow data. Historical hydrologic data are routinely used in statistical hydrologic models for the purposes of water resources management in the United States and other countries of the World. Therefore, hydrologic predictions in a non-stationary climate present an enormous problem for future management of water resources. The scaling theory of floods is developing new scientific foundations that would be particularly suited to make flood predictions in the context of the emerging problem of non-stationary hydro-climate change due to global warming. The scientific foundations of the scaling theory of floods can be generalized to include ecological and bio-geo-chemical processes that are coupled to water, for example, riparian evapotranspiration, and to make predictions in a changing hydro-climate.
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