Javascript must be enabled to continue!
Quantifying uncertainty in estimation of hydrologic metrics for ecohydrological studies
View through CrossRef
AbstractHydrologic metrics have been used extensively in ecology and hydrology to summarize the characteristics of riverine flow regimes at various temporal scales but there has been limited evaluation of the sources and magnitude of uncertainty involved in their computation. Variation in bias, precision and overall accuracy of these metrics influences the ability to correctly describe flow regimes, detect meaningful differences in hydrologic characteristics through time and space, and define flow‐ecological response relationships. Here, we examine the effects of two primary factors—discharge record length and time period of record—on uncertainty in the estimation of 120 separate hydrologic metrics commonly used by researchers to describe ecologically relevant components of the hydrologic regime. Metric bias rapidly decreased and precision and overall accuracy markedly increased with increasing record length, but tended to stabilize >15 years and did not change substantially >30 years. We found a strong positive relationship between the degree of overlap of discharge record and similarity in hydrologic metrics when based on 15‐ and 30‐year discharge periods calculated within a 36‐year temporal window (1965–2000), although hydrologic metrics calculated for a given stream gauge tended to vary only within a restricted range through time. Our study provides critical guidance for selecting an appropriate record length and temporal period of record given a degree of metric bias and precision deemed acceptable by a researcher. We conclude that: (1) estimation of hydrologic metrics based on at least 15 years of discharge record is suitable for use in hydrologic analyses that aim to detect important spatial variation in hydrologic characteristics; (2) metric estimation should be based on overlapping discharge records contained within a discrete temporal window (ideally >50% overlap among records); and (3) metric uncertainty varies greatly and should be accounted for in future analyses. Copyright © 2009 John Wiley & Sons, Ltd.
Title: Quantifying uncertainty in estimation of hydrologic metrics for ecohydrological studies
Description:
AbstractHydrologic metrics have been used extensively in ecology and hydrology to summarize the characteristics of riverine flow regimes at various temporal scales but there has been limited evaluation of the sources and magnitude of uncertainty involved in their computation.
Variation in bias, precision and overall accuracy of these metrics influences the ability to correctly describe flow regimes, detect meaningful differences in hydrologic characteristics through time and space, and define flow‐ecological response relationships.
Here, we examine the effects of two primary factors—discharge record length and time period of record—on uncertainty in the estimation of 120 separate hydrologic metrics commonly used by researchers to describe ecologically relevant components of the hydrologic regime.
Metric bias rapidly decreased and precision and overall accuracy markedly increased with increasing record length, but tended to stabilize >15 years and did not change substantially >30 years.
We found a strong positive relationship between the degree of overlap of discharge record and similarity in hydrologic metrics when based on 15‐ and 30‐year discharge periods calculated within a 36‐year temporal window (1965–2000), although hydrologic metrics calculated for a given stream gauge tended to vary only within a restricted range through time.
Our study provides critical guidance for selecting an appropriate record length and temporal period of record given a degree of metric bias and precision deemed acceptable by a researcher.
We conclude that: (1) estimation of hydrologic metrics based on at least 15 years of discharge record is suitable for use in hydrologic analyses that aim to detect important spatial variation in hydrologic characteristics; (2) metric estimation should be based on overlapping discharge records contained within a discrete temporal window (ideally >50% overlap among records); and (3) metric uncertainty varies greatly and should be accounted for in future analyses.
Copyright © 2009 John Wiley & Sons, Ltd.
Related Results
Attribution of Eco-hydrological changes based on coupled SWAT-ML method
Attribution of Eco-hydrological changes based on coupled SWAT-ML method
Vegetation is an important part of terrestrial ecosystem, and the vegetation growth condition is closely related to hydro-meteorological elements. Accurate simulation of ecohydrolo...
New Perspectives for 3D Visualization of Dynamic Reservoir Uncertainty
New Perspectives for 3D Visualization of Dynamic Reservoir Uncertainty
This reference is for an abstract only. A full paper was not submitted for this conference.
Abstract
1 Int...
Reserves Uncertainty Calculation Accounting for Parameter Uncertainty
Reserves Uncertainty Calculation Accounting for Parameter Uncertainty
Abstract
An important goal of geostatistical modeling is to assess output uncertainty after processing realizations through a transfer function, in particular, to...
The uncertainty–investment relationship: scrutinizing the role of firm size
The uncertainty–investment relationship: scrutinizing the role of firm size
PurposeThe objective of this paper is threefold. First, it aims to empirically study whether firm-specific/idiosyncratic uncertainty, macroeconomic/aggregate uncertainty and politi...
Ecohydrological modelling to assist decision making for land- and water management: applications from The Netherlands
Ecohydrological modelling to assist decision making for land- and water management: applications from The Netherlands
Ecohydrological modelling to assist decision making for land- and water management: applications from The NetherlandsBiodiversity in nature areas is severely declining on both glob...
Multi-order hydrologic position: a high-resolution dataset for the conterminous United States
Multi-order hydrologic position: a high-resolution dataset for the conterminous United States
The location of a point within a stream network can be an important measure in hydrology. Hydrologic position (HP) is defined here by two metrics: lateral position (LP) and distanc...
Constraining simulation uncertainties in a hydrological model of the Congo River Basin including a combined modelling approach for channel-wetland exchanges
Constraining simulation uncertainties in a hydrological model of the Congo River Basin including a combined modelling approach for channel-wetland exchanges
Compared to other large river basins of the world, such as the Amazon, the Congo River Basin appears to be the most ungauged and less studied. This is partly because the basin lack...
Ecohydrological drivers of Neotropical vegetation in montane ecosystems
Ecohydrological drivers of Neotropical vegetation in montane ecosystems
AbstractMontane ecosystems are known for their high numbers of endemic species, unique climate conditions, and wide variety of ecosystem services such as water supply and carbon st...

