Beyond annual streamflow reconstructions for the Upper Colorado River Basin: A paleo-water-balance approach

14Citations
Citations of this article
31Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

In this paper, we present a methodology to use annual tree-ring chronologies and a monthly water balance model to generate annual reconstructions of water balance variables (e.g., potential evapotranspiration (PET), actual evapotranspiration (AET), snow water equivalent (SWE), soil moisture storage (SMS), and runoff (R)). The method involves resampling monthly temperature and precipitation from the instrumental record directed by variability indicated by the paleoclimate record. The generated time series of monthly temperature and precipitation are subsequently used as inputs to a monthly water balance model. The methodology is applied to the Upper Colorado River Basin, and results indicate that the methodology reliably simulates water-year runoff, maximum snow water equivalent, and seasonal soil moisture storage for the instrumental period. As a final application, the methodology is used to produce time series of PET, AET, SWE, SMS, and R for the 1404-1905 period for the Upper Colorado River Basin.

Cite

CITATION STYLE

APA

Gangopadhyay, S., McCabe, G. J., & Woodhouse, C. A. (2015). Beyond annual streamflow reconstructions for the Upper Colorado River Basin: A paleo-water-balance approach. Water Resources Research, 51(12), 9763–9774. https://doi.org/10.1002/2015WR017283

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free