Abstract

Snow depletion curves (SDC) are functions that are used to show the relationship between snow covered area and snow depth or water equivalent. Previous snow cover data assimilation (DA) studies have used theoretical SDC models as observation operators to map snow depth to snow cover fraction (SCF). In this study, a new approach is introduced that uses snow water equivalent (SWE) observations and satellite-based SCF retrievals to derive SDC relationships for use in an Ensemble Kalman filter (EnKF) to assimilate snow cover estimates. A histogram analysis is used to bin the SWE observations, which the corresponding SCF observations are then averaged within, helping to constrain the amount of data dispersion across different temporal and regional conditions. Logarithmic functions are linearly regressed with the binned average values, for two U.S. mountainous states: Colorado and Washington. The SDC-based logarithmic functions are used as EnKF observation operators, and the satellite-based SCF estimates are assimilated into a land surface model. Assimilating satellite-based SCF estimates with the observation-based SDC shows a reduction in SWE-related RMSE values compared to the model-based SDC functions. In addition, observation-based SDC functions were derived for different intra-annual and physiographic conditions, and landcover and elevation bands. Lower SWE-based RMSE values are also found with many of these categorical observation-based SDC EnKF experiments. All assimilation experiments perform better than the open-loop runs, except for the Washington region’s 2004–2005 snow season, which was a major drought year that was difficult to capture with the ensembles and observations.

Highlights

  • Snow depletion curves (SDC) define the relationship between changes in snow cover area (SCA)and the snow pack, which can impact, for example, snow-albedo feedback in global climate models [1]and the amount of water storage and melt for hydrological models [2,3]

  • We present a new approach to estimating snow depletion curves and their application for assimilating snow cover fraction observations, using an Ensemble Kalman filter (EnKF) data assimilation approach and a land surface model with a multi-layer snow physics scheme

  • A secondary goal in applying this SDC approach is to see how accounting for varying vegetation, elevation, and temporal conditions may better capture heterogeneous features related to the snowpack and snow cover patterns when assimilating snow cover observations

Read more

Summary

Introduction

Snow depletion curves (SDC) define the relationship between changes in snow cover area (SCA). The amount of water storage and melt for hydrological models [2,3]. SDCs typically involve functions that are fit or tuned to a given set of snow-based observations or theoretical conditions. Many hydrological, land surface models (LSMs), and climate models use simple to complex schemes to define this snow depth-cover relationship, with many models still using very simple schemes, which do not account for even regional or temporal changes [4]. Some approaches to estimating snow depth-snow cover relationships involve statistical approaches, from using simple fitted functions to more shape and scale parameter-based gamma and beta distributions [4,5,6,7,8]. Much of the snowpack depletion in mountainous regions relates to late winter and early spring peak snow water equivalent (SWE) melt energy and radiation spatial variations (e.g., [2,9]), even though SWE can decrease without decreasing areal snow cover.

Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call