How do tradeoffs in satellite spatial and temporal resolution impact snow water equivalent reconstruction?

Author:

Bair Edward H.ORCID,Dozier JeffORCID,Rittger KarlORCID,Stillinger TimboORCID,Kleiber William,Davis Robert E.

Abstract

Abstract. Given the tradeoffs between spatial and temporal resolution, questions about resolution optimality are fundamental to the study of global snow. Answers to these questions will inform future scientific priorities and mission specifications. Heterogeneity of mountain snowpacks drives a need for daily snow cover mapping at the slope scale (≤30 m) that is unmet for a variety of scientific users, ranging from hydrologists to the military to wildlife biologists. But finer spatial resolution usually requires coarser temporal or spectral resolution. Thus, no single sensor can meet all these needs. Recently, constellations of satellites and fusion techniques have made noteworthy progress. The efficacy of two such recent advances is examined: (1) a fused MODIS–Landsat product with daily 30 m spatial resolution and (2) a harmonized Landsat 8 and Sentinel 2A and B (HLS) product with 3–4 d temporal and 30 m spatial resolution. State-of-the-art spectral unmixing techniques are applied to surface reflectance products from 1 and 2 to create snow cover and albedo maps. Then an energy balance model was run to reconstruct snow water equivalent (SWE). For validation, lidar-based Airborne Snow Observatory SWE estimates were used. Results show that reconstructed SWE forced with 30 m resolution snow cover has lower bias, a measure of basin-wide accuracy, than the baseline case using MODIS (463 m cell size) but greater mean absolute error, a measure of per-pixel accuracy. However, the differences in errors may be within uncertainties from scaling artifacts, e.g., basin boundary delineation. Other explanations are (1) the importance of daily acquisitions and (2) the limitations of downscaled forcings for reconstruction. Conclusions are as follows: (1) spectrally unmixed snow cover and snow albedo from MODIS continue to provide accurate forcings for snow models and (2) finer spatial and temporal resolution through sensor design, fusion techniques, and satellite constellations are the future for Earth observations, but existing moderate-resolution sensors still offer value.

Funder

National Aeronautics and Space Administration

Cold Regions Research and Engineering Laboratory

Publisher

Copernicus GmbH

Subject

Earth-Surface Processes,Water Science and Technology

Reference58 articles.

1. Baba, M. W., Gascoin, S., Kinnard, C., Marchane, A., and Hanich, L.: Effect of digital elevation model resolution on the simulation of the snow cover evolution in the High Atlas, Water Resour. Res., 55, 5360–5378, https://doi.org/10.1029/2018WR023789, 2019.

2. Bair, E. H.: SPIReS-MODIS-ParBal Snow Water Equivalent Reconstruction: Western USA, water years 2001–2021, Dryad [data set], https://doi.org/10.25349/D9TK7H, 2023a.

3. Bair, E. H.: Snow cover and snow water equivalent for “How do tradeoffs in satellite spatial and temporal resolution impact snow water equivalent reconstruction?”, Dryad [data set], https://doi.org/10.25349/D9PW47, 2023b.

4. Bair, E. H.: ParBal, Zenodo [code], https://doi.org/10.5281/zenodo.8106305, 2023c.

5. Bair, E. H.: SPIRES, Zenodo [code], https://doi.org/10.5281/zenodo.8106303, 2023d.

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